Abstract
Prominences are intriguing, but poorly understood, magnetic structures of the solar corona. The dynamics of solar prominences has been the subject of a large number of studies, and of particular interest is the study of prominence oscillations. Ground and spacebased observations have confirmed the presence of oscillatory motions in prominences and they have been interpreted in terms of magnetohydrodynamic (MHD) waves. This interpretation opens the door to perform prominence seismology, whose main aim is to determine physical parameters in magnetic and plasma structures (prominences) that are difficult to measure by direct means. Here, we review the observational information gathered about prominence oscillations as well as the theoretical models developed to interpret small amplitude oscillations and their temporal and spatial attenuation. Finally, several prominence seismology applications are presented.
1 Prominences
Quiescent solar filaments are clouds of cool and dense plasma suspended against gravity by forces thought to be of magnetic origin. They form along the inversion polarity line in or between the weak remnants of active regions. Early observations already suggested that their fine structure is apparently composed by many horizontal and thin dark threads (de Jager, 1959; Kuperus and TandbergHanssen, 1967). More recent highresolution Hα observations obtained with the Swedish Solar Telescope (SST) in La Palma (Lin et al., 2005) and the Dutch Open Telescope (DOT) in La Palma (Heinzel and Anzer, 2006) have allowed to observe this fine structure with much greater detail (see Lin, 2010, for a review). The measured average width of resolved thin threads is about 03 arcsec (∼ 210 km), while their length is between 5 and 40 arcsec (∼ 3500 – 28,000 km). The fine threads of solar filaments seem to be partially filled with cold plasma (Lin et al., 2005), typically two orders of magnitude denser and cooler than the surrounding corona, and it is generally assumed that they outline the magnetic flux tubes in which they reside (Engvold, 1998; Lin, 2005; Lin et al., 2005; Okamoto et al., 2007; Engvold, 2008; Martin et al., 2008; Lin et al., 2008). This idea is strongly supported by observations which suggest that threads are skewed with respect to the filament long axis in a similar way to what has been found for the magnetic field (Leroy, 1980; Bommier et al., 1994; Bommier and Leroy, 1998). On the opposite, Heinzel and Anzer (2006) suggest that these dark horizontal filament structures are a projection effect. According to this view, many magnetic field dips of rather small vertical extension, but filled with cool plasma, are aligned in the vertical direction and the projection against the disk produces the impression of a horizontal thread.
Prominences are highly dynamic structures that display flows. These flows have been observed in Hα, UV, and EUV lines, and their study and characterization are of great interest for the understanding of prominence formation and stability, the mass supply, and the prominence magnetic field structure. In the Hα line, and in quiescent limb prominences, a complex dynamics with vertical downflows and upflows (Berger et al., 2008) as well as horizontal flows is often observed. The velocities are in the range between 2 and 35 km s^{1}, while in EUV lines flow velocities seem to be slightly higher. When comparing these values one should be aware that these lines correspond to different temperatures, so probably the reported flow speeds correspond to different parts of the prominence. In active region prominences, flow velocities seem to be higher than in quiescent prominences, even reaching 200 km s^{1}, and some of these highspeed flows are probably related with the prominence formation itself. In the case of filaments observed on the disk in the Hα line, horizontal flows in the filament spine are often observed, while in barbs flows are vertical. The range of observed velocities of filament flows is between 5 and 20 km s^{1}. A particular feature in these observations is the presence of counterstreaming flows, i.e., oppositely directed flows (Zirker et al., 1998; Lin et al., 2003). Because of the physical conditions of the filament plasma, all these flows seem to be fieldaligned. For a thorough information about flows in prominences see Labrosse et al. (2010) and Mackay et al. (2010).
Solar prominences are subject to various types of oscillatory motions. Some of the first works on this subject were concerned with oscillations of large amplitude induced by disturbances coming from a nearby flare. Later, observations performed with groundbased telescopes pointed out that many quiescent prominences and filaments display small amplitude oscillations (Harvey, 1969). These oscillations have been commonly interpreted in terms of standing or propagating magnetohydrodynamic (MHD) waves. Using this interpretation, a number of theoretical models have been set up in order to try to understand the prominence oscillatory behaviour. Such as we will point out in the following, the study of prominence oscillations can provide an alternative approach for probing their internal structure. The magnetic field structure and physical plasma properties are often hard to infer directly and wave properties directly depend on these physical conditions. Therefore, prominence seismology seeks to obtain information about prominence physical conditions from a comparison between observations and theoretical models of oscillations.
This review is mainly devoted to small amplitude oscillations, although a brief section deals with large amplitude oscillations. The layout of the review is the following: large amplitude oscillations are succinctly summarized in Section 2; in Section 3, the observational background about small amplitude oscillations is reviewed; in Section 4, theoretical models of small amplitude oscillations based on linear ideal MHD waves in different configurations are described; next, in Section 5, the damping of prominence oscillations produced by different mechanisms is studied from a theoretical point of view; finally, in Section 6, prominence seismology using large and small amplitude oscillations is introduced.
2 Large Amplitude Oscillations
Oscillations with velocity amplitude greater than 20 km s^{1} have been observed in filaments. It was suggested that their exciter was a wave, caused by a flare, which disturbs the filament and induces damped oscillations. This hypothesis was confirmed by Moreton and Ramsey (1960), who used a refined photographic technique that permitted the observation of the propagating perturbation, with velocities in the range 500 – 1500 km s^{1}. In some cases, during the course of the oscillations, the filament becomes visible in the Hα image when the prominence is at rest, but when its lineofsight velocity is sufficiently large, the emission from the material falls outside the bandpass of the filter and the prominence becomes invisible in Hα. This process is repeated periodically and for this reason this type of event is called a “winking filament”. Ramsey and Smith (1965) and Hyder (1966) studied 11 winking filaments and derived oscillatory periods between 6 and 40 min, and damping times between 7 and 120 min. They reported that there seemed to be no correlation between the period and the filament dimensions, the distance to the perturbing flare or its size. In addition, a single filament perturbed by four flares during three consecutive days oscillated with essentially the same frequency and damping time in each event. As a consequence, it was suggested that prominences possess their own frequency of oscillation.
The oscillatory velocity of the winking filaments studied by Ramsey and Smith (1965, 1966) and Hyder (1966) is quite large compared with the relevant wave speeds in prominences (namely the sound and Alfvén speeds). For this reason, one usually refers to these events as large amplitude oscillations. Recently, and thanks to space and groundbased instruments, new observations of large amplitude oscillations have been published. The exciters seem to be Moreton or EIT waves (Eto et al., 2002; Okamoto et al., 2004; Gilbert et al., 2008) or nearby jets and subflares (Jing et al., 2003, 2006; Vršnak et al., 2007), while in other cases the oscillations are associated to the eruptive phase of a filament (Isobe and Tripathi, 2006; Isobe et al., 2007; Pouget, 2007; Chen et al., 2008) or are produced by the Alfvénic vortex shedding mechanism recently developed by Nakariakov et al. (2009). In this last case, oscillations could be a signature of the transition from a stable to an unstable situation. Although in most of the observed flareinduced filament oscillations the material undergoes vertical oscillations, Kleczek and Kuperus (1969) and Hershaw et al. (2011) have also reported horizontal oscillations. Moreover, periodic motions along the longitudinal filament axis have also been observed (Jing et al., 2003, 2006; Vršnak et al., 2007).
The most recent interpretation of observations of large amplitude oscillations in a prominence has been given by Hershaw et al. (2011), who studied this kind of oscillations in an arched prominence observed with SoHO/EIT on 30 July 2005. The perturbations were produced by two consecutive trains of coronal waves coming from two different flares in an active region located far away from the prominence site. Both oscillatory trains had periods of around 100 min and excited prominence oscillations that lasted for about 18 h. During the oscillations, the displacement of the prominence was horizontal with respect to the solar surface. In the case of the first wave train, induced by a more energetic flare than the second one, the displacement in all the considered prominence locations shows a clear time damped oscillatory behaviour (see Figure 1). The oscillatory period, the damping time, and the horizontal velocity at different heights along the two prominence legs were determined (see Table 1 in Hershaw et al., 2011). The prominence oscillatory periods seem to depend on the height at which they were measured and, for each wave train, they show some differences depending on the leg in which they were measured. Focussing on the first wave train, which seems to trigger a clearly damped oscillation, the periods range between 86 and 101 min in one leg, and between 92 and 104 min in the other. Furthermore, the velocity amplitude also changes with height and reaches a maximum value of 50 km s^{1} in one leg and 33 km s^{1} in the other. This growth of the velocity amplitude with height, together with the fact that the oscillation seems to start in phase for both legs, led the authors to suggest that the oscillatory behaviour is caused by a global kink mode. The approximate analytical relationship between the damping time and the period τ = (1.6 ± 0.2)P^{0.9±0.1} was derived for the disturbance caused by the first wave train. This analytical fit suggests a linear dependence between the damping time and the period that could be compatible with resonant absorption as the damping mechanism (Ruderman and Roberts, 2002; Ofman and Aschwanden, 2002; Arregui et al., 2008b). However, this interpretation must be taken with care since the use of scaling laws to discriminate between damping mechanisms is questionable, at least for resonant absorption (Arregui et al., 2008a). Furthermore, some observational features such as differences in the periods measured in both legs, in the velocity amplitudes at both legs, etc., enabled the authors to suggest that the prominence could be composed by separate oscillating filamentary threads. In summary, from the reported observations it seems that one of the wave trains was able to induce large amplitude oscillations in the prominence while the effect of the second wave train was not so strong. The reason for these different behaviours could be attributed to the different energy carried by the wave trains or, in spite of the wave train periods being apparently similar, to a resonance effect between the wave train frequency and the natural oscillatory frequency of the prominence. Also, it is worth to remark that the reported observation was made in EUV while other observations of large amplitude oscillations have been made in Hα. The correspondence between oscillations observed in EUV and in Hα remains to be ascertained. Probably, only simultaneous observations could cast light on this relationship.
From the theoretical point of view, models that explain large amplitude filament oscillations are lacking. To explain the vertical motions, Anderson (1967) suggested that the disturbance coming from the flare propagates along the magnetic field and when it arrives to the filament, the material is pushed down. Hyder (1966) proposed a model which explains the vertical motions in terms of harmonically damped oscillations. The restoring force is provided by the magnetic tension, while the damping is due to coronal viscosity. Using this model, Hyder was able to calculate the strength of the vertical component of the magnetic field in the prominence. Later, Kleczek and Kuperus (1969) proposed a similar model to explain the horizontal oscillations, although in this case the damping is provided by the emission of acoustic waves. On the other hand, Sakai et al. (1987) developed a model for the formation of a prominence in a current sheet. One of the features of this model is the presence of nonlinear oscillations of the current sheet. Bakhareva et al. (1992) considered a partially ionized plasma and developed a dynamical model for a solar prominence in which nonlinear oscillations are present. Chin et al. (2010) have considered possible oscillatory regimes of nonlinear thermal overstability which can occur in prominences. Finally, numerical simulations (Chen et al., 2002) suggest that Moreton and EIT waves can be produced by CMEs. Then, the theoretical modelling of large amplitude oscillations excited by these events is a task that remains to be done. For a more extensive review about large amplitude prominence oscillations see Tripathi et al. (2009).
3 Small Amplitude Oscillations: Observational Aspects
Quiescent prominences are also subject to small amplitude oscillations, a type of periodic events characterized by one or more of these features:

1.
Not related to flare activity.

2.
Small velocity amplitude.

3.
Only a restricted volume of the prominence displays periodic variations.
Regarding item 1, so far it has not been possible to identify the trigger of small amplitude oscillations. A popular conjecture about their excitation is that it lies in the periodic motions of magnetic fields caused by photospheric or chromospheric oscillations. The idea is that Alfvén waves ought to propagate upwards and that any prominence material threaded by the field should also be subject to periodic motions if there is enough energy available to overcome the inertia of the dense plasma (Harvey, 1969); this idea was later suggested by other authors too (e.g., Yi et al., 1991). Harvey made orderofmagnitude calculations to show that the ratio of prominence to photospheric oscillatory energy is around or smaller than 10^{4}, which indicates that this excitation mechanism is feasible. On the other hand, Harvey also noted that a few prominences in his study appear to oscillate with periods nearly twice as large as those of the photospheric oscillation. This appears to contradict the above hypothesis about the initiator of small amplitude oscillations. Much longer and shorter periods than those present in Harvey’s work have been detected afterwards (see Section 33), so probably this mechanism of energy transfer from the photosphere (or chromosphere), if correct, may not be the only one to cause these prominence oscillations. Mashnich et al. (2009a,b) studied the Doppler velocity field in some filaments and the underlying photosphere by means of simultaneous observations of the Hα line and the neighbouring photospheric Fe i line at 4863 .A. They detected a quasihourly oscillation in certain areas of the filaments and photosphere and found a good spatial correlation between them. They also reported that the parts of the photosphere displaying this oscillation are often observed below filament barbs. The spatial coincidence of this periodicity and the relation of filament barbs and the photosphere led these authors to suggest that the photosphere was the origin of these particular prominence oscillations. From an observation of a limb prominence with Hinode, Ning et al. (2009b) reported that the detected oscillatory behaviour only lasted about one period and that new oscillations appeared nearby simultaneously. These authors then concluded that the exciters or drivers of such oscillations are numerous and of small scale. The current understanding (see Section 4) is that periodic perturbations in prominences can be produced by an external impulsive agent that excites different eigenmodes of the structure or by a continuous agent, as may be the case with the 5min photospheric and 3min chromospheric oscillations whose influence could propagate along magnetic field lines and force motions of the prominence plasma. Recently, some evidence about the effect of the chromospheric 3min oscillations on the corona has been found by Sych et al. (2009).
Regarding item 2, the detected Doppler velocity peak ranges from the noise level (down to 0.1 km s^{1} in some cases) to 2 – 3 km s1 (e.g., Harvey, 1969), although larger values have also been reported (e.g., Bashkirtsev and Mashnich, 1984; MolownyHoras et al., 1999; Ning et al., 2009a). This maximum value has to be compared with the typical speeds of the prominence plasma (the sound and Alfvén speeds), which are larger than 10 km s^{1} for typical prominence conditions. The main purpose of studying prominence oscillations is to obtain insight into their physics via a seismological approach (see Section 6). Therefore, the information that observations should provide are the periods, wavelength, phase, and group velocity and damping time of these phenomena. In addition, observations should also determine whether these periodic variations are standing oscillations or propagating waves, whether they affect some prominence threads or larger areas of a prominence, whether threads oscillate independently from their neighbours or which physical variables are disturbed and by which amount.
The solar origin of prominence oscillations remained controversial until the beginning of the 1990s. For example, Engvold (1981) failed to detect oscillatory motions in the velocity field of a limb prominence, although the observational setup used prevented him from reliably distinguishing velocity amplitudes below 2 km s^{1}, the range in which many peak values are found. In addition, Malherbe et al. (1981, 1987) recognized no oscillatory pattern in time series of lineofsight velocities obtained with the MSDP operating on the Meudon solar tower, although positive results were later achieved using the same instrument (Thompson and Schmieder, 1991). On the other hand, the lack of small amplitude, periodic variations in signals coming from solar prominences cannot be considered a proof against the existence of these kind of processes. Harvey (1969) noted that in a sample of 68 nonactive region prominences, 31% of the objects presented no significant velocity change along the lineofsight, 28% showed apparently random lineofsight velocity variations, and 41% presented a definite oscillatory behaviour. Analogous results were obtained for a set of 45 active region prominences. There are several reasons that may lead to the absence of periodic variations in some prominences: the velocity amplitude or its projection along the lineofsight may be too small to stand above the instrumental noise level; or the prominence material may actually not oscillate at the time the observations are performed; or the light emitted or absorbed by various plasma elements along the lineofsight and having different oscillatory properties may result in a noisy signal.
3.1 Detection methods
The investigation of small amplitude prominence oscillations has most often been done by spectroscopical means, but also using images (e.g., Foullon et al., 2004) or filtergrams, i.e., images taken in a given spectral line (e.g., Yi et al., 1991; Yi and Engvold, 1991; Lin, 2005; Berger et al., 2008; Ning et al., 2009b,a). Regarding these studies using a twodimensional field of view, in some of them the variations along selected straight paths have been analyzed (Berger et al., 2008; Ning et al., 2009b,a). This simplifies the study but also reduces the amount of oscillatory information that can be derived (see Figure 2).
Regarding spectroscopic observations, different setups have been used to gather the temporal variation of the spectral indicators and more complexity and refinement has been gained over the years. For example, in some initial studies an entrance hole was placed on a selected area of a prominence (Wiehr et al., 1984). Another technique that provides information about a small region of a prominence is the socalled differential method (Kobanov, 1983; Bashkirtsev and Mashnich, 1984). A very widely used method in the investigation of small amplitude prominence oscillations is to place a spectrograph slit on a prominence (a few examples from a very long list are: Tsubaki and Takeuchi, 1986; Suematsu et al., 1990; Balthasar et al., 1993; Balthasar and Wiehr, 1994; Suetterlin et al., 1997). Then, this yields a time series of spectra on each slit position (see, for example, Figure 4 of Tsubaki and Takeuchi 1986), from which the temporal variation of the spectral indicators (Doppler shift, line intensity, integrated line intensity, line width) can be derived. These time series can be later analyzed to obtain the period, wavelength, etc. of the oscillations (an example is shown in Figure 5 of Tsubaki and Takeuchi 1986). Slit observations have also been conducted from space, using SUMER on SoHO (Blanco et al., 1999; Régnier et al., 2001) and CDS on SoHO (Pouget et al., 2006).
A spectroscopic observation using a slit yields restricted information on the spatial distribution of oscillations and, what is even worse, does not ensure that the same plasma elements are placed on the slit during the observing time. The first of these concerns also applies to the analysis of a twodimensional data set in which only variations in one direction are considered. Observations using a twodimensional field of view and with high spatial resolution have diminished these worries, while allowing to study how prominence threads participate of the oscillatory motions. These observations have been conducted both with groundbased telescopes (Yi et al., 1991; Yi and Engvold, 1991; Lin et al., 2003; Lin, 2005; Lin et al., 2005, 2007, 2009) and with spacebased telescopes (Okamoto et al., 2007). In addition, twodimensional Dopplergrams have also been employed (MolownyHoras et al., 1999; Terradas et al., 2002), although the spatial resolution of this particular observation is not good enough to appreciate the prominence thread structure.
Although most data used in the analysis of small amplitude prominence oscillations come from typical prominence lines, in some cases spectral lines or images formed at hotter temperatures have also been considered. Examples are the He i line at 58433 Å, formed at 20,000 K (Régnier et al., 2001; Pouget et al., 2006); the Si iv and Oiv lines at 1393.76 Å and around 1401 – 1405 Å, formed at transition region temperatures (Blanco et al., 1999); and 195 Å images, with a formation temperature of 1.5 MK (Foullon et al., 2004). Cool prominences or filaments can be identified in coronal lines since the line intensity is reduced by means of two different mechanisms: absorption and volume blocking (Anzer and Heinzel, 2005). In the first case, coronal radiation coming from behind the cool structure is partially absorbed, while in the second case the volume filled with cool plasma does not contribute to coronal emission and in this region the radiative output is reduced as compared with the surrounding corona. These two mechanisms give place to a brightness reduction of coronal lines and allows us to identify the volume occupied by cool and dark structures like prominences or filaments. Arguably, oscillations in the dense prominence affect their rarer neighbourhood, so a joint investigation of the dynamics of the two media has a very promising seismological potential.
3.2 Spectral indicators
The vast majority of spectroscopic reports of prominence oscillations are based on the analysis of the Doppler velocity. Some other spectral indicators (line intensity and line width) have also been used in the search for periodic variations in prominences and, sometimes, a periodic signal has been recognized in more than one of these indicators. Landman et al. (1977) observed periodic fluctuations in the integrated line intensity and line width with period around 22 min, but not in the Doppler shift. In addition, Yi et al. (1991) detected periods of 5 and 12 min in the power spectra of the lineofsight velocity and the line intensity. Also, Suematsu et al. (1990) found signs of a ∼ 60 min periodic variation in the Doppler velocity, line intensity, and line width. Nevertheless, the Doppler signal also displayed shorter period variations (with periods around 4 and 14 min) which were not present in the other two data sets. We here encounter a common feature of other investigations, namely that the temporal behaviour of various indicators corresponding to the same time series of spectra do not agree, either because they show different periods in their power spectra (as in Tsubaki et al., 1987) or because one indicator presents a clear periodicity while the others do not (Wiehr et al., 1984; Tsubaki and Takeuchi, 1986; Balthasar et al., 1986; Tsubaki et al., 1988; Suetterlin et al., 1997). Only rarely have the oscillations been detected in several of these spectral indicators at the same time and with the same period, which constitutes a puzzling feature of prominence oscillations. This can be caused by insufficient instrumental sensitivity or by the effect different waves have on the plasma parameters (pressure, magnetic field, ...), which in turn may give rise to perturbations of one spectral indicator alone. In addition, Harvey (1969) failed to detect periodic perturbations in the lineofsight component of the magnetic field in a set of prominences that displayed oscillations of the Doppler velocity. He attributed this to the fact that variations in this magnetic field component were below the observational limit.
Special mention must be made of the study performed by Balthasar and Wiehr (1994), who simultaneously observed the spectral lines He at 3888 Å, H_{8} at 3889 Å and Ca^{+}IR_{3} at 8498 Å. From this information they analyzed the temporal variations of the thermal and nonthermal line broadenings, the total H_{8} line intensity, the He 3888 Å to H_{8} emission ratio and the Doppler shift of the three spectral lines. The power spectra of all these parameters yield a large number of power maxima, but only two of them (with periods of 29 and 78 min) are present in more than one indicator.
The interpretation of the results just summarized appears difficult. First, the theoretical models (see Section 4) can give the temporal behaviour of the plasma velocity, the density, and other physical parameters, in a prominence. The observations, however, yield information on quantities such as the line intensity or the line width. Hence, a clear identification of the spectral parameters with physical variables (density, pressure, temperature, magnetic field strength) is required before further progress can be achieved. Then, the presence of a certain period in more than one signal could be used to infer the properties of the MHD wave involved. Another useful source of information could be the detection of a given period in one signal but not in the others, such as reported in some works discussed above.
3.3 Detected periods
Early observational studies of small amplitude prominence oscillations revealed a wide range of characteristic periods, ranging from a few minutes (Harvey, 1969; Wiehr et al., 1984; Tsubaki and Takeuchi, 1986; Balthasar et al., 1986), to 15 – 25 min (Harvey, 1969; Landman et al., 1977), to 40 – 90 min (Bashkirtsev et al., 1983; Bashkirtsev and Mashnich, 1984; Wiehr et al., 1984; Balthasar et al., 1986). The apparent tendency of periods to group below 10 min or in the range 40 – 90 min led to the distinction between short and longperiod oscillations to refer to these two period ranges. Later, more reports of periods in the range 10 – 40 min were published (e.g., Yi et al., 1991; Suetterlin et al., 1997; Blanco et al., 1999; Régnier et al., 2001) and the intermediateperiod class emerged. However, this classification (solely based on the period value) is far from complete: Balthasar et al. (1993) observed a prominence simultaneously with the GCT and VTT telescopes in Tenerife to remove doubts about the instrumental or atmospheric origin of prominence oscillations and obtained strong power in the Doppler shift from both telescopes with period around 30 s; hence, very shortperiod small amplitude oscillations also exist. Furthermore, a few works in which prominences have been observed from space during extended time intervals show that very longperiod oscillations also exist: Pouget et al. (2006) detected periodicities of 5 – 6 h, while Foullon et al. (2004) and Foullon et al. (2009) have observed variations in EUV filaments with periods around 12 h, and 10 – 30 h, respectively. Although the classification in terms of shortperiod, longperiod, etc. oscillations is still in use, it does not cast any light nor gives any help with regard to the nature, origin, or exciter of the oscillations.
In some occasions, a given prominence has been observed over a few consecutive days and the outcome is that the same period seems to be recovered (Bashkirtsev and Mashnich, 1984; Mashnich and Bashkirtsev, 1990; Suetterlin et al., 1997). This seems to indicate that the overall properties of this prominence did not change much over this time interval. Similar studies have not been later carried out.
Some authors have tried to find correlations of the periods of small amplitude oscillations with other parameters. Harvey (1969) reported a correlation of the period with the unperturbed longitudinal magnetic field, such that long periods are associated with strong field strengths (Figure 3). This dependence is difficult to understand since, other parameters being equal (density, magnetic field line length, etc.), one expects just the inverse behaviour for fast MHD waves, and no dependence of the period on the magnetic field strength for slow MHD waves. Bashkirtsev and Mashnich (1993) claimed that the period of oscillation depends on solar latitude. Only periods above 40 min were included in this study and some 40 observations gathered along more than eight years were taken into account. The question then is whether this latitudinal dependence, if real, is related to the solar activity cycle or not. In a subsequent work by Mashnich and Bashkirtsev (1999) a similar latitudinal dependence was obtained for the quasihourly oscillations of the photosphere and chromosphere. The implications of these findings are profound and further checks are essential before their reality is firmly demonstrated.
3.4 Spatial distribution of oscillations
It now appears well established that small amplitude, periodic changes in solar prominences do not normally affect the whole object at a time, but are of local nature instead, and that this conclusion is independent of the oscillatory period. Thus, variations with a given period are seldom reported to occur over the whole prominence (see Tsubaki and Takeuchi, 1986). One case in which a periodic signal is present in all slit positions was presented by Balthasar et al. (1988), who detected longperiod oscillations over the whole height of three limb prominences by placing a vertical spectrograph slit on them. In contrast, it is usually found that only a few consecutive points along the slit present time variations with a definite period, while all other points lack any kind of periodicity (e.g., Tsubaki and Takeuchi, 1986; Suematsu et al., 1990; Balthasar et al., 1993; Balthasar and Wiehr, 1994; Suetterlin et al., 1997; MolownyHoras et al., 1997).
The works mentioned in the previous paragraph use a spectrograph slit to detect oscillations; obviously, a twodimensional data set is much more advantageous when it comes to ascertaining which part of a prominence is affected by oscillations. Terradas et al. (2002) reported on the propagation of waves over a large region (some 54,000 km by 40,000 km in size) in a limb prominence and high spatial resolution observations with Hinode/SOT (Berger et al., 2008) also show oscillations that affect a small area of a prominence. See also the discussion in Section 3.6.4 of the work by Lin et al. (2007) that gives evidence of coherent Doppler shift oscillations over a rectangular area 3.4 arcsec × 10 arcsec in size.
Other observations with high spatial resolution have shown that individual threads or small groups of threads may oscillate independently from the rest of the prominence with their own periods (Thompson and Schmieder, 1991; Yi et al., 1991). Figure 4 displays some of the results in Yi et al. (1991). It is clear that threads 1, 4, 13, and 14 oscillate in phase with their own period, which ranges from 9 to 14 min. In addition, Tsubaki et al. (1988) obtained successively two time series of spectra by placing the spectrograph slit first at a height of 30,000 km above the solar limb and next 40,000 km above the limb. A group of vertical threads detached from the prominence main body displayed 10^{7}min periodic variations at both heights, which was a first indication that threads can oscillate collectively. After these preliminary studies, much attention has been given to the detection of thread oscillations (Lin et al., 2003; Lin, 2005; Lin et al., 2005, 2007, 2009; Okamoto et al., 2007; Ning et al., 2009b,a). Apart from reporting on thread oscillations, these works have also provided detailed information about wave features such as the period, wavelength, and phase speed. Because of the importance of these quantities in the seismology of prominences, these works are discussed in more detail in Section 3.6.4.
There is also some evidence that velocity oscillations are more easily detected at the edges of prominences or where the material seems fainter, while they sometimes look harder to detect at the prominence main body (Tsubaki and Takeuchi, 1986; Tsubaki et al., 1988; Suematsu et al., 1990; Thompson and Schmieder, 1991; Terradas et al., 2002). This result has occasionally been interpreted as the consequence of integrating the velocity signals coming from various moving elements along the lineofsight. This explanation, however, would imply the presence of broader spectral lines at the positions showing periodic variations, which is not observed, so other explanations are also possible (Suematsu et al., 1990). Mashnich et al. (2009a,b) gave evidence that different parts of filaments may support different periodicities: shortperiod variations (with periods shorter than 10 min) had coherence scales shorter than 10 arcsec and were detected near the edges of filaments placed close to the Sun’s central meridian. These oscillations, hence, were characterized preferentially by vertical plasma displacements. On the other hand, variations with period around 1 h occured in different positions of the filament and the size of the oscillating area was not larger than 15 – 20 arcsec. In addition, these oscillations had an amplitude that increased by an order of magnitude or more in filaments far from the solar center compared to those near the center of the Sun’s disk. Then, these oscillations showed a mainly horizontal velocity.
More information about the spatial distribution of prominence oscillations comes from Ning et al. (2009b), who detected transverse oscillations of 13 threads in a quiescent prominence observed with Hinode/SOT. These authors found that prominence threads in the upper part of the prominence oscillate independently, whereas oscillations in the lower part of the prominence do not follow this pattern. Furthermore, the oscillatory periods were short (between 210 to 525 s), with the dominant one appearing at 5 min (more information is given in Section 3.6.4). In a subsequent work, Ning et al. (2009a) used the same data set to analyze the motions of two spines in the same quiescent prominence. The spine is synonymous with the horizontal fine structure along the filament axis and is the highest part of the prominence. In the observations of Ning et al. (2009a), the spines showed drifting motions that were removed by the subtraction of a linear trend, which allowed the authors to uncover the existence of oscillations with a very similar period (around 98 min) in both structures. Further insight into the behaviour of the spines comes from a fit of a function A[0] sin(2πt/A[1] + A[2]) exp(A[3]t) to the detrended data. Here A[0] is the oscillatory amplitude, A[1] the period, A[2] the oscillatory phase, and 1/A[3] the damping time. The detrended signals and the function fits are displayed in Figure 5, which includes the fitted parameters, that give the following information: from the oscillatory amplitude, the peak velocities of the spines are 1 and 5 km s^{1}. The periods are almost identical (96.5 and 98.5 min) and the phase difference is 149°, which means that the spines oscillated almost in antiphase. These results about the period and phase were taken by Ning et al. (2009a) as an indication of a collective behaviour of the two structures. These authors considered an analogy with the transverse MHD oscillations of two cylinders (a problem studied by Luna et al., 2008, and discussed in Section 4.4) and concluded that a coupling of kinklike modes can give the observed behaviour. In particular, the A_{ x } mode of the system has motions resembling the antiphase oscillatory behaviour found by Ning et al. (2009a).
3.5 Wave damping and oscillation lifetime
A visual inspection of the data sometimes reveals the existence of outstanding periodic variations and use of the FFT, or even better the periodogram (which yields an increased frequency resolution), is only necessary to derive a precise value of the period. In such cases it usually turns out that the oscillatory amplitude tends to decrease in time in such a way that the periodicity totally disappears after a few periods (e.g., Landman et al., 1977; Tsubaki and Takeuchi, 1986; Wiehr et al., 1989; MolownyHoras et al., 1999; Terradas et al., 2002; Lin, 2005; Berger et al., 2008; Ning et al., 2009b,a), just as found in large amplitude oscillations. This is then interpreted as a sign of wave damping, although the specific mechanism has not been commonly agreed on (see Section 5 for a summary of theoretical results on this topic).
Reliable values of the damping time, τ , have been derived by MolownyHoras et al. (1999) after fitting the function _{ v }_{0} cos(ωt + φ) exp(t/τ) to Doppler velocity time series recorded simultaneously in different positions of a polar crown prominence (Figure 6). The values of τ thus obtained are usually between 1 and 4 times the corresponding period, in agreement with previous observational reports. In addition, there is one particular case for which the lineofsight velocity grows in time, but no interpretation of this result is given by these authors.
Terradas et al. (2002) performed a deeper investigation of the data of MolownyHoras et al. (1999). After fitting the same sinusoidal function to all points in the twodimensional field of view, Terradas et al. (2002) generated twodimensional maps of various oscillatory parameters, such as the period, damping time and velocity amplitude (Figure 7). Terradas et al. (2002) stressed that there is a region near the prominence edge (54,000 km by 40,000 km in size) in which the correlation coefficient of the fit is rather large and in which the period and damping time are very uniform. The mentioned region is around position x = 80, y = 50 of Figure 7. In Section 3.63 we discuss other aspects of this work, which is unique since it is one of a few in which coherent wave behaviour has been found in a large area of a prominence and the only one in which the wave parameters in a twodimensional prominence area have been computed.
Very often the presence of a periodic signal in the data is not obvious under a visual scrutiny and the FFT or periodogram simply provide the period of such signal, but not its duration. Dividing the time series into shorter intervals and calculating the Fourier spectrum of each of them allows to narrow down the epoch of occurrence of the oscillation. Wiehr et al. (1984) followed this procedure and determined that a 3min oscillation found in a 2h Doppler velocity record only existed in the last 40 min of the sample. The wavelet technique, however, is much better suited for the calculation of lifetimes since it can be used to precisely determine the beginning and end of the time interval in which a periodicity, previously detected in the Fourier spectrum, takes place. This approach was used by MolownyHoras et al. (1997), who obtained a period around 7.5 min in 16 consecutive points, spanning a distance of 7300 km, along the spectrograph slit. The time/frequency diagram of the corresponding 16 time signals indicates that the periodic perturbation is not present for the whole duration of the data and that it only operates for about 12 min (Figure 8). MolownyHoras et al. (1998) performed a similar study by placing the slit on a filament, rather than on a limb prominence, with comparable results. Two oscillations with periods around 2.7 and 12.5 min were present at consecutive points covering some 2000 and 3300 km, respectively. From the wavelet analysis, the lifetimes of these two perturbations are of the order of 10 and 20 min, respectively. These results provide convincing evidence of the trainlike character of some prominence oscillations. Further details of the work by MolownyHoras et al. (1997) are provided in Section 3.6.2.
Oscillations of prominence threads also display fast attenuation. For example, Lin (2005) detected several periodicities over large areas of a filament, with maximum power at periods of 26, 42, and 78 min. Pronounced Doppler velocity oscillations with 26 min period could only be observed for 2 – 3 periods, after which they became strongly damped.
3.6 Wavelength, phase speed, and group velocity
To derive the wavelength (λ) and phase speed (c_{p}) of oscillations, time signals at different locations on the prominence must be acquired. The signature of a propagating wave is a linear variation of the oscillatory phase with distance. Hence, when several neighbouring points are found to oscillate with the same frequency, one can compute the Fourier phase of the signal at each of the points and check whether it varies linearly with distance. If it does, this gives place to a wave propagation interpretation and the wavelength can be calculated. This approach has been followed by Thompson and Schmieder (1991), MolownyHoras et al. (1997) (about which more details are given in Section 3.6.2), and Terradas et al. (2002) (see Section 3.63). On the other hand, Lin (2005) and Lin et al. (2007) (see Section 3.6.4) detected wave propagation along threads by studying Doppler velocity variations at fixed times. They observed a sinusoidal variation of the Doppler shift with distance along the thread, which allowed them to compute the wavelength. Moreover, the phase velocity of the oscillations can be derived from the inclination of the coherent features in the Doppler velocity timeslice diagrams. Other authors have followed less strict methods to calculate these wave parameters.
It must be mentioned that observations of wave propagation in slender waveguides or plane wave propagation in a uniform medium do not provide the actual value of the wavelength (λ), but its projection on the plane of the sky, which is shorter than λ. And if a slit or some points along a straight line are used, then the computed wavelength is the projection of λ on the slit or the line. The observationally measured period and wavelength can in turn be used to calculate the phase speed, but since the observational wavelength is a lower limit to λ, this observational phase speed is also a lower limit to c_{p} (Oliver and Ballester, 2002). Hence, even if it is not explicitly mentioned, the values of λ and c_{p} quoted here are observationally derived lower bounds to the actual values.
The results presented in this section are grouped in four parts, the first three of them in increasing order of complexity of the data analysis; the fourth one is devoted to thread oscillations. The reported wavelength values cover a range from less than 3000 km (for waves propagating along some threads) to 75,000 km (for waves propagating in a large area of a quiescent prominence). These numbers must be taken into account in the theoretical study of these events.
3.6.1 Simple analyses
Malville and Schindler (1981) observed a loop prominence some 90 min before the onset of a nearby flare and detected periodic changes with a wavelength along the loop of 37,000 km. This value, together with the period of 75 min, results in a phase speed of about 8 km s^{1}.
Subsequent reports, which we now describe, are based on sheetlike prominences. Thompson and Schmieder (1991) detected periodic variations with periods between 3.5 and 4.5 min in a filament thread. They then computed the Fourier phase of the points along the thread and, after confirming its linearity from a phase versus distance plot, the value λ ≃ 50, 000 km was derived, from which the phase speed is c_{p} ≃ 150 – 200 km s^{1}. In other works (e.g., Tsubaki and Takeuchi, 1986; Tsubaki et al., 1987, 1988; Suematsu et al., 1990) the signal in some consecutive locations along the slit has been found to be in phase. Although this seems to indicate that the wavelength of oscillations is much larger than the distance between the first and last of those points, this may not be necessarily true and a proper determination of the wavelength requires computing the Fourier phase corresponding to the oscillatory period.
Blanco et al. (1999) detected 15 – 20 min periodic variations corresponding to a pulse travelling with a speed of 170 km s^{1}. Such a large phase velocity is hard to reconcile with the typical speeds in a prominence, but it must be taken into account that this result has been obtained using Si iv and Oiv lines, which are formed at transition region temperatures. Still, Blanco et al. (1999) mention that the sound speed in the prominencecorona transition region must be considerably faster than 170 km s^{1}, which leads them to conclude that the detected wave is of fast or Alfvénic character. Assuming a density of 10^{10} cm^{3}, a magnetic field of 8 G is derived.
Foullon et al. (2004) analyzed the intensity on a set of points along the main axis of a filament in 195Å images. A timespace plot shows a clear oscillatory pattern at one end of the filament (around position 25 in Figure 9a). The oscillatory phase, displayed in Figure 9b, presents oscillatory fronts that are well correlated along the filament, meaning that the oscillations of neighbouring points along the filament are almost in phase. This is true in particular for positions around 25, although in positions around 5 and 10 the phase presents a linear trend in neighbouring points, which can be interpreted as wave propagation along the filament axis. Lower bounds to the wavelength and phase speed in this area could be determined as explained above. It is remarkable that the most pronounced periodic intensity variations, those around position 25, were detected during 6 days, which suggests that they suffered very little damping or were excited continuously during this time span.
Berger et al. (2008) used highresolution observations of limb prominences made by SOT on Hinode and detected oscillations that do not affect the whole prominence body. They considered three horizontal time slices at heights separated by 4.7 Mm and detected the presence of coherent oscillations in the three slices (Figure 2). A phase matching of the sinusoidal profiles of these oscillations results in a vertical propagation speed (i.e., phase speed) around 10 km s^{1}. Again this value comes from a projection on the plane of the sky and is therefore a lower bound of the real value.
3.6.2 An elaborate onedimensional analysis
MolownyHoras et al. (1997) took into account the projection effects in their analysis of the Doppler velocity along the spectrograph slit. They detected periodic velocity variations with period of 7.5 min some 7300 km along the slit and found that the Fourier phase of the velocity at this period changes linearly with distance (Figure 10). The value λ ≥ 20, 000 km was derived. The corresponding phase speed is c_{p} ≥ 44 km s^{1}.
To obtain the group velocity of this event, MolownyHoras et al. (1997) performed a wavelet analysis of the same set of data, which revealed the presence of a train of 7.5min waves in the slit locations (Figure 8). Moreover, the time of occurrence of the train of waves increases linearly along the slit, which agrees with the assumption of a propagating disturbance. The velocity of propagation along the slit can then be computed and the value v_{‖} ≃ 4.4 km s^{1} is obtained. Taking into account that v_{‖} is the projection of the group velocity, v_{g}, on the slit, one concludes that the above value provides a lower limit for the group velocity, so v_{g} ≥ 4.4 km s^{1}.
3.6.3 A twodimensional analysis
This section is devoted to review the work by Terradas et al. (2002), that stands out among all other works in which wave properties have been determined since in this one a fully twodimensional analysis is carried out. Figure 11 shows a time series of Hβ filtergrams of the prominence studied by Terradas et al. (2002). The corresponding time series of the Doppler signal is presented in Figure 12.
The data used by MolownyHoras et al. (1999) were reanalysed by Terradas et al. (2002) and clear evidence for propagating and standing waves was uncovered. These authors started from the Doppler velocity, which in many areas of the twodimensional field of view can be very well fitted by a damped sinusoid (Figures 6 and 7). The subsequent analysis was performed in a rectangle (black box in Figure 13) that includes an area in which the correlation coefficient of the fit is large. The period of the oscillations in this rectangle is quite uniform and with a value around 75 min. First, Terradas et al. (2002) conducted an analysis of the phase along two straight lines inside the rectangle. Along the continuous line in Figure 13, it is found that waves emanate from a point and propagate away from it (Figure 14). It is clear both from the raw and the fitted signals in Figure 14 that the slope of wave propagation to the left is larger than that to the right. To derive the wavelength, Terradas et al. (2002) plotted the Fourier phase associated to the most relevant period in the Fourier spectrum (i.e., the one with 75 min period) along the selected path (right panel of Figure 14). There is an almost linear decrease of the phase between positions 5 and 30, a linear increase between positions 50 and 62 and a region of roughly constant phase in between. The first two patterns correspond to propagation to the left and right along the path, such as was pointed out from the first two panels of Figure 14, while the third pattern is caused by standing wave motions. The slope of a straight line fitted to the Fourier phase in each of the regions with wave propagation gives the wavelength of oscillation (projected on the selected path) which is around 75,000 km and 70,000 km for propagation to the left and right, respectively. The corresponding phase velocities are around 17 km s1 and 15 km s^{1}.
Another interesting feature of this data set can be discerned by considering the dashed path in Figure 13. A representation of the Doppler velocity versus position and time (Figure 15) shows that, at least for the first half of the observational time, positive and negative velocities seem to alternate in phase separated by a region, around position 25, with nearly zero amplitude. This pattern suggests that rather than a propagating feature, the signal in this area behaves like a standing wave with two regions completely out of phase. The Fourier phase (right panel of Figure 15) is practically constant in a small region around position 10 and in a larger region for positions greater than 30, which indicates that there is no signal propagation in these locations. The phase difference between positions 10 and 50 is close to π, which, together with the fact that between these points the amplitude takes low values, is in close agreement with the standing wave picture and so a tentative identification of nodes and antinodes is possible. The estimated distance between the two antinodes visible in the left panel of Figure 15 is around 22,000 km. This implies that the (projected) wavelength of the standing wave is about 44,000 km and the corresponding phase speed is 10 km s^{1}. These values are about half those obtained for propagation along the other selected path and are a consequence of the anisotropic propagation of the perturbation.
In addition to the identification of standing and propagating wave features in the prominence, Terradas et al. (2002) went on to perform an investigation of the twodimensional distribution of the wavelength and phase speed. They started by plotting the Fourier phase for the most relevant period in the Fourier spectrum at each point (Figure 16), which shows that a deep global minimum is found around the central position of the plot. This particular phase structure is an indication that motions have their origin at the position of the minimum and propagate, although in an anisotropic way, from this point. Terradas et al. (2002) gave a much more clear interpretation of the twodimensional phase by plotting the wavevector field (Figure 17), computed as the gradient of the Fourier phase. The arrows in this figure indicate the direction of wave propagation, their length being proportional to the modulus of the wavenumber, k. The projection of the phase velocity on the plane of the sky (computed from c_{p} = ω/k) is also displayed in Figure 17. The analysis of the wavevector field shown in this figure clearly indicates that motions seem to be generated in a narrow strip close to positions x = 35 – 50 and y = 20 – 30 and spread out from this region. It is remarkable that the direction of the propagating waves from the source region is essentially parallel to or towards the prominence edge, revealing the anisotropic character of the observed wave propagation. The values of the phase velocity in Figure 17 are also quite different for both directions, being greater for the direction parallel to the edge, with c_{p} ∼ 20 km s^{1}, than for the direction perpendicular to the edge, with c_{p} ∼ 10 km s^{1}. This is an indication of the possible existence of some wave guiding phenomenon, which shows a preferential direction of propagation. Note the good agreement between the values of the phase velocity in the directions parallel and perpendicular to the edge and those derived from the analysis of the two selected paths based on Figures 14 and 15.
3.6.4 Thread oscillations
Yi et al. (1991) and Yi and Engvold (1991) used twodimensional spectral scans and investigated the presence of periodic variations of the Doppler shift and central intensity of the He i 10,830 Å line in two filaments. Yi et al. (1991) performed a first examination of the data and found oscillations with welldefined periods along particular threads in each prominence. For this reason, Yi and Engvold (1991) plotted the Doppler velocity versus position for different times in a given thread, so that a periodic spatial structure would directly yield a measure of the wavelength. Instead of this pattern, an almost linear variation of the velocity along the thread was found and consequently a value of λ much larger than the length of the threads, some 20,000 km in the two cases considered, was reported. Given that the periods are between 9 and 22 min, the corresponding phase speed is c_{p} ≫ 15 km s^{1}. This result suggests that the thread is oscillating in the fundamental kink mode (whose wavelength is of the order of the length of the supporting magnetic tube, that is, around 100,000 – 200,000 km; see Section 4.4.1), rather than being disturbed by a travelling wave. Let us mention that, in general, this analysis may be misleading since the velocity signal does not generally consist of the detected periodic component only, but it is made of this component mixed with other velocity variations. If the periodic component is weak, then the method used by Yi and Engvold (1991) may fail because the signature of the propagating wave is masked by the rest of the signal.
In the analysis of the Doppler velocity in two threads (denoted as T1 and T2) belonging to the same filament, Lin (2005) found a clear oscillatory pattern in timeslice diagrams along the two thin structures. She determined the following wave properties for thread T1: c_{p} = 60 km s^{1}, λ = 22, 12, 15 arcsec, and P in the range 2.5 – 5 min (the 4.4 min period being particularly pronounced). For thread T2, the wave properties are: c_{p} = 91 km s^{1}, λ = 38, 23, 18 arcsec, and P in the range 2.5 – 5 min (the 5min period being particularly pronounced).
The previous study by Lin (2005) is followed by a much more profound one in which the twodimensional motions and Doppler shifts of 328 features (or absorbing “blobs”) of different threads are examined (see also Lin et al., 2003). Forty nine of these features are observed to flow along the filament axis with speeds of 5 – 20 km s^{1} while oscillating in the lineofsight at the same time with periods of 4 – 20 min (see Figure 18). To simplify the examination of oscillations, Lin (2005) computed average Doppler signals along each thread and found that groups of adjacent threads oscillate in phase with the same period. This has two consequences: first, since the periodicity is outstanding in the averaged signal for each thread, the wavelength of oscillations is larger than the length of the thread. Again the interpretation of this result is that the threads oscillate in their fundamental kink mode. Second, in this data set threads have a tendency to vibrate collectively, in groups, rather than independently.
Horizontally flowing threads that undergo simultaneous transverse oscillations have not only been detected by Lin et al. (2003) and Lin (2005), but also by Okamoto et al. (2007) using SOT on Hinode. A Ca iiH line movie shows continuous horizontal thread motions along an active region prominence (cf. Figure 19). This movie also shows that the threads suffer apparently synchronous vertical oscillatory motions. An example of this phenomenon is shown in Figure 20. Six threads displaying the same behaviour were studied and periods in the range 135 – 250 s were measured. The thread flow velocities range from 15 to 46 km s^{1} and the vertical oscillation amplitudes range from 408 to 1771 km. These values are, of course, minimum estimates. A particularly interesting feature of these oscillations is that points along each thread oscillate transversally with the same phase. To reach this conclusion, a given thread is selected and several cuts along its length are considered. A representation of the signal as a function of time reveals that oscillations are synchronous along the entire length of the thread (Figure 21). Once more this points to the kink mode as the responsible for the oscillations, as first pointed out by Van Doorsselaere et al. (2008a).
Hα observations conducted with the Swedish 1m Solar Telescope by Lin et al. (2007) allowed to detect waves propagating in some selected threads. Figure 22 serves to illustrate the data analysis procedure for one thread. Here the line intensity shows no coherent behaviour (Figure 22a), while the lineofsight velocity presents some inclined features caused by waves propagating along the thread; two such features are labelled 1 and 2 in Figure 22b. Figure 22c is another way of presenting Figure 22b and is useful to illustrate more clearly the wavy character of the lineofsight velocities along an individual thread. Two shorter time sequencies of Doppler velocity are extracted from Figure 22c and shown in Figures 22d and e. It is clear that oscillations are of small amplitude since the Doppler shift has an amplitude of 1 – 2 km s^{1}. The power spectra of two of the curves in Figure 22c (shown in Figures 22f and g) yield wavelengths of the oscillatory pattern of, respectively, 3.8 arcsec and 4.7 arcsec. The phase velocity of the oscillations can be derived from the inclination of the features appearing in the Doppler timeslice diagrams of Figure 22b. The phase velocities thus obtained correspond to, respectively, 8.8 and 10.2 km s^{1}. Lin et al. (2007) found similar evidence of travelling waves in eight different threads. The mean phase velocity and period (obviously affected by the projection effect) are 12 km s^{1} and 43 min. Periods between 3 and 9 min were found; longer period oscillations could not be detected in the data set used in this work because of its limited duration (18 min).
To test the coherence of oscillations over a larger area, covering several threads, Lin et al. (2007) averaged the lineofsight velocity in a 3.4 arcsec × 10 arcsec rectangle containing closely packed threads. The averaged Doppler signal (left panel of their Figure 4) displays a very clear oscillation. In addition, the power spectrum of this signal has a significant power peak at 3.6 min. Thus, the conclusion is that neighboring threads tended to oscillate coherently in this rectangular area, possibly because they were separated by very short distances. This signal averaging could be analogous to acquiring data with poor seeing, such as in Terradas et al. (2002) (see Section 3.63).
Using data from the Swedish 1m Solar Telescope in La Palma, Lin et al. (2009) performed a novel analysis of thread oscillations by combining simultaneous recordings of motions along the lineofsight and in the plane of the sky, which provides information about the orientation of the oscillatory velocity vector. From the measurements of swaying motions in the plane of the sky, several threads in this work presented travelling disturbances whose main features were characterized (period, phase velocity, and oscillatory amplitude). These parameters were obtained following the procedure of Figure 22. Moreover, two of the previous threads also showed Doppler velocity oscillations with a period similar to that of the swaying motions, so that the threads had a displacement that was neither in the plane of the sky nor along the lineofsight. By combining the observed oscillations in the two orthogonal directions, Lin et al. (2009) derived the full velocity vectors. They suggested that thread oscillations were probably polarized in a fixed plane that may attain various orientations relative to the local reference system (for example, horizontal, vertical, or inclined). Swaying motions are most clearly observed when a thread sways in the plane of the sky, while Doppler signals are strongest for oscillations along the line of sight. In the case of the two analyzed threads, a combination of the observed velocity components yielded an orientation of the velocity vectors of 42° and 59° with respect to the plane of the sky. Once the heliocentric position of the filament was taken into account, these angles transformed into oscillatory motions which were reasonably close to the vertical direction. Lin et al. (2009) alerted that this conclusion is only based on two cases and that it is not possible to draw any general conclusion about the orientation of the planes of oscillation of filament threads. In fact, Yi and Engvold (1991) found no centerto limb variations of the velocity amplitude of threads displaying Doppler velocity oscillations, so they concluded that there did not seem to be a preferred direction of oscillatory motions in their data set.
Ning et al. (2009b) analyzed the oscillatory behaviour of 13 threads in a quiescent prominence observed with Hinode/SOT. They found that many prominence threads exhibited vertical and horizontal oscillatory motions and that the corresponding periods did not substantially differ for a given thread. In some parts of the prominence, the threads seemed to oscillate independently from one another, and the oscillations were strongly damped. Some of the oscillating threads presented a simultaneous drift in the plane of the sky with velocities from 1.0 to 9.2 km s^{1}. The reported periods were short (between 210 to 525 s), with the dominant one appearing at 5 min. Peak to peak amplitudes were in the range 720 – 1440 km and the phase velocity varied between 5.0 and 9.1 km s^{1}.
4 Theoretical Aspects of Small Amplitude Oscillations: Periods and Spatial Distribution
The usual interpretation of small amplitude oscillations is that some external agent excites MHD waves in the form of periodic disturbances of the cold plasma. MHD waves can be propagating or standing. In the first case, there is a periodic disturbance of the particles of the prominence plasma that may propagate in the medium. In the second case, the wave is confined to a region with fixed boundaries, thus producing the positive interference of propagating waves. Theoretical models usually consider small amplitude perturbations superimposed on an equilibrium configuration. Then the properties of propagating/standing MHD waves are analyzed. In the case of standing waves, we usually refer to the MHD eigenmodes of the system or to the modes for short.
Following our previous discussion of observations (Section 3.4), oscillations may affect individual threads, groups of threads or even larger areas of a prominence. The wave information (period, wavelength, phase speed, damping time) obtained from the analysis of this kind of events has been presented in Sections 3.5 and 3.6. Given that the main purpose of studying prominence oscillations is to gain a more profound understanding of their nature via seismological studies, it is necessary to study these oscillations theoretically. The information one expects to derive from these works consists of the main wave properties (period, wavelength, phase speed, damping time, spatial distribution, ... ). They can then be compared with the observationally determined values. The theory also allows us to determine the temporal variation of the perturbed magnetic field strength and its orientation, the perturbed density, temperature, etc., which means that these variables constitute another source of comparison with observations that will hopefully be exploited in the near future.
Theoretical works are here divided into five groups that reflect widely different choices of prominence equilibrium models: (a) simple, “toy” prominence models (Section 4.1); (b) models in which the prominence is represented as a plasma slab of finite width surrounded by the solar corona (Section 4.2); (c) line current prominence models (Section 43); (d) models of infinitely long prominence threads (Section 4.4); and (e) models concerned with the oscillations of prominence threads of finite length (Section 4.5).
4.1 Oscillations of very simple prominence models
The aim of the works discussed in this section is to follow elementary arguments to derive approximations for the oscillatory period and the polarization of plasma motions of the main modes of oscillation of a prominence. Some of the obtained results correspond to MHD modes studied in more detail in other works (see Section 4.2). One of these works (Joarder and Roberts, 1992b) is concerned with a prominence treated as a plasma slab embedded in the solar corona and with a magnetic field perpendicular to the prominence main axis (Figure 27). Waves are allowed to propagate along the slab. The coordinate system introduced by Joarder and Roberts (1992b) has the xaxis pointing across the prominence (i.e., parallel to the magnetic field), the z axis in the direction of wave propagation and the yaxis along the prominence. Three MHD modes exist in this configuration: the fast, Alfvén, and slow modes, with motions polarized in the z, y and xdirections, respectively. Some of the simple analogies discussed next allow us to derive approximations for the period of these modes.
A very simplified view of a prominence (Roberts, 1991; Joarder and Roberts, 1992a) is to consider it as a concentrated mass, M, suspended on an elastic string (representing the sagged magnetic field that supports the prominence; Figure 23a). Such a model provides some insight into the period of the prominence oscillating vertically as a whole under the action of gravity and magnetic tension. The equilibrium state is simply one in which the gravitational force, Mg, is balanced by the upward component of the tension forces, 2T sin θ, where T is the tension in one of the two strings and θ is the angle made by the string and the horizontal. Small amplitude oscillations of the mass about this equilibrium state have a period
with 2L the separation distance between the two anchor points, which is analogous to the distance between the photospheric feet of the magnetic tube supporting the prominence plasma. Roberts (1991) noted that for typical parameter values (g = 274 m s^{2}, 2L = 50,000 km, and θ between 3° and 30°), the period of these vertical oscillations is in the range 7 – 24 min, consistent with observationally reported values.
Roberts (1991) and Joarder and Roberts (1992b) considered a second model of interest (Figure 23b), that resembles the previous one except that now gravity is ignored. In this configuration there are two possible types of oscillation: either longitudinal or transversal. The frequencies of oscillation are given by
where again 2L is the distance between the anchor points, ρ is the mass density of the string (per unit length) and c_{str} is a natural wave speed of the string. To simplify matters one can assume that the mass of the string (2ρL) is negligible in comparison with M, that is, M ≫ ρL. Translating this inequality to prominences, it is equivalent to assuming that the mass of the cold plasma in a magnetic tube is much larger than the coronal mass in the same tube; this assumption seems most reasonable. Then, Equation (2) reduces to a simple expression for the fundamental mode frequency,
where it has been taken into account that the tension force is T = ρc ^{2}_{str} str. Although M has been considered a point mass, one can assume that it has a short, but finite, width 2x_{p}. Then, the previous expression for the tension force applied to the prominence part of the structure is T = M c ^{2}_{pro} /(2x_{p}), with c_{pro} a natural prominence wave speed. Now, inserting this expression into Equation (3) we obtain for the period
For fast magnetoacoustic waves in a prominence (with transverse polarization of motions), ..pro can be taken as the fast speed,
with v_{A} and c_{s} the Alfvén and sound speeds, respectively. These quantities are given by
and
with γ the ratio of specific heats, R the gas constant, μ the mean atomic weight, μ the magnetic permeability of vacuum, and T, ρ, and B the temperature, density, and magnetic field strength. For Alfvén modes (also characterized by transverse displacements in this simplified model) c_{pro} = v_{A}. The Alfvén velocity is the group velocity but not the phase velocity for Alfvén waves except for parallel propagation. On the other hand, for slow magnetoacoustic waves (with longitudinal polarization of motions), c_{pro} can be taken to be the cusp speed,
The fast speed in Equation (5) and the cusp speed in Equation (8) are in general different from the phase speed and the group speed for fast and slow magnetoacoustic waves. Only for very specific directions of propagation are these quantities phase and/or group speeds. Using the same parameters as above together with v_{A} = 28 km s^{1}, c_{s} = 15 km s^{1} and a prominence width equal to one tenth the length of magnetic field lines (i.e., 2x_{p} = 2L/10 = 5000 km), Equation (4) yields the periods P_{fast} = 26 min, P_{Alfven} = 30 min, and P_{slow} = 63 min, all of them within the range of observed intermediate to longperiod oscillations in prominences.
Oliver et al. (1993) (see also Roberts and Joarder, 1994) modified the mass loaded string model of Figure 23b by replacing the point mass M by a denser central string of width 2x_{p} (Figure 23c). To solve the wave equation it is necessary to impose the continuity of the displacement and its spatial derivative at the joints x = ± x_{p}. Here the xaxis is placed along the string with x = 0 the string centre. Then, upon imposing that the string is tied at its ends, the dispersion relation for even solutions about the centre of the string can be expressed as
whereas the dispersion relation for odd solutions can be written as
In these formulas c_{pro} and c_{cor} represent the natural wave speeds of the prominence and coronal parts of the string and ρ_{p} and ρ_{c} their respective densities. These expressions contain a rich array of solutions representing oscillatory modes of the system with different properties. And since there are three characteristic wave modes (fast, Alfvén, and slow, with their specific fast, Alfvén, and tube speeds in the prominence and corona), each set of modes is repeated three times. For the sake of simplicity, we here keep the parameters c_{pro} and c_{cor} in the following expressions, although it must be understood that these two speeds need to be substituted by their corresponding c_{f}, v_{A}, or c_{T} to derive the frequencies of the fast, Alfvén, and slow solutions.
Equations (9) and (10) can be numerically solved to obtain the frequencies of the various solutions. Nevertheless, some simplifications can be done by taking into account that the prominence width is much shorter than the length of magnetic field lines (x_{p} ≪ L) and that the prominence density is much larger than the coronal one (ρ_{p} ≫ ρ_{c}) (Joarder and Roberts, 1992b; Roberts and Joarder, 1994). Further assuming that ρ_{c}/ρ_{p} ≪ x_{p}/L ≪ 1 the following expression for the period of the fundamental mode can be obtained from Equation (9)
It is not surprising that the period corresponding to this frequency is just the one given by Equation (4). Other solutions to Equation (9) can be obtained by simply assuming ρ_{c}/ρ_{p} ≪ 1. They come in two sets (Joarder and Roberts, 1992b)
and
On the other hand, Equation (10) has no lowfrequency solution analogous to that of Equation (11). Instead, it has just two sets of solutions: one of them is identical to Equation (13) and the other one is similar to that given by Equation (12), namely
To understand the standing solutions supported by the string of Figure 23c, we now concentrate on their spatial distribution. Figures 24a and b display the two lowest frequency solutions of Equation (9), while Figures 24c and d show the two lowest frequency solutions of Equation (10). Their frequencies are approximately given by Equations (11), (12) with n = 1, (14) with n = 0, and (13) with n = 1, respectively. Let us refer to the parts of the string with density ρ_{c} and ρ_{p} as the external and internal regions. The eigenfunction in Figure 24d differs from the other three in that the displacement in the external region is an order of magnitude larger than in the internal region. For this reason it is termed an external mode, since its properties are dominated by the nature of the external part of the string (Joarder and Roberts, 1992b). One then is tempted to call the other three solutions in Figure 24 internal modes, but a simple experiment will prove this to be wrong (Oliver et al., 1993). Let us gradually reduce the size of the internal part of the string (by reducing x_{p}). Then internal mode frequencies (cf. Equations (12) and (14)) tend to infinity and in the limit x_{p} → 0 internal modes disappear and only external modes remain. It turns out that this process of gradually removing the density enhancement in the central part of the string does not eliminate the mode of Figure 24a, which is transformed into the fundamental mode of the string. Thus, this is not an internal mode. By a similar process (i.e., by letting x_{p} → L), the central part of the string can be progressively expanded so that we end up with a uniform density ρ_{p}. This makes external mode frequencies grow unbounded (cf. Equation (13)) and for x_{p} → L only internal modes remain. In this process the mode of Figure 24a transforms into the fundamental mode of the string. Hence, this mode is not an external mode, either, and it owes its existence to the concurrent presence of both the internal and external parts of the string. For this reason Oliver et al. (1993) labelled this solution a hybrid mode. The hybrid mode frequency is approximately given by Equation (11), the internal mode frequencies by Equations (12) and (14) and the external mode frequencies by Equation (13).
This string analogy points out the basic nature of a prominence’s modes of oscillation. Because there are in general three MHD modes, there is a fast hybrid mode, an infinite number of internal fast modes, and an infinite number of external fast modes (Joarder and Roberts, 1992b; Oliver et al., 1993; Roberts and Joarder, 1994). Their respective frequencies are given by Equations (11), (12), (13) and (14) with c_{pro} and c_{cor}, substituted by the prominence and coronal fast speeds. Something similar can be said about Alfvén and slow modes.
Anzer (2009) performed some simple estimates of the main oscillatory periods of a prominence using the KippenhahnSchlüter model (Kippenhahn and Schlüter, 1957) modified so as to include the corona in which the prominence is embedded (for a general solution see Poland and Anzer, 1971). In this configuration, see Figure 25, a curved magnetic field provides support of the cold plasma against gravity. Field lines outside the prominence do not bend downwards and so the magnetic field in the coronal environment does not present the desired arcade shape. For this reason, the role of the dense photosphere is played by two vertical rigid walls. Note that the configuration used by Anzer (2009) bears some resemblance to that of Figure 23a: the coronal magnetic field is almost uniform and makes an angle θ with the horizontal direction. Hence, tan θ = B_{z1}/B_{ x }, with B_{z1} the magnetic field at the prominence boundary. A further similarity between the present model and the previous ones is that the density is analogous to that of Figure 23c.
Instead of solving the MHD equations, Anzer (2009) took the clever approach of making educated guesses for the restoring forces acting over the prominence (F(ξ)) and then solving the equation
where ξ is the plasma displacement and M is the prominence column mass. For magnetically driven oscillations in the xdirection, caused by the magnetic pressure gradient, it is postulated that
so that the corresponding oscillatory period is
For oscillations in the y and zdirections the restoring force is the magnetic tension of the stretched field lines. In both cases the restoring force is
and the oscillatory period is
It does not come as a surprise that this formula is identical to Equation (1).
Anzer (2009) noted that the field line inclination is expected to be very small and, therefore, B_{z1}/B_{ x } ≪ 1. As a consequence, the period of xoscillations will be much larger than that of the other two modes, polarized in the y and zdirections.
Anzer (2009) also investigated perturbations driven by the gas pressure. He assumed that the coronal magnetic field is so strong that the prominence cannot distort it by a large amount. Further assuming that the magnetic field is horizontal, then the difference in gas pressure on either side of the prominencecorona interface can drive oscillations in the x direction. The restoring force is approximated by
and consequently the period of this mode is
This result coincides with that obtained from the simple string models of Figures 23b and c; see Equation (4).
Four oscillatory modes can be identified from these elementary considerations, but the restoring forces in the xdirection act in unison to create a single mode, so we are left with the familiar three MHD modes: fast, Alfvén, and slow.
Some values of the periods given by Anzer (2009) are similar to those in previous works: 200 min for the magnetically dominated oscillations in the xdirection, 430 min for the gas pressure driven oscillations and 20 min for the transverse, magnetically driven oscillations.
A further refinement of the string analogy (Joarder and Roberts, 1992b; Roberts and Joarder, 1994) can be introduced by noting that the magnetic field of a prominence is not at 90° with the prominence axis, contrary to the simple models of Figures 23 and 25. Instead, the prominence magnetic field makes an angle ϕ, typically around 20°, with the long axis of the slab. This is not too important for the almost isotropic fast modes, but Alfvén and slow modes propagate mainly along field lines, which in a skewed magnetic configuration are longer than 2L by a factor 1/ sin ϕ ≈ 3. Thus, the periods of these waves become larger by this same factor since the travel time needed for them to travel back and forth between the anchor points increases by 1/ sin ϕ. The result is that the hybrid Alfvén and slow modes can have periods up to 60 min and 5 h, respectively. It has been suggested that the last one may be the cause of the very longperiod oscillations observed by Foullon et al. (2004); Pouget et al. (2006).
4.2 Oscillations of prominence slabs
In a series of three papers, Joarder and Roberts conducted analyses of the modes of oscillation of a magnetized prominence slab embedded in the corona. The influence of gravity was neglected and so the plasma variables (temperature, pressure, and density) are uniform both in the prominence and in the coronal region. In the first of these works (Joarder and Roberts, 1992a) a purely longitudinal magnetic field was taken (see Figure 26). The dispersion relation contains a variety of modes, which can be fast or slow, combined with kink or sausage and body or surface. Because of the strong difference of the prominence and coronal physical parameters, some eigensolutions are slow in the external medium and fast in the internal medium. Tabulated periods range from 9 h and 5 h to a few minutes. The first values had not been reported at the time this work was published, so emphasis was given by the authors to fast surface modes, with shorter periods around 1 h, and to 5min and 3min Pekeris and Love modes.
Joarder and Roberts (1992b) considered the purely transverse magnetic field of Figure 27. From the characteristic wavenumbers of the solutions in the xdirection, Joarder and Roberts (1992b) created the distinction between internal and external modes (see Section 4.1 for a discussion of the features of these solutions). According to these authors, the former group of modes arises principally from the magnetoacoustic properties of the plasma slab, although these modes are somewhat influenced by the external material because of the presence of free interfaces between the prominence and corona. External modes are present, on the other hand, even in the absence of the prominence plasma but are modified because of the introduction of this cool, dense slab. The dispersion diagrams of kink and sausage modes are shown in Figure 28, where c_{sp} and v_{Ap} are the sound and Alfvén speeds in the prominence, while c_{sc} and v_{Ac} are their coronal counterparts. Moreover, Joarder and Roberts (1992b) also removed propagation along the prominence by setting k_{ z } = 0. The mode frequencies are then those on the vertical axes of Figure 28. In this case the dispersion relations of kink and sausage modes are those discussed for a string with densities ρ_{c} and ρ_{p} (Figure 23c), namely Equations (9) and (10). Joarder and Roberts (1992b) gave the approximate solutions of Equations (11) to (14), which are in very good agreement with the results of Figure 28 for k_{ z } = 0.
Oliver et al. (1993) provided more insight into the nature of internal and external modes while using the nonisothermal KippenhahnSchlüter solution represented in Figure 25. These authors followed the evolution of fast and slow modes in the dispersion diagram when the prominence is slowly removed by taking x_{p} → 0. They noted that the frequency of internal modes, both slow and fast, progressively grows until the modes disappear from the dispersion diagram and, therefore, only external modes remain. The presence of the prominence region thus provides physical support for the existence of internal modes. The same is true for external modes when the corona is gradually removed by making x_{p} → L. A clear distinction then arises between the two types of modes, although it turns out that the fundamental mode is internal and external at the same time, since it survives both when the prominence and the corona are eliminated. For this reason, this mode with mixed internal and external properties was called hybrid by Oliver et al. (1993) and later string by Joarder and Roberts (1993b) because it arises in the string analogy. Nevertheless, internal and external modes are also present in the string analogy (Section 4.1), so perhaps hybrid mode is a better denomination for this solution.
From Oliver et al. (1993) it also appears that the amplitude of perturbations in the prominence is rather small for external modes, a feature that is also present in the string solutions of Figure 24. For this reason it was postulated that they would probably be difficult to detect in solar prominences and that the reported periodic variations are produced by the hybrid and internal modes. In addition, the frequency of internal modes is shown to depend on prominence properties only, while that of hybrid and external modes depends on other physical variables such as the length of field lines. This is in agreement with the approximate Equations (11) to (14).
The essential difference between the equilibrium models in Joarder and Roberts (1992b) and in Oliver et al. (1993) is that gravity is neglected in the former, which results in straight magnetic field lines, while it is a basic ingredient in the later, which results in the curved shape of field lines characteristic of the KippenhahnSchlüter equilibrium model. Despite the different shape of field lines, the main features of the oscillatory spectrum are similar and so the influence of gravity and field line shape on the properties of the MHD modes is not too relevant in this kind of configurations.
A study of the oscillatory modes of the Kippenhahn and Schlüter (1957) prominence model was undertaken by Oliver et al. (1992). The equilibrium model is represented in Figure 25 although the corona is omitted. This implies that this work only provides a restricted account of the MHD modes of a slab prominence since there are no hybrid and external solutions in the absence of the corona. Oliver et al. (1992) noted that the three MHD modes possess different velocity orientations. The fast mode is characterized by vertical motions. The Alfvén mode by motions along the filament long axis, and the slow mode by plasma displacements parallel to the equilibrium magnetic field, which in this configuration is practically horizontal and transverse to the prominence. The immediate consequence of this association between modes and velocity polarization is that periodic variations in the Doppler shift are more likely to be detected in filaments near the disk centre for fast modes and in limb prominences for Alfvén and slow modes, depending on the orientation of the prominence with respect to the observer. These features of the MHD modes are retained in other models in which the equilibrium magnetic field is assumed perpendicular to the filament axis (Joarder and Roberts, 1992b, 1993a; Oliver et al., 1993; Oliver and Ballester, 1995, 1996). Nevertheless, the distinction between the three MHD modes is lost when the observed longitudinal magnetic field component is taken into account (Joarder and Roberts, 1993b). Probably, there are no characteristic oscillatory directions associated to the various modes (unfortunately, the issue of velocity polarization in a skewed magnetic equilibrium model has not yet been addressed in the context of prominence oscillations). The actual velocity field in prominences can be substantially more complex than that indicated by investigations based on models with magnetic field purely transverse to the prominence slab.
It is wellknown (Leroy, 1988, 1989) that magnetic lines are actually oriented at a rather small angle (around 20°) with the prominence axis. Joarder and Roberts (1993b) took this observational fact into account by adding a longitudinal magnetic field component to the equilibrium model used in Joarder and Roberts (1992b); see Figure 29. Now, the xyplane is defined to contain the assumed horizontal magnetic field. Then, it is not possible to place the z axis parallel to the wavenumber along the prominence axis, so now the k_{ y } and k_{ z } components must be considered. The assumptions of transverse field and propagation of perturbations in the zdirection made in the works discussed above simplify the MHD wave equations since the Alfvén mode is decoupled from the slow and fast modes, which can be studied separately with a subsequent reduction in complexity of the mathematical problem. The problem considered by Joarder and Roberts (1993b) contains coupled fast, Alfvén and slow modes. The resulting dispersion diagram (Figure 30) displays a very rich mode structure with plenty of mode couplings, which anticipates the complex nature of actual prominence MHD modes. Unfortunately, the physical properties of perturbations (velocity polarization, importance of the various restoring forces, perturbations of the equilibrium variables, ...) for the modes in the dispersion diagram have not been examined yet. Oscillation periods up to 4 h (for the slow hybrid mode) are present in this configuration.
The previous results rely on models in which the prominence and coronal temperatures are uniform, with a sharp jump of this physical variable from the cool to the hot region at an infinitely thin interface. A smoothed temperature transition between the two domains, representing the prominencecorona transition region (PCTR), was used by Oliver and Ballester (1996) to investigate the MHD modes of a more realistic configuration. Despite the presence of the PCTR in the equilibrium model, internal, external, and hybrid modes are still supported, just like in configurations with two uniform temperature regions. Nevertheless, the PCTR results in a slight frequency shift and in the modification of the spatial velocity distribution so as to decrease the oscillatory amplitude of internal modes inside the prominence. Hybrid modes are not so much affected by the presence of the PCTR because their characteristic wavelength is much longer than the width of the PCTR. Then, the conclusion is that the PCTR may influence the detectability of periodic prominence perturbations arising from internal modes.
Some twodimensional equilibrium models were considered by Galindo Trejo (1987, 1989a,b, 1998, 2006). The focus of these works was in the stability properties of prominence equilibrium configurations (using the MHD energy principle of Bernstein et al., 1958) and for this reason the author concentrated in the lowest eigenvalue squared. This means that information about all other modes of the system is absent. Galindo Trejo (1987) considered four prominence models, namely those by Kippenhahn and Schlüter (1957), Dungey (1953), Menzel (1951), and Lerche and Low (1980). All these models are isothermal, i.e., they do not incorporate the corona around the prominence plasma. This implies that the important hybrid modes are absent in the analysis. In spite of this, some interesting results were obtained by Galindo Trejo (1987). Here we only mention the most relevant ones. For example, the fundamental mode of the KippenhahnSchlüter configuration, whose period is 16 min, has motions polarized mainly across the prominence slab, so it can be associated with the internal slow mode. On the other hand, the fundamental mode of Dungey’s model has horizontal motions mostly along the prominence axis (such as corresponds to Alfvén waves) which are more important at the top of the prominence than at the bottom. The oscillatory period ranges from 55 to 80 min. In the case of Menzel’s model, the lowest frequency eigenmode has a period of 40 min and motions whose amplitude increases with height and oriented across the prominence. The eigenmode of Lerche & Low’s solution presents a greater range of periods (17 – 50 min) and, once more, with horizontal plasma displacements transverse to the prominence axis. Two improvements of this elaborated work can be done: the inclusion of the coronal plasma and the consideration of the oscillatory properties of other modes.
In two subsequent papers the stability of the prominence model of Low (1981) was investigated. In the first one (Galindo Trejo, 1989a) a uniform magnetic field component along the prominence axis was used, whereas in the second one (Galindo Trejo, 1989b) this quantity is not uniform. The author concluded that, as long as this magnetic field component is weak, these different choices of the magnetic configuration do not influence much the period of the fundamental mode, which is in the range 3 – 7 min. The spatial distribution of motions is similar to that found by Galindo Trejo (1987) for Menzel’s and Lerche & Low’s equilibrium models.
The following paper of this series (Galindo Trejo, 1998) is concerned with the prominence model of Osherovich (1985), which is characterized by a surrounding horizontal magnetic field connected with the prominence field. Different values of the equilibrium parameters were used and as a result the fundamental mode has periods that range from 4 to 84 min. Galindo Trejo (1998) found that for small values of the longitudinal magnetic field component large velocity amplitudes predominate in the upper part of the prominence, while the opposite happens for a stronger longitudinal component. The magnetic field shear is also relevant: for a moderate (and hence nonuniform) shear, the fundamental eigenmode is in the intermediateperiod range and for a uniform shear long periods are obtained.
Galindo Trejo (2006) investigated the equilibrium solution of Osherovich (1989), that is characterized by an external vertical magnetic field that allows the prominence to be placed on the boundary between two regions of opposite photospheric magnetic polarity. A wide range of periods was obtained in this work (9 – 73 min). Also, horizontal oscillatory motions either along the prominence or almost across it were found. Therefore, it seems that in most configurations studied by Galindo Trejo the fundamental oscillatory mode is a slow mode.
4.3 Oscillations of line current models
A completely different approach, based on line current models of filaments, was taken by van den Oord and Kuperus (1992), Schutgens (1997a,b), and van den Oord et al. (1998) in order to study filament vertical oscillations. They used the model introduced by Kuperus and Raadu (1974), in which the prominence is treated as an infinitely thin and long line, i.e., without internal structure. The interaction of the filament current with the surrounding magnetic arcade and photosphere was taken into account. Furthermore, both normal (NP) and inverse polarity (IP) configurations were considered. When a perturbation displaces the whole line current representing the filament, that remains parallel to the photosphere during its motion, the coronal magnetic field is also disturbed and the photospheric surface current is modified. This restructuring affects the magnetic force acting on the filament current. As a consequence, either this force enhances the initial perturbation and the original equilibrium becomes unstable, or the opposite happens and the system is stable against the initial disturbance. As a further complication, van den Oord and Kuperus (1992), Schutgens (1997a,b), and van den Oord et al. (1998) took into account the finite travel time of the perturbations between the line current and the photosphere and investigated the effect of these time delays on the filament dynamics. For both NP and IP configurations, exponentially growing or decaying solutions were found, which means that perturbations are amplified and the equilibrium becomes unstable, or that oscillations are damped in time and the equilibrium is stable.
Schutgens and Tóth (1999) considered an IP magnetic configuration in which the prominence is not infinitely thin but is represented by a currentcarrying cylinder. They solved numerically the magnetohydrodynamic equations assuming that the temperature has a constant value (10^{6} K) everywhere. The inner part of the filament is disturbed by a suitable perturbation that causes the prominence to move like a rigid body in the corona, both vertically and horizontally, undergoing exponentially damped oscillations. Horizontal and vertical motions can be studied separately since they are decoupled. It turns out that the period and damping time of horizontal oscillations are much larger than those of vertical oscillations. Some remarks about the damping mechanism at work in these models is presented in Section 5.6.
4.4 Fine structure oscillations (infinitely long thread limit)
Prominence models considered in Sections 4.1, 4.2, and 43 are very simplified representations of solar prominences. They provide us with information about a prominence global oscillatory behaviour, but high resolution observations (see Sections 3.4 and 3.6.4) have given us detailed information about the local oscillatory behaviour of the fine, internal structure of filaments. This has prompted the study of thread oscillations. Two situations can be considered: the simplest one is that of short waves propagating along a thread. By short we mean that the wavelength is much shorter than the thread length, so we refer to this problem as the infinitely long thread limit. On the other hand, the second situation includes propagating waves whose wavelength is comparable to or larger than the length of the thread and standing modes, whose wavelength is of the order of the length of the supporting magnetic tube and thus much larger than the thread length; the works concerned with this second kind of problem are presented in Section 4.5. Other important ingredients uncovered by observations (Sections 3.4 and 3.6.4) are the collective behaviour and the presence of flows in some oscillating threads. These features have been incorporated into some investigations and will be also discussed here.
4.4.1 Individual thread oscillations
A simple thread model consists of an infinitely long cylinder filled with cold, dense plasma and embedded in the hotter and less dense corona; field line curvature is neglected. The magnetic field is parallel to the cylinder axis and uniform everywhere (Figure 31).
The MHD modes of this structure have been extensively studied in the context of coronal and photospheric magnetic tube oscillations (Spruit, 1982; Edwin and Roberts, 1983; Cally, 1986). The mode of interest here is the kink mode because it is the only one that produces a significant transverse displacement of the thread, which is the observed behavior of oscillating threads. In the absence of mass flows and assuming that the thread radius is much smaller than the wavelength, the kink frequency is given by
with k_{ z } the axial wavenumber, ρ_{p} and ρ_{c} the prominence thread and coronal densities, ζ = ρ_{p}/ρ_{c} the density contrast, and \(v_{Ap,c} = B/\sqrt {\mu \rho _{p,c} }\) the prominence thread and coronal Alfvén velocities. In terms of the density contrast, the period of kink oscillations with wavelength λ = 2π/k_{ z } can then be written as
Note that the factor containing the density contrast varies between √2 and 1 when ζ is allowed to vary between a value slightly larger that 1 (extremely tenuous thread) and ζ → ∞. This defines a narrow range of Alfvén speed values when the inverse problem is solved for plasma diagnostic purposes (see Section 6). One can plug typical parameter values into Equation (23) and periods ranging from 30 s to a few minutes are obtained. This result is in agreement with the observed periods of traveling waves in threads (see Section 3.6.4).
This formula for P is based on some assumptions, namely that the thread is much longer than the wavelength, which in turn is much larger than the thread radius (this last approximation is also know as the thin tube limit). Shortwavelength propagating waves in threads have been detected by Lin et al. (2007) (see Section 3.6.4 and Figure 22). The length of the fine structure is around 20 arcsec, the reported wavelength is 3.8 arcsec, and the radius of threads is typically between 0.1 and 0.15 arcsec. We can appreciate that the assumptions made to derive Equation (23) are satisfied in this event.
Nakariakov and Roberts (1995) studied the magnetosonic modes of a magnetic slab when flows are present, while Soler et al. (2008) considered non adiabatic waves and included a mass flow parallel to the magnetic field in the thread model of Figure 32, which is identical to that of Figure 31 except for the inclusion of plasma flows. Without loss of generality the flow speed in the corona was neglected in this last work, while typical values observed in prominences were taken for the flow speed in the thread (namely U_{p} ≤ 30 km s^{1}). In the absence of flow, the complex oscillatory frequencies for a fixed, real and positive wavenumber k_{ z } appear in pairs, ω_{1} = ω_{R} + iω_{I} and ω_{2} = ω_{R} + iω_{I}. The solution ω_{1} corresponds to a wave propagating towards the positive zdirection (parallel to magnetic field lines). The ω_{2} solution corresponds to a wave that propagates toward the negative zdirection (antiparallel to magnetic field lines). Both solutions have exactly the same physical properties in the absence of flows. In the presence of flow, the frequencies are Doppler shifted. In addition, the symmetry between parallel and antiparallel propagation is broken. For instance, for strong enough flows, slow waves can only propagate parallel to the flow direction, antiparallel propagation being forbidden. Figure 33 presents the period of the slow, fast and thermal modes as a function of the flow speed in the thread. For U_{p} ≠ 0 the fast and slow waves acquire different periods that diverge as U_{p} is increased. For U_{p} ∼ 8.5 km s^{1} the antiparallel slow wave becomes a backward wave, which causes its period to grow dramatically near this flow velocity. The influence of the flow on the fast mode is not so severe, while the thermal mode has a finite period that takes very large values.
4.4.2 Collective thread oscillations
Some authors have reported that groups of threads oscillate in unison (e.g., Yi et al., 1991) and that large areas of a prominence present inphase oscillations (e.g., Terradas et al., 2002; Lin et al., 2007), which may be also taken as a sign of collective thread behaviour (see Sections 3.4, 3.63, and 3.6.4). Similar collective oscillations have been observed in coronal loops (Verwichte et al., 2004) and their properties have been studied by, e.g., Murawski (1993), Luna et al. (2008), Van Doorsselaere et al. (2008b), and Robertson and Ruderman (2011). To model this situation, an equilibrium model made of two homogeneous and infinitely long prominence threads embedded in the coronal medium has been considered (see Figure 34).
When identical threads are considered, the system exhibits four kinklike transverse oscillatory modes (Luna et al., 2008; Soler et al., 2009a). These modes are denoted by S_{ x }, A_{ x }, S_{ y } and A_{ y }. The S and A denote symmetry or antisymmetry of the total pressure perturbation with respect to the yzplane. The subscript describes the main direction of polarization of motions, that is in the xyplane; the choice of the coordinate axes is shown in Figure 34 and the spatial distribution of the modes is displayed in Figure 35. In addition to the kinklike modes, Soler et al. (2009a) studied the collective slow modes and obtained only two fundamental collective solutions, one symmetric and the other antisymmetric with respect to the yzplane, with motions mainly polarized along the zdirection (Figure 35).
A measure of the interaction between threads is the frequency of their normal modes. If the modes have frequencies similar to that of the isolated cylinder, then the threads oscillate independently from one another. If the frequencies are significantly different, the threads oscillate in a collective manner. The left panel of Figure 36 displays the real part of the frequency of the four kinklike solutions as a function of the distance between cylinders. For large separations, i.e., for a distance between threads larger than about 6 or 7 radii, the collective kink mode frequencies are almost identical to the individual kink frequency. This is a signature of a weak interaction between threads, which behave as independent structures. On the other hand, for short thread separations the four frequencies separate in two branches as a consequence of a strong interaction between the cylinders. Therefore, the collective behaviour of oscillations becomes stronger when the threads are closer. In the case of slow modes the interaction between threads is almost negligible and as a result the frequencies of the S_{ z } and A_{ z } modes are almost identical to the individual slow mode frequency (cf. right panel of Figure 36) in the whole range of thread separations. This is in agreement with the fact that transverse motions (responsible for the interaction between threads) are not significant for slow modes in comparison with their longitudinal motions. Therefore, the S_{ z } and A_{ z } modes essentially behave as individual slow modes, contrary to kinklike modes, which display a more significant collective behaviour.
Soler et al. (2009a) assessed the effect of material flows along two threads on the behaviour of collective modes (see Figure 37 for a sketch of the model). Arbitrary flows U_{1} and U_{2} were assumed in both cylinders, while coronal flows were neglected. The first main conclusion of this work is that the flows do not eliminate wave modes with collective dynamics (i.e., those that produce significant perturbations in the two threads), even in the case U_{1} ≠ U_{2}. Nevertheless, the requisite for retaining the collective dynamics is that the Dopplershifted individual frequencies of the threads must be very similar. In the case of kinklike modes the Dopplershifted frequencies are given by
where ω_{k1} and ω_{k2} are the kink frequencies of each thread, which are not equal if the thread densities differ. In the limit λ ≫ a, with a the tube radius, these frequencies are given by Equation (22). Now, the requirement for the two threads to oscillate in phase rather than independently is Ω_{k1} ∼ Ω_{k2}. Using Equation (22) and making the reasonable assumption that the density contrast in both cylinders is much larger than one, Soler et al. (2009a) obtained
where the + sign is for parallel waves and the − sign is for antiparallel propagation. A similar analysis can be performed for slow modes to obtain,
which points out that the coupling between slow modes occurs at different flow velocities than the coupling between kink modes. Therefore, the simultaneous existence of collective slow and kinklike solutions in systems of nonidentical threads is difficult. In the above equations, v_{A1,2} and c_{s1,2} correspond to Alfvén and sound speeds in both threads, respectively.
Soler et al. (2009a) extracted another conclusion from Equations (26) and (27): the difference between the Alfvén (sound) speed of the threads determines the difference of the flow speeds for the existence of collective behaviour of kink (slow) modes. Therefore, when flows are present in the equilibrium, collective motions can be found even in systems of nonidentical threads for very specific combinations of the two flow velocities. These velocities are within the observed values in prominences if threads with not too different temperatures and densities are considered. However, since the flow velocities required for collective oscillations must take very particular values, such a special situation may rarely occur in prominences. This conclusion has important repercussions for future prominence seismological applications, given that if collective oscillations are observed in large areas of a prominence, threads in such regions should possess very particular combinations of temperatures, densities, magnetic field strengths and flows.
4.5 Fine structure oscillations (finite length threads)
Filament threads have been modeled as magnetic flux tubes anchored in the solar photosphere (Ballester and Priest, 1989; Rempel et al., 1999) which are stacked one on top of one another in the vertical and horizontal directions, giving place to the filament body.
Many observations of oscillatory events in threads (see Section 3.6.4) cannot be accounted for by the simple models of Section 4.4 because the obtained results rely on the assumption that the thread length is much larger than the wavelength. Exceptions to this hypothesis are standing waves and propagating waves whose wavelength is of the order of or larger than the thread length. In the models presented in this section a thread is envisaged as a cold, dense condensation that fills the central part of a magnetic tube containing hot coronal plasma and anchored in the solar photosphere. Although this structure has been modeled with some complexity (Ballester and Priest, 1989; Rempel et al., 1999), only oscillations of much simpler thread configurations have been investigated so far. Because the reported thread oscillations are transverse, we here concentrate on works that investigate this kind of motions.
Joarder et al. (1997) considered a thin thread with finite width and length in Cartesian geometry (Figure 38). The thread is infinitely deep since the equilibrium configuration is invariant along the yaxis. The influence of the plasma pressure was neglected (i.e., the zeroβ limit was taken) and consequently the slow mode is absent from their analysis. Joarder et al. (1997) obtained the dispersion relations for Alfvén and fast modes, and restricted their study to the oscillatory frequencies, omitting other properties that are also relevant for the understanding of oscillations such as the spatial structure and the polarization of perturbations.
Using the same twodimensional configuration, Díaz et al. (2001) performed an analytical and numerical study of the behaviour of fast modes when a proper treatment of the boundary conditions at the different interfaces of this thread configuration is included. The main conclusion is that prominence threads can only support a few nonleaky modes of oscillation, those with the lowest frequencies. Also, for reasonable values of the thread length, the spatial structure of the fast fundamental even and odd kink modes is such that the velocity amplitude outside the thread takes large values over long distances (Figure 39). Fast kink modes are associated to normal motions with respect to the thread length (i.e., in the xdirection; see Figure 38). The fundamental kink mode (simply referred to as the kink mode) has a velocity maximum at the thread centre, while its first harmonic (that is, the fundamental odd kink solution) has a node in the same position.
Later on, Díaz et al. (2003) included wave propagation in the ydirection (see Figure 38) making the model fully threedimensional, and two important features appeared. The first is that the cutoff frequency, that separates confined and leaky modes, varies with the longitudinal wavenumber (k_{ y }), which allows the structure to trap more modes. The second one is that a much better confinement of the wave energy is obtained compared to the k_{ y } = 0 case (see Figure 40). An interesting issue concerning these results obtained using Cartesian threads is that large velocity amplitudes are found in the corona, which seems to favour collective thread oscillations in front of individual oscillations.
Since cylindrical geometry is more suitable to model prominence threads, Díaz et al. (2002) considered a straight cylindrical flux tube with a cool region representing the prominence thread, which is confined by two symmetric hot regions (Figure 41). With this geometry the fundamental sausage mode (m = 0, with m the azimuthal wavenumber) and its harmonics are always leaky. However, for all other modes (m > 0), at least the fundamental solution lies below the cutoff frequency. Hence, if any of these modes is excited the oscillatory energy in the prominence plasma does not vary in time after the initial transient has elapsed. Regarding the spatial structure of perturbations, in cylindrical geometry the modes are always confined to the dense part of the flux tube (Figure 42). Therefore, an oscillating cylindrical thread is less likely to induce oscillations in its neighbouring threads than a Cartesian one.
To study the oscillations of the above mentioned configurations, Díaz et al. (2001, 2002) developed a very general, although cumbersome procedure. However, Dymova and Ruderman (2005) considered the same problem and to simplify its study took advantage of the fact that the observed thickness of oscillating threads is orders of magnitude shorter than their length. Taking this into account, Dymova and Ruderman (2005) used the socalled thin flux tube (TT) approximation, that enables a simpler solution for the MHD oscillations of longitudinally inhomogeneous magnetic tubes. Once the partial differential equation for the total pressure perturbation is obtained, a different scaling (stretching of radial and longitudinal coordinates) of this equation inside the tube and in the corona can be performed. Following this procedure, two different equations for the total pressure perturbation inside and outside the flux tube, with well known solutions, are obtained. After imposing boundary conditions, the analytical dispersion relations for even and odd modes were derived and a parametric study was performed. A comparison between the numerical values of the periods obtained with this approach and that of Díaz et al. (2002) points out differences of the order of 1%. The only drawback of the method of Dymova and Ruderman (2005) is that it can be only applied to the fundamental mode with respect to the radial dependence.
Taking into account observations by, e.g., Lin (2005), which suggest inphase oscillations of neighbouring threads in a filament, Díaz et al. (2005) studied multithread systems in Cartesian geometry. The equilibrium configuration consists of a collection of twodimensional threads modeled as in Díaz et al. (2001) and separated by an adjustable distance 2c (Figure 43). An inhomogeneous filament composed of five threads was constructed (Figure 44) with thread density ratios thought to represent the density inhomogeneity of a prominence. The separations between threads were chosen randomly within a realistic range. The thread separations were then changed with respect to the values of Figure 44 by a certain factor and the kink modes were computed. Their frequencies are displayed in Figure 45, where c_{ref} is a reference value representative of the separations between threads. When the separations are small, i.e., for c_{ref}/L ≪ 1, there is a strong interaction between threads since the perturbed velocity in a given thread can easily extend over its neighbours. As a result, there is only one even nonleaky mode: the one producing inphase oscillations of all threads. The other extreme of Figure 45, i.e., c_{ref}/L ≫ 1, corresponds to very large separations. In this situation all threads oscillate independently and the individual kink mode frequencies are recovered. Note that realistic thread separations correspond to c_{ref}/L ∼ 10^{3} – 10^{2}, for which only the kink mode mentioned before is supported by the system. Its frequency is lower than the individual kink mode frequencies. Although these results show some agreement with observations about the collective oscillations of threads, the use of Cartesian geometry favours this kind of combined behaviour and so a similar study based on a cylindrical model is also of interest.
Díaz and Roberts (2006) studied the properties of the fast MHD modes of a periodic, Cartesian thread model (see Figure 1 of Díaz and Roberts 2006). This configuration provides a bridge between a structure with a limited number of threads (studied by Díaz et al., 2005, see Figure 43) and a homogeneous prominence with a transverse magnetic field (investigated by Joarder and Roberts, 1992b, see Figure 27). Díaz and Roberts (2006) found that for thread separations of the order of their thickness the only confined modes are those in which large numbers of threads are constrained to oscillate nearly in phase. The spatial structure of these solutions is similar to that of the propagating modes of a homogeneous prominence, with smallscale deviations due to the presence of the dense threads. Their period is equal to\(\sqrt f P\), with P the period of the prominence slab and ƒ the filling factor. The system with a limited number of threads has an even shorter period and a comparison between the different configurations considered by Díaz and Roberts (2006) gives periods of 23.6 min for the homogeneous prominence, between 12.1 and 193 min for the system of periodic threads and 53 for the fourthread configuration studied by Díaz et al. (2005). Hence, the main conclusion of Díaz and Roberts (2006) is that prominence fine structure plays an important role and cannot be neglected.
Terradas et al. (2008) modeled the transverse oscillations of flowing prominence threads observed by Okamoto et al. (2007) with HINODE/SOT (Section 3.6.4). The kink oscillations of a flux tube containing a flowing dense part, which represents the prominence material, were studied from both the analytical and the numerical point of view. In the analytical case, the Dymova and Ruderman (2005) approach with the inclusion of flow was used, while in the numerical calculations the linear ideal MHD equations were solved. The results point out that for the observed flow speeds there is almost no difference between the oscillation periods when static versus flowing threads are considered, and that the oscillatory period matches that of a kink mode. In addition, to obtain information about the Alfvén speed in oscillating threads, a seismological analysis as described in Section 6.6 was also performed. Also motivated by the observations by Okamoto et al. (2007), Soler and Goossens (2011) have further studied the properties of kink MHD waves propagating in flowing threads. In good agreement with Terradas et al. (2008), the period is seen to be slightly affected by mass flows. When the thread is located near the center of the supporting magnetic tube, and for realistic flow velocities, the effect of the flow on the period is estimated to fall within the error bars from observations. On the other hand, as the thread approaches the footpoint of the magnetic structure, flows introduce differences up to 50% in comparison to the static case. The variation of the amplitude of kink waves due to the flow is additionally analysed by Soler and Goossens (2011). It is found that the flow leads to apparent damping or amplification of the oscillations. During the motion of the prominence thread along the magnetic structure, the amplitude grows as the thread gets closer to the center of the tube and decreases otherwise. This effect might be important, since it would modify the actual observed attenuation, if any physical damping mechanisms is present.
Theoretical models described in this section have considered prominence plasmas as either slabs or cylindrical magnetic flux tubes. Slab models were intended to study the global oscillation properties of prominences, while flux tube models seem to be more appropriate for their application to the fine structure of prominences. Nevertheless, the properties of modes of oscillation like the kink mode have often been first studied in Cartesian geometry and then in cylindrical configurations. A few differences that arise are relevant when comparing the theoretical results to observations.
The theoretical frequencies for the kink mode in Cartesian geometry are above the value obtained for a cylindrical equivalent with the same physical properties. This has been shown by Arregui et al. (2007b), in the context of coronal loop oscillations. By assuming that a kink mode in a cylinder can be modeled in Cartesian geometry by adding a large perpendicular wavenumber, these authors show that in that limit the cylindrical kink mode frequency is recovered. A similar analogy was used by Hollweg and Yang (1988) who derived an expression for the damping time of a surface wave in Cartesian geometry and applied their result to coronal loops in the limit of large perpendicular wave number.
The spatial distribution of the eigenfunctions also differ when one compares, e.g., the kink mode properties in Cartesian and cylindrical geometry. The dropoff rate of the transverse velocity component is faster in cylindrical flux tubes than in slabs. A cylinder is a much better wave guide. For this reason, an oscillating cylindrical thread is less likely to induce oscillations in its neigboring threads than a Cartesian thread.
5 Theoretical Aspects of Small Amplitude Oscillations: Damping Mechanisms
Temporal and spatial damping is a recurrently observed characteristic of prominence oscillations (see Section 3.5). Several theoretical mechanisms have been proposed in order to explain the observed damping. Direct dissipation mechanisms seem to be inefficient, as shown by Ballai (2003), who estimated, through order of magnitude calculations, that several isotropic and anisotropic dissipative mechanisms, such as viscosity, magnetic diffusivity, radiative losses, and thermal conduction cannot in general explain the observed wave damping. The time and spatial damping of linear nonadiabatic MHD waves has been considered by Carbonell et al. (2004, 2009), Terradas et al. (2001), Terradas et al. (2005), Carbonell et al. (2006), and Soler et al. (2007, 2008). The overall conclusion from these studies is that thermal mechanisms can only account for the damping of slow waves in an efficient manner, while fast waves remain almost undamped. Since prominences can be considered as partially ionized plasmas, a possible mechanism to damp fast and Alfvén waves could be ionneutral collisions (Forteza et al., 2007, 2008), although the ratio of the damping time to the period does not completely match the observations. Besides nonideal mechanisms, another possibility to attenuate fast waves in thin filament threads comes from resonant wave damping (see, e.g., Goossens et al., 2010), which needs the presence of a smooth radial profile of the Alfvén speed. This phenomenon is well studied for transverse kink waves in coronal loops (Goossens et al., 2006; Goossens, 2008) and provides a plausible explanation for quickly damped transverse loop oscillations first observed by TRACE (Aschwanden et al., 1999; Nakariakov et al., 1999).
The time scales of damping produced by these different mechanisms should be compared with those obtained from observations, that indicate that the ratio of the damping time to the period, τ_{d}/P, is of the order of 1 to 4. The theoretical approach of many works about the damping of prominence oscillations has been to first study a given damping mechanism in a uniform and unbounded medium and, thereafter, to introduce structuring and nonuniformity. This has led to an increasing complexity of theoretical models in such a way that some of them now combine different damping mechanisms. Detailed reports on theoretical studies of small amplitude oscillations in prominences and their damping can be found in Oliver (2009), Ballester (2010), and Arregui and Ballester (2011). Here, we collect the most significant aspects of the theoretical mechanisms that have been proposed to explain the observed timescales.
5.1 Damping of oscillations by thermal mechanisms
In a seminal paper, Field (1965) studied the thermal instability of a dilute gas in mechanical and thermal equilibrium. Using this approach, the time damping of magnetohydrodynamic waves in bounded KippenhahnSchlüter and Menzel prominence models was studied by Terradas et al. (2001). Similar studies using prominence slabs embedded in the solar corona were undertaken by Soler et al. (2007) and Soler et al. (2009b).
5.1.1 Nonadiabatic magnetoacoustic waves in prominence slabs
Terradas et al. (2001) studied the radiative damping of quiescent prominence oscillations. They adopted a relatively simple nonadiabatic damping mechanism, by including a radiative loss term based on Newton’s law of cooling with constant relaxation time. The influence of this type of radiative dissipation on the normal modes of KippenhahnSchlüter and Menzel quiescent prominence models was analyzed. The normal modes of these configurations had previously been investigated by Oliver et al. (1992) and Joarder and Roberts (1993a); cf. Section 4.2. In a KippenhahnSchlüter prominence model, the fundamental slow mode is unaffected by radiation, but its harmonics are strongly damped. On the other hand, in a Menzel prominence configuration all slow modes are characterized by short damping times. The damping time depends on the curvature of field lines, in such a way that more curved models produce larger damping times. In both prominence models, fast modes are practically unaffected by radiative losses and have very long damping times.
A more involved analysis was performed by Soler et al. (2007) by including thermal conduction, optically thin or thick radiation, and heating in the energy equation. The prominence was modeled as a plasma slab embedded in an unbounded corona and with a magnetic field oriented along the direction parallel to the slab axis (see Figure 26); this is the equilibrium configuration of Joarder and Roberts (1992a), whose normal modes have been discussed in Section 4.2. Soler et al. (2007) found that radiation losses have a different effect on magnetoacoustic waves depending on their wavenumber. For typical values of observed wavelengths, the internal slow mode is attenuated by radiation from the prominence plasma, the fast mode by the combination of prominence radiation and coronal conduction and the external slow mode by coronal conduction. This study highlights the relevance of the coronal physical properties on the damping properties of fast and external slow modes, whereas this aspect does not affect the internal slow modes at all. For thin slabs, representing a fine thread, Soler et al. (2007) found that the fast mode is less attenuated, whereas both internal and external slow modes are not affected by nonadiabatic damping mechanisms.
Damping of magnetoacoustic waves in slab prominence models with a transverse magnetic field (see Figure 27 and Section 4.2 for a description of the normal modes) were studied by Soler et al. (2009b). The most relevant damping processes are coronal thermal conduction and radiative losses from the prominence plasma. In terms of the spatial distribution of the studied normal modes, it was found that both mechanisms govern together the attenuation of hybrid modes, whereas prominence radiation is responsible for the damping of internal modes and coronal conduction essentially dominates the attenuation of external modes. In terms of the different magnetohydrodynamic wave types, slow modes were found to be efficiently damped, with damping times compatible with observations. On the contrary, fast modes are less attenuated by nonadiabatic effects and their damping times are several orders of magnitude larger than those observed. The inclusion of the coronal medium in the analysis causes a decrease of the damping times compared to those of an isolated prominence slab, but this effect is still insufficient to obtain fast mode damping times compatible with observations.
5.1.2 Nonadiabatic magnetoacoustic waves in a single thread with mass flows
Soler et al. (2008) investigated the effects of both mass flow and nonadiabatic processes on the oscillations of an individual prominence thread modeled as an infinite homogeneous cylinder Figure 32). Thermal conduction and radiative losses were taken into account as damping mechanisms. For a discussion of the oscillatory features of this system, see Section 4.4.1.
The analysis of the damping timescales for the different wave types shows that slow and thermal modes are efficiently attenuated by nonadiabatic mechanisms. On the contrary, fast kink modes are much less affected and their damping times are much larger than those observed. These results are compatible with the known damping properties of these waves in the absence of flows.
In addition, Soler et al. (2008) analyzed how mass flows affect these damping properties. Figure 46 shows the dependence of the period, damping time, and their ratio as a function of the flow velocity for the slow, fast and thermal modes (for a discussion of the thermal mode, see Carbonell et al., 2009). Note that the left column of this figure has been already presented in Figure 33, but it is retained here to facilitate our explanation. Flow velocities in the range 0 – 30 km s^{1}, that correspond to the observed flow speeds in quiescent prominences, were considered. The damping time of slow and thermal modes is found to be independent of the flow velocity, but the attenuation of the fast kink mode is affected by the flow. The larger the flow velocity, the more attenuated the parallel fast kink wave, whereas the opposite occurs for the antiparallel solution. This behaviour is due to the weak coupling of the fast modes to external slow modes (Soler et al., 2008).
Although the presence of steady mass flows improves the efficiency of nonadiabatic mechanisms on the attenuation of transverse kink oscillations for propagation parallel to the flow, its effect is still not enough to obtain damping times compatible with observations.
5.1.3 Nonadiabatic magnetoacoustic waves in a twothread system with mass flows
The oscillatory properties, namely the frequency and spatial distribution, of fast and slow magnetoacoustic waves in a system made of two infinite threads with mass flows are described in Section 4.4.2; see Figure 37 for a sketch of the equilibrium configuration. Soler et al. (2009a) evaluated the damping timescales caused by nonadiabatic effects as a function of the distance between the thread axes. The left panel of Figure 47 shows that the ratio of the damping time to the period of the four kink modes is very large, so that dissipation by nonadiabatic mechanisms is not efficient enough to damp these modes. Hence, the collective nature of the transverse oscillations in a system of two identical threads does not change the conclusion about the irrelevance of thermal mechanisms to account for the damping of fast modes already obtained for one thread.
As concluded in Section 5.1.2, slow wave damping can be explained by thermal mechanisms. The right panel of Figure 47 shows the damping ratios of the S_{ z } and A_{ z } solutions versus the distance between the two threads. Slow modes in a threaded prominence are efficiently attenuated by nonadiabatic mechanisms. Note that τ_{d}/P is almost independent of the thread separation and the mode because the two threads oscillate independently in the S_{ z } and A_{ z } modes. Timescales τ_{d}/P ≈ 5 are obtained, which is in agreement with previous studies (Soler et al., 2007, 2008) and consistent with observations.
Soler et al. (2009a) concluded that collective slow modes are efficiently damped by thermal mechanisms, with damping ratios similar to those reported in observations, while collective fast waves are poorly damped. This is a key point since efficiently damped transverse oscillations have been observed, which could suggest that other attenuation mechanisms could be at work.
5.2 Damping of oscillations by ionneutral collisions
Since the temperature of prominences is typically of the order of 10^{4} K, the prominence plasma is only partially ionized. The exact ionization degree of prominences is unknown and the reported ratio of electron density to neutral hydrogen density (see, e.g., Patsourakos and Vial, 2002) covers about two orders of magnitude (0.1 – 10). Partial ionization brings the presence of neutrals in addition to electrons and ions, thus collisions between the different species are possible. Because of the occurrence of collisions between electrons with neutral atoms and ions, and more importantly between ions and neutrals, Joule dissipation is enhanced when compared with the fully ionized case. A partially ionized plasma can be represented as a singlefluid in the strong coupling approximation, which is valid when the ion density in the plasma is low and the collision time between neutrals and ions is short compared with other timescales of the problem. Using this approximation it is possible to describe the very low frequency and largescale fluidlike behaviour of plasmas (Goossens, 2003).
Partial ionization affects the induction equation, which contains additional terms due to the presence of neutrals and a nonzero resistivity (Soler et al., 2009d). These terms account for the processes of ohmic diffusion, with coefficient η; ambipolar diffusion, with coefficient η_{A}; and Hall’s magnetic diffusion, with coefficient η_{H}. They govern collisions between the different plasma species. Ohmic diffusion is mainly due to electronion collisions and produces magnetic diffusion parallel to the magnetic field lines; ambipolar diffusion is mostly caused by ionneutral collisions and Hall’s effect is enhanced by ionneutral collisions since they tend to decouple ions from the magnetic field, while electrons remain able to drift with the magnetic field (Pandey and Wardle, 2008). The ambipolar diffusivity can be expressed in terms of Cowling’s coefficient, η_{C}, that accounts for diffusion perpendicular to magnetic field lines, as
with B the magnetic field strength. For a fully ionized plasma, η_{C} = η and there is no ambipolar diffusion, so magnetic diffusion is isotropic. Due to the presence of neutrals, ηC ≫ η, which means that perpendicular magnetic diffusion is much more efficient than longitudinal magnetic diffusion in a partially ionized plasma. It is important to note that η_{C} ≫ η even for a small relative density of neutrals.
5.2.1 Homogeneous and unbounded prominence medium
Several studies have considered the damping of MHD waves in partially ionized plasmas of the solar atmosphere (De Pontieu et al., 2001; James et al., 2003; Khodachenko et al., 2004; Leake et al., 2005). In the context of solar prominences, Forteza et al. (2007) derived the full set of MHD equations for a partially ionized, onefluid hydrogen plasma and applied them to the study of the time damping of linear, adiabatic fast and slow magnetoacoustic waves in an unbounded prominence medium. This study was later extended to the nonadiabatic case by including thermal conduction by neutrals and electrons and radiative losses (Forteza et al., 2008). The main effects of partial ionization on the properties of MHD waves manifest through a generalized Ohm’s law, which adds some extra terms in the resistive magnetic induction equation, in comparison to the fully ionized case. Forteza et al. (2007) considered a uniform and unbounded prominence plasma and found that ionneutral collisions are more important for fast waves, for which the ratio of the damping time to the period is in the range 1 to 10^{5}, than for slow waves, for which values between 10^{4} and 10^{8} are obtained. Fast waves are efficiently damped for moderate values of the ionization fraction, while in a nearly fully ionized plasma, the small amount of neutrals is insufficient to damp the perturbations.
A hydrogen plasma was considered in the above studies, but 90% of the prominence chemical composition is hydrogen and the remaining 10% is helium. The effect of including helium in the model of Forteza et al. (2008) was assessed by Soler et al. (2010b). The species present in the medium are electrons, protons, neutral hydrogen, neutral helium (He i) and singly ionized helium (He ii), while the presence of He iii is neglected (Gouttebroze and Labrosse, 2009).
The hydrogen ionization degree is characterized by \(\tilde \mu H\), which varies between 0.5 for fully ionized hydrogen and 1 for fully neutral hydrogen. The helium ionization degree is characterized by \(\delta _{He} = \frac{{\xi _{He} II}} {{\xi _{He} I}}\), where ξ_{He II} and ξ_{He I} denote the relative densities of single ionized and neutral helium, respectively. Figure 48 displays τ_{d}/P as a function of the wavenumber, k, for the Alfvén, fast and slow waves, and the results corresponding to several helium abundances are compared for hydrogen and helium ionization degrees of \(\tilde \mu H\) = 0.8 and δ_{He} = 0.1, respectively. We can observe that the presence of helium has a minor effect on the results.
The thermal mode is a purely damped, nonpropagating disturbance (ω_{R} = 0), so only the damping time, τ_{d}, is plotted (Figure 48d). We observe that the effect of helium is different in two ranges of k. For k > 10^{4} m^{1}, thermal conduction is the dominant damping mechanism, so the larger the amount of helium, the shorter τ_{d} because of the enhanced thermal conduction by neutral helium atoms. On the other hand, radiative losses are more relevant for k < 10^{4} m^{1}. In this region, the thermal mode damping time grows as the helium abundance increases. Since these variations in the damping time are very small, we again conclude that the damping time obtained in the absence of helium does not significantly change when helium is taken into account. Therefore, the inclusion of neutral or single ionized helium in partially ionized prominence plasmas does not modify the behaviour of linear, adiabatic or nonadiabatic MHD waves already found by Forteza et al. (2007) and Forteza et al. (2008).
5.2.2 Cylindrical filament thread model
Soler et al. (2009c) applied the equations derived by Forteza et al. (2007) to the study of MHD waves in a partially ionized filament thread modeled as an infinite cylinder with radius a embedded in the solar corona (see Figure 32). As in Forteza et al. (2007), the onefluid approximation for a hydrogen plasma was considered. The internal and external media are characterized by their densities, temperatures, and their own relative densities of neutrals, ions and electrons. The contribution of the electrons is neglected. The coronal medium is considered as fully ionized, while the ionization fraction in the prominence plasma, \(\tilde \mu _p\), is allowed to vary.
In their analysis, Soler et al. (2009c) neglected Hall’s term since it can be ignored when the plasma is magnetized, i.e., when ions and electrons are tightly bound to the magnetic field. The condition to neglect Hall’s term can be written in terms of the iongyrofrequency (ω_{ i }) and the ionneutral collision time (τ) as ω_{ i }τ ≫ 1, which once expanded gives,
where Σ_{ in } is the ionneutral crosssection and n_{ n }n the neutrals number density (Leake et al., 2005; Pandey and Wardle, 2008). Using prominence conditions (ρ = 5 × 10^{11} kg m^{3}, B = 10 G, T = 8000 K, \(\tilde \mu _p\) = 0.8), we obtain the numerical value ω_{ i }τ = 467, which fully justifies the neglect of Hall’s term. Parallel and perpendicular magnetic diffusion can be evaluated by defining the corresponding Reynolds numbers as R_{m‖} = c_{sp}a/η and R_{m┴}= 4π^{2}c_{sp}/η_{C}k ^{2}_{ z } a, where the typical velocity scale has been associated to the sound speed in the prominence, c_{sp}. The parallel Reynolds number is independent of the wavenumber, while the relative importance of Cowling’s diffusion increases with k_{ z }, the longitudinal wavenumber. In the range of observed wavelengths (k_{ z }a ∼ [10^{3} – 10^{1}]) both Cowling’s and ohmic diffusion could therefore be important. Soler et al. (2009c) analyzed separately the effect(s) of partial ionization in Alfvén, fast kink and slow waves.
For torsional Alfvén waves, Soler et al. (2009c) found that wave propagation is constrained between two critical wavenumbers (top panels of Figure 49). These critical wavenumbers are, however, outside the range of the observed wavelengths, in which τ_{d}/P is in the range 10 – 100 and so is considerably larger than the observed damping rate. Nevertheless, a prominence ionization fraction larger than the maximum one considered here (namely \(\tilde \mu _p\) > 0.95) can yield τ_{d}/P = 1–10, in agreement with observations. For short wavenumbers, the values of the damping time over the period are independent of the ionization degree, while for large wavenumbers they become smaller for larger values of \(\tilde \mu _p\). This behaviour is explained in Soler et al. (2009c) by considering solutions to the dispersion relation in which one of the two possible damping mechanisms, i.e., partial ionization or ohmic dissipation, is neglected. Soler et al. (2009c) observed that ohmic diffusion dominates for small wavenumbers. Nevertheless, for large wavenumbers Cowling’s diffusion dominates over ohmic dissipation and so a larger number of neutrals decreases the damping time: the larger \(\tilde \mu\) in the thread, the shorter τ_{d} and, consequently, the smaller τ_{d}/P.
The presence of critical wavenumbers is also found in the case of transverse kink waves (middle panels of Figure 49). Within the range of observed wavelengths, the phase speed closely corresponds to its ideal counterpart, c_{k} = ω/k_{ z }, so nonideal effects are irrelevant for wave propagation. The behaviour of the damping rate as a function of wavelength and ionization fraction is seen to closely resemble the result obtained for Alfvén waves, with τ_{d}/P > 10 in the range of observed wavelengths. Therefore, neither ohmic diffusion nor ionneutral collisions seem to provide damping times as short as those observed for kink waves in filament threads. Only for an almost neutral plasma, with \(\tilde \mu _p\) > 0.95, the obtained damping rates are compatible with the observed timescales. Just like for Alfvén waves, ohmic diffusion dominates for small wavenumbers, while ionneutral collisions are the dominant damping mechanism for large wavenumbers.
Regarding slow waves (bottom panels of Figure 49), Soler et al. (2009c) concentrated their analysis on the radially fundamental mode with m = 1, since the behaviour of the slow mode is weakly affected by the value of the azimuthal wavenumber. Slow wave propagation is constrained by only one critical wavenumber, that strongly depends on the ionization fraction, in such a way that for k_{ z } below this critical wavenumber the wave is totally damped. More importantly, for large enough values of the ionization fraction, the corresponding critical wavelength lies in the range of observed wavelengths of filament oscillations. As a consequence, the slow wave might not propagate in filament threads under certain circumstances. As for the damping rate, it is found that ionneutral collisions are a relevant damping mechanism for slow waves, since very short damping times are obtained, especially close to the critical wavenumber. By comparing the particular effects of ohmic diffusion and ionneutral collisions, the slow mode damping is seen to be completely dominated by ionneutral collisions. Ohmic diffusion is found to be irrelevant, since the presence of the critical wavenumber prevents slow wave propagation for small wavenumbers, where ohmic diffusion would start to dominate.
5.3 Resonant damping of infinitely long thread oscillations
The phenomenon of resonant wave damping in nonuniform plasmas has been extensively studied in connection to wavebased coronal heating mechanisms (Ionson, 1978) and the damping of transverse coronal loop oscillations (Hollweg and Yang, 1988; Ruderman and Roberts, 2002; Goossens et al., 2002, 2010). The mechanism relies in the energy transfer from the transverse kink mode to small scale Alfvén waves because of the plasma inhomogeneity at the transverse spatial scales of the structures. This idea was put forward by Arregui et al. (2008b), whose analysis is restricted to the damping of kink oscillations due to the resonant coupling to Alfvén waves in a pressureless (zero plasmaβ) plasma. It was extended to the case in which both the Alfvén and the slow resonances are present by Soler et al. (2009e). Here we discuss the main results from these works, whose aim is to assess the damping properties of resonant absorption. For this reason, the considered configurations are based on the infinitely long thread model of Figure 31.
5.3.1 Resonant damping in the Alfvén continuum
Arregui et al. (2008b) considered an individual and isolated thread modeled as a cylindrical magnetic flux tube of radius a in a gravityfree environment. The uniform magnetic field points along the axis of the tube (Figure 50). In the zero plasmaβ approximation, the thread is modeled as a density enhancement with a radial variation of density from its internal constant prominence value ρ_{p} to the coronal constant value ρ_{c} over a nonuniform layer of thickness l. A typical value of the density contrast between the filament and coronal plasma is ζ = ρ_{p}/ρ_{c} = 200.
MHD waves of axisymmetric onedimensional cylindrical flux tubes are characterized by two wavenumbers, i.e., the azimuthal wavenumber, m, and the axial wavenumber, k_{ z }. They can have different nodes in the radial direction. Arregui et al. (2008b) concentrated their analysis on the radially and longitudinally fundamental transverse wave with azimuthal number m = 1, the kink mode. This eigenmode is consistent with the detected Doppler velocity variations (see Section 3.6.4) and their associated transverse motions, discussed in Section 4.4.1. The frequency of this mode is not influenced by the presence of a layer with small thickness, so the result of Section 4.4.1 is approximately correct; see Equation (22).
When transverse inhomogeneity is considered, the fundamental transverse kink mode resonantly couples to Alfvén waves. The consequence is the transfer of wave energy from the global transverse motion to azimuthal motions of localized nature, and thus the time damping of the kink mode (Goossens et al., 2009 1). Analytical expressions for the damping time scale can be obtained under the assumption that the transverse inhomogeneity lengthscale is small (l/a ≪ 1). This is the socalled thin boundary approximation. When the long wavelength and the thin boundary approximations are combined, the analytical expression for the damping time over period for the kink mode can be written as (see, e.g., Goossens et al., 1992, 1995; Ruderman and Roberts, 2002; Goossens et al., 2002)
Here F is a numerical factor that depends on the particular variation of the density in the nonuniform layer. For a linear variation, F = 4/π^{2} (Hollweg and Yang, 1988; Goossens et al., 1992); for a sinusoidal variation, F = 2/π (Ruderman and Roberts, 2002). Consider for example ζ = 200 as a typical density contrast and l/a = 0.1. Then, Equation (30) predicts a damping time of ∼ 6 times the oscillatory period, thus producing a timescale compatible with observations.
Quantitative parametric results for the damping of resonant kink waves in prominence threads as a function of the relevant parameters are provided by Arregui et al. (2008b). The accuracy of the analytical approximations is compared to full numerical results, beyond the long wavelength and thin boundary approximations. These results are shown in Figure 51. The damping is affected by the density contrast in the low contrast regime and τ_{d}/P rapidly decreases for increasing thread density (Figure 51a). Interestingly, τ_{d}/P stops depending on this parameter in the large contrast regime, typical of filament threads. The damping time over period is independent of the wavelength of perturbations (Figure 51b), but rapidly decreases with increasing inhomogeneity lengthscale (Figure 51c).
Resonant damping in the Alfvén continuum appears to be a very efficient mechanism for the attenuation of transverse thread oscillations, especially because large density contrasts and transverse plasma inhomogeneities are combined together.
5.3.2 Resonant damping in the slow continuum
Although the plasmaβ in solar prominences is probably small, it is definitely nonzero. Soler et al. (2009e) showed that, in prominence plasmas, resonant damping of kink waves can additionally be produced due to the coupling to slow continuum waves. In the context of coronal loops, which are presumably hotter and denser than the surrounding corona, the ordering of sound, Alfvén and kink speeds does not allow for the simultaneous matching of the kink frequency with both Alfvén and slow continuum frequencies. Because of their relatively higher density and lower temperature conditions, this becomes possible in the case of prominence threads. Therefore, the kink mode phase speed is also within the slow (or cusp) continuum, which extends between the internal and external sound speeds, in addition to the Alfvén continuum. By considering gas pressure in the cylindrical thread model of Arregui et al. (2008b), Soler et al. (2009e) evaluated the contribution of the damping due to the slow continuum to the total resonant damping of the kink mode.
Soler et al. (2009e) used the density model of Section 5.3.1 and the plasmaβ ≃ 0.04. In order to obtain an analytic expression for the damping rate of the kink mode, first the long wavelength and thin boundary limits were considered. In terms of the physically relevant quantities, the damping time over the period can be cast as
Here F is the same numerical factor as in Equation (30), while α_{A} = π(r_{A} – a)/l and α_{S} = π(r_{S} – a)/l, with r_{A} and r_{S} the Alfvén and slow resonant positions. The term with k_{ z } corresponds to the contribution of the slow resonance. If this term is dropped and m = 1 and cos α_{A} = 1 are taken, Equation (31) becomes Equation (30), that only takes into account the Alfvén resonance.
Equation (31) can now be directly applied to measure the relative contribution of each resonance to the total damping. To do that, Soler et al. (2009e) assumed r_{A} ≃ r_{S} ≃ a, for simplicity, so cos α_{A} ≃ cos α_{S} ≃ 1. The ratio of the two terms in Equation (31) is then
where τ_{dA} and τ_{dS} are the respective contributions of the Alfvén and slow resonances in Equation (31). A simple calculation shows that, for typical wavelengths of observed thread oscillations, the contribution of the slow resonance is irrelevant in front of that of the Alfvén resonance. Take for instance, m = 1 and k_{ z }a = 10^{2}, then Equation (32) gives τ_{dA}/τ_{dS} ≃ 10^{7}.
This analytical predictions were further confirmed by Soler et al. (2009e) by performing numerical computations outside the thin tube and thin boundary approximations. Figure 52 shows that the slow resonance is much less efficient than the Alfvén resonance. For the wavenumbers relevant to observed prominence oscillations, the value of τ_{d}/P due to the slow resonance is between 4 and 8 orders of magnitude larger than the same ratio obtained for the Alfvén resonance. The overall conclusion by Soler et al. (2009e) is that the slow resonance is very inefficient when it comes to damping the kink mode for typical prominence conditions and in the observed wavelength range. The damping times obtained with this mechanism are comparable to those due to the thermal effects discussed in Section 5.1. Hence, resonant damping of transverse thread oscillations is governed by the Alfvén resonance.
5.4 Resonant damping in partially ionized infinitely long threads
5.4.1 Temporal damping
Damping by resonant absorption in a partially ionized prominence plasma was studied by Soler et al. (2009d), who integrated both mechanisms in a nonuniform cylindrical prominence thread model in order to assess their combined effects. Partial ionization is relevant for the damping of short wavelength fast waves (Forteza et al., 2007), while resonant damping of kink waves is efficient whenever a transverse density inhomogeneity is present. The question arises on whether partial ionization affects the mechanism of resonant absorption and vice versa.
The model adopted by Soler et al. (2009d) has the magnetic and density structuring of the models used in Section 5.3 (see Figure 50), but the plasma properties are also characterized by the ionization fraction, \(\tilde \mu\). The radial behaviour of the ionization fraction in threads is unknown, so Soler et al. (2009d) assumed a onedimensional transverse profile akin to the one employed to model the equilibrium density. The thread ionization fraction, \(\tilde \mu _p\), is considered a free parameter and the corona is assumed to be fully ionized, so \(\tilde \mu _c\) = 0.5. The nonuniform transitional layer of thickness l therefore connects two plasmas with densities ρ_{p} and ρ_{c} and ionization degrees \(\tilde \mu _p\) and \(\tilde \mu _c\). Soler et al. (2009d) used the onefluid approximation and, for simplicity, the β = 0 limit, which excludes slow waves. The quantities η, η_{C} and η_{H} are here functions of the radial direction.
Soler et al. (2009d) first considered resonant damping in combination with Cowling’s diffusion and excluded Hall’s dissipation. They derived the following approximate expression for the damping ratio over the period, under the thin boundary approximation,
with \(\tilde \eta _{Cc,p} = \eta _C /v_{AC,p} a\) the coronal and prominence Cowling’s diffusivities in dimensionless form. Notice that Equation (33) reduces to Equation (30) in a fully ionized plasma, and is in agreement with Equation (31), in which the slow resonance is additionally included. In this expression, the term due to resonant damping is independent of the value of Cowling’s diffusivity and, therefore, of the ionization degree. The second term, related to the damping by Cowling’s diffusion, is proportional to k_{ z }, so its influence in the longwavelength limit is expected to be small. Soler et al. (2009d) performed a simple calculation by considering m = 1, k_{ z }a = 10^{2} and l/a = 0.2. This results in τ_{d}/P ≈ 3.18 for a fully ionized thread (\(\tilde \mu _p\) = 0.5) and τ_{d}/P ≈ 3.16 for an almost neutral thread (\(\tilde \mu _p = 0.95\) = 0.95). Thus, this approximate expression suggests that the ratio τ_{d}/P depends very slightly on the ionization degree, suggesting that resonant absorption dominates over Cowling’s diffusion.
The analytical estimates described above can be verified and extended by numerically solving the full eigenvalue problem. This approach allowed Soler et al. (2009d) to additionally include Hall’s diffusion in addition to ohmic and Cowling’s dissipation. In their study, these authors first considered a configuration with an abrupt density variation across the thread boundary (that is, l = 0), which prevents resonant absorption from working. Next, they included the thin transitional layer between the thread and the corona, so that both resonant absorption and ionneutral effects are at work.
For a homogeneous thread (l/a = 0), Soler et al. (2009d) computed the damping rate for different ionization degrees (see Figure 53). In agreement with the results displayed for the kink mode in Figure 49, τ_{d}/P has a maximum at the transition between the ohmicdominated regime, which is almost independent of the ionization degree, to the region where Cowling’s diffusion is more relevant and the ionization degree has a significant influence. The approximate analytical solution for a given value of \(\tilde \mu _p\) agrees very well with the numerical solution in the region where Cowling’s diffusion dominates, while it significantly diverges from the numerical solution in the region where ohmic diffusion is relevant. Within the range of typically reported wavelengths, τ_{d}/P is between 1 and 2 orders of magnitude larger than the measured values, so neither ohmic nor Cowling’s diffusion can account for the observed damping time.
For the inhomogeneous thread case (l/a ≠ 0), Figure 54a displays some relevant differences. First, the damping time is dramatically reduced for intermediate values of k_{ z }a, which include the region of typically observed wavelengths. In this region, the ratio τ_{d}/P becomes smaller as l/a is increased, a behaviour consistent with damping by resonant absorption. The inclusion of the inhomogeneous transitional layer removes the smaller critical wavenumber and consequently the kink mode exists for very small values of k_{ z }a Figure 54a also shows a very good agreement between the numerical and the approximate solutions, this one given by Equation (33), for wavenumbers above k_{ z }a ∼ 10^{4}, and a poor agreement in the range for which ohmic diffusion dominates, below k_{ z }a ∼ 10^{4}. To understand this behaviour one has to bear in mind that the analytic approximate solution includes the effects of resonant absorption and Cowling’s diffusion, but not the influence of ohmic diffusion. Such as shown in Figure 54b, the ionization degree is only relevant for large wavenumbers, where the damping rate significantly depends on the ionization fraction through ohmic diffusion.
Figure 55 displays the ranges of k_{ z }a for which Cowling’s and Hall’s diffusion dominate. Hall’s diffusion is irrelevant in the whole range of k_{ z }a studied by Soler et al. (2009d), while Cowling’s diffusion dominates the damping for large k_{ z }a. In the whole range of relevant wavelengths, resonant absorption is the most efficient damping mechanism and the damping time is independent of the ionization degree, as predicted by the analytical result (Equation [33]). On the contrary, ohmic diffusion dominates for very small k_{ z }a. In this region, the damping time related to Ohm’s dissipation becomes even shorter than that due to resonant absorption, which means that the kink wave is mainly damped by ohmic diffusion.
5.4.2 Spatial damping
Motivated by the spatially damped propagating waves observed by Terradas et al. (2002) (see Section 3.6.3), the spatial damping of linear nonadiabatic magnetohydrodynamic waves in a homogenous, unbounded, magnetized, and fully ionized plasma was studied by Carbonell et al. (2006). The spatial damping in a flowing partially ionized plasma has been studied by Carbonell et al. (2010). Carbonell et al. (2006) found that the thermal (fast) wave shows the strongest (weakest) spatial damping. For periods longer than 1 s the spatial damping of magnetoacoustic waves is dominated by radiation, while at shorter periods the spatial damping is dominated by thermal conduction. Therefore, radiative effects on linear magnetoacoustic slow waves can be a viable mechanism for the spatial damping of short period prominence oscillations, while thermal conduction does not play any role. On the other hand, Carbonell et al. (2010) found that in the presence of a background flow, new strongly damped fast and Alfvén waves appear whose features depend on the joint action of flow and resistivity. The damping lengths of adiabatic fast and slow waves are strongly affected by partial ionization, which also modifies the ratio between damping lengths and wavelengths. For nonadiabatic slow waves, the unfolding in both wavelength and damping length induced by the flow allows efficient damping for periods compatible with those observed in prominence oscillations. In the case of nonadiabatic slow waves and within the range of periods of interest for prominence oscillations, the joint effect of both flow and partial ionization leads to efficient spatial damping of oscillations. For fast and Alfvén waves, the most efficient damping occurs at very short periods not compatible with those observed in prominence oscillations.
Using the same equilibrium model as in Soler et al. (2009d) (see Figure 50), whose results have been presented in Section 5.4.1, Soler et al. (2011) investigated the spatial damping of propagating kink MHD waves in transversely nonuniform and partially ionized prominence threads. The damping mechanisms are resonant absorption and ionneutral collisions (Cowling’s diffusion). In the absence of transitional layer, i.e., when the damping is due to Cowling’s diffusion exclusively, the nondimensional wavelength, the damping length, L_{D}, and the ratio of the damping length to the wavelength are displayed in Figure 56. Regarding the wavelength, we see that the effect of Cowling’s diffusion is only relevant for periods much shorter than those observed (1 – 10 min, corresponding to 40 ≤ P/τ_{Ap} ≤ 400, with τ_{Ap} = a/v_{Ap} the thread Alfvén travel time). On the other hand, an almost neutral plasma, i.e., \(\tilde \mu _p\) → 1, has to be considered to obtain an efficient damping and to achieve small values of the damping ratio within the relevant range of periods. Such very large values of \(\tilde \mu _p\) are probably unrealistic (Labrosse et al., 2010).
For resonantly damped modes, Figure 57 shows the results for different values of the thickness of the layer and fixed ionization degree. Figure 58 displays the results for different values of the ionization degree and a fixed transverse inhomogeneity length scale. Since the wavelength is not affected by the value of l/a and has the same behaviour as in Figure 56a, both Figures 57 and 58 focus on L_{D}/a and L_{D}/λ. Depending on the period, two different behaviours of the solutions are obtained. For short periods, the damping length is independent of the layer thickness and is governed by the value of the ionization degree. On the contrary, for large periods, the damping length depends on the value of l/a, but is independent of the ionization degree. This result indicates that resonant absorption dominates the damping for large periods, whereas Cowling’s diffusion is more relevant for short period oscillations. In addition, we can observe that the approximate transitional period for which the damping length by Cowling’s diffusion becomes shorter than that due to resonant absorption is much lower than the typically observed periods. This shows that resonant absorption is the dominant damping mechanism in the relevant range. The analytical approximation for the damping ratio obtained by Soler et al. (2011) provides an accurate description of the kink mode spatial damping in the relevant range of periods, such as shown by the diamonds in Figures 56 and 57.
For typically reported periods of thread oscillations, resonant absorption is an efficient mechanism for the kink mode spatial damping, while ionneutral collisions have a minor role. Cowling’s diffusion dominates both the propagation and damping for periods much shorter than those observed, while resonant absorption could explain the observed spatial damping of kink waves in prominence threads.
5.5 Resonant damping in partially ionized finite length threads
The results described in Sections 5.3, 5.4.1, and 5.4.2 indicate that, because of the coupling of kink waves to Alfvén waves, resonant absorption constitutes a very plausible mechanism for the explanation of the observed spatial and time decay of transverse oscillations. The main limitation of these studies is that they adopt a onedimensional density model that might not be appropriate in view of the longitudinal structuring of prominence threads. This led Soler et al. (2010a) to investigate the time damping properties of twodimensional thread models, that is, with density inhomogeneity across the thread and along the magnetic tube in which it is contained. In this study, resonant absorption and damping by partial ionization effects were considered simultaneously.
Soler et al. (2010a) (see Figure 59) modeled a prominence fine structure as a straight cylindrical magnetic tube only partially filled with the cold and dense material. The length of the dense part is L_{p}. The thread may either occupy the centre of the magnetic tube or be displaced, so that the lengths of both evacuated parts of the tube are different. By denoting the lengths of the right and left handside evacuated regions as L ^{+}_{e} e and L ^{}_{e} , one has L ^{+}_{e} = L – L ^{}_{e} – L_{p}, with L the full length of the tube. Just like in the works discussed in Section 5.4, the prominence plasma is partially ionized and a transverse inhomogeneous transitional layer is included between the prominence thread and the coronal medium. Ionneutral collisions and resonant absorption are the considered damping mechanisms. The main model improvements in comparison to the thread model by Díaz et al. (2002), discussed in Section 4.5 (see Figure 41), are the ability to model noncentered threads, the inclusion of a nonuniform transverse layer and partial ionization of the thread plasma.
First, damping by Cowling’s diffusion alone is considered by setting l = 0. When the thread is located in the center of the tube the ratio of the damping time to the period is given by the approximate expression
with \(\tilde \eta _{Cp} = \eta _C /v_{Ap} a\) the filament Cowling’s diffusivity in dimensionless form. For ρ_{p}/ρ_{c} = 200, L_{p}/L = 0.1 and L = 10^{5} km, Equation (34) gives τ_{d}/P ≈ 5 × 10^{3} for \(\tilde \mu _p\) = 0.8 and τ_{d}/P ≈ 150 for \(\tilde \mu _p\) = 0.99. Therefore, in a transversally homogeneous thread, an almost neutral prominence plasma is needed, i.e., \(\tilde \mu _p\) ≈ 1, for the damping due to Cowling’s diffusion to be efficient. Although the precise ionization degree is unknown, such large values of are probably unrealistic in the context of prominences.
Next, Soler et al. (2010a) considered l/a ≠ 0, so that both resonant absorption and Cowling’s diffusion can cause wave damping. An approximate expression for the damping ratio for a sinusoidal density variation in the transitional layer is
As a numerical example, in the case m = 1, L_{p}/L = 0.1, L = 10^{7} m and l/a = 0.2, the damping ratio is τ_{d}/P ≈ 3.18 for a fully ionized thread (\(\tilde \mu _p\) = 0.5) and τ_{d}/P ≈ 3.16 for an almost neutral thread (\(\tilde \mu _p\) = 0.95). Note that the obtained damping times are consistent with the observations. Moreover, as seen in Section 5.4.1, the contribution of resonant absorption to the damping is much more important than that of Cowling’s diffusion, so the ratio τ_{d}/P depends only very slightly on the ionization degree and the second term on the righthand side of Equation (35) can in principle be neglected.
When the prominence region is not at the center of the tube, and assuming l = 0, an approximate expression for the damping ratio is
Taking the limits L ^{}_{e} → 0 or L ^{+}_{e} → 0 in this expression, it can be shown that the minimum value of the damping ratio by Cowling’s diffusion takes place when the prominence region is located at the magnetic tube center (L ^{}_{e} = L ^{+}_{e} ).
Soler et al. (2010a) find that for l ≠ 0 and under the thin tube and thin boundary approximations, the period and damping time by resonant absorption have the same dependence on L ^{}_{e} and L ^{+}_{e} . This means that for resonant absorption the damping ratio does not depend on these quantities. Since resonant damping dominates over Cowling’s diffusion, this leads to the conclusion that when considering both damping mechanisms, the damping ratio will be almost unaffected by the position of the prominence region within the fine structure.
The accuracy of the above analytical solutions can be assessed by numerically solving the general dispersion relation derived by Soler et al. (2010a). Here we only show the results obtained by Soler et al. (2010a) for the case in which the prominence thread is centered in the tube.
In the case without transverse transitional layer, l/a = 0, damping is only due to Cowling’s diffusion. Figure 60a displays the period as a function of L_{p}/L for different values of the ionization degree in the prominence region, whereas Figure 60b shows the corresponding values of the damping time. As can be seen, the period increases when the length of the thread is increased and tends to the value for a homogeneous prominence cylinder when L_{p}/L → 1. In addition, the period is independent of the ionization degree. On the contrary, the damping time strongly depends on the ionization degree, and for a fixed \(\tilde \mu _p\) it slightly increases as L_{p}/L becomes larger. In all solutions, the analytical expressions for the period and the damping time are in agreement with the solution of the full dispersion relation for realistic, small values of L_{p}/L, i.e., L_{p}/L ≤ 0.4, whereas the approximate expressions diverge from the actual solution when the prominence region occupies most of the magnetic tube. Figure 60c displays τ_{d}/P versus L_{p}/L. The numerical solution shows little dependence on L_{p}/L, while the analytical approximation (Equation [34]) diverges from the numerical value in the limit of large L_{p}/L. Given the obtained large values of τ_{d}/P, Soler et al. (2010a) concluded that the efficiency of the damping due to Cowling’s diffusion in a partially filled flux tube does not improve with respect to the longitudinally homogeneous tube case shown in Section 5.4.1.
Next, Soler et al. (2010a) included resonant damping. The period and the damping time of the fundamental kink mode were computed as a function of the different parameters, namely \(\tilde \mu _p\), l/a, and L_{p}/L. Regarding the period, Soler et al. (2010a) found that both its value and its dependence on L_{p}/L are the ones plotted in Figure 60a because the period is almost independent \(\tilde \mu _p\) and l/a. For a fixed ionization degree of \(\tilde \mu _p\), the damping time decreases with l/a. The approximate analytical estimate of the damping time is in good agreement with the full solution for L_{p}/L below 0.4. In order to assess the efficiency of resonant damping, Figure 61b displays the corresponding values of τ_{d}/P. In comparison with the damping ratio by Cowling’s diffusion (see Figure 60c), much smaller values of ..d/.. are now obtained. The damping ratio is almost independent of the length of the thread. This is because, under the assumptions made by Soler et al. (2010a), the dependence of the period and damping time on the length of the thread is the same. Overall, a very good agreement is obtained between the numerical result and the analytical approximation, even for large values of the length of the thread.
In summary, the dominant damping mechanism is resonant absorption, which provides damping ratios in agreement with the observations, whereas ionneutral collisions are irrelevant for the damping. The values of the damping ratio are independent of both the prominence thread length and its position within the magnetic tube, and coincide with the values for a tube fully filled with the prominence plasma. A recent study that further analyses resonant damping of thread oscillations in twodimensional equilibrium models can be found in Arregui et al. (2011). These authors additionally analyzed the influence of the density in the evacuated part of the thread. This quantity is seen to influence periods and damping times, but has little influence on the damping rate of transverse thread oscillations. The implications of some of these results for the determination of physical properties in transversely oscillating threads are discussed in Section 6.
5.6 Damping by wave leakage
The solutions obtained for the oscillations of prominence line current models (van den Oord and Kuperus, 1992; Schutgens, 1997a,b; van den Oord et al., 1998) mentioned in Section 4.3 suggest the existence of time amplification and damping of the studied oscillations. While the amplification should be linked to a prominence destabilization, the attenuation seems to be very efficient for many of the considered parameter values, and the ratio of the damping time to the period is between 1 and 10 (i.e., in agreement with observations). This indicates that the oscillations are efficiently damped (Figure 62a). On the other hand, in the prominence model used by Schutgens and Tóth (1999) vertical oscillations are very efficiently attenuated for all the parameters considered and the same happens with horizontal oscillations (Figure 62b) for coronal densities above ≃ 5 × 10^{13} kg m^{3}. These constraining properties of damped horizontal and vertical oscillations could be used for prominence seismology.
However, the exact nature of the damping mechanism should be pointed out, and Schutgens and Tóoth (1999) suggest that the damping of oscillations is due to the emission of waves by the prominence, i.e., wave leakage. The damping of horizontal motions is attributed to the emission of slow waves, whereas fast waves are invoked as the cause of the damping of vertical motions. Taking into account that the main difference between this work and those of van den Oord and Kuperus (1992), Schutgens (1997a,b), and van den Oord et al. (1998) lies essentially in the cross section of the filament, it seems that the physics involved should be the same, so wave leakage should be the mechanism responsible for the accounted damping. However, in Schutgens and Tóoth (1999), the plasmaβ in the prominence ranges from β > 1 in its central part to β < 0.1 at its boundary. Hence, waves emitted by the prominence into the corona propagate in a β ≪ 1 environment in which magnetic field lines are closed. Under these conditions, slow modes propagate along magnetic field lines and are unable to transfer energy from the prominence into the corona and so wave leakage in the system studied by Schutgens and Tóoth (1999) is only possible by fast waves. Then, it is hard to understand how the prominence oscillations can be damped by the emission of slow waves in this particular model, in which the dense, cool plasma is only allowed to emit fast waves. It must be mentioned, however, that the plasma.. in the corona increases with the distance from the filament, which implies that the emitted fast waves can transform into slow waves when they traverse the β ≃ 1 region. This effect has been explored by McLaughlin and Hood (2006) and McDougall and Hood (2007); see also references therein for similar studies.
6 Prominence Seismology
Solar atmospheric seismology aims to determine physical parameters that are difficult to measure by direct means in magnetic and plasma structures. It is a remote diagnostics method that combines observations of oscillations and waves in magnetic structures, together with theoretical results from the analysis of oscillatory properties of given theoretical models. The philosophy behind this discipline is akin to that of Earth seismology, the sounding of the Earth interior using seismic waves, and helioseismology, the acoustic diagnostic of the solar interior. It was first suggested by Uchida (1970) and Roberts et al. (1984), in the coronal context, and by TandbergHanssen (1995) in the prominence context. The increase in the number and quality of high resolution observations in the 1990s has lead to the rapid development of solar atmospheric seismology. In the context of coronal loop oscillations, recent applications of this technique have allowed the estimation and/or restriction of parameters such as the magnetic field strength (Nakariakov and Ofman, 2001), the Alfvén speed in coronal loops (Zaqarashvili, 2003; Arregui et al., 2007a; Goossens et al., 2008), the transversal density structuring (Goossens et al., 2002; Verwichte et al., 2006) or the coronal density scale height (Andries et al., 2005; Verth et al., 2008).
The application of inversion techniques to prominence seismology is less developed. This is due to the complexity of these objects in comparison to, e.g., coronal loops. The recent refinement of theoretical models that incorporate the fine structuring of prominences and the high resolution observations of small amplitude oscillations have produced an increase in prominence seismology studies. Several techniques for the inversion of physical parameters have been developed that make use of observational estimates for quantities such as phase velocities, periods, damping times, and flow speeds. In general, the solution to the inverse problem cannot provide a single value for all the physical parameters of interest. However, important information about unknown physical quantities can be obtained using this method. The most relevant results of the MHD prominence seismology technique are here discussed.
The theoretical models decribed in Section 4 make use of different conceptual views of prominences, such as the string model, the slab model, and the thread model for their fine structure. Seismology efforts in the area have followed the same pattern. We describe them in increasing intricacy order, starting with a mechanical analogue (Section 6.1), followed by slab models (Section 6.2), and ending with the seismology of fine structure oscillations (Sections 6.3 to 6.6).
6.1 Seismology of large amplitude prominence oscillations
Several studies have made use of the observed characteristics of large amplitude oscillations in prominences to deduce physical parameters of these objects. The classic example is the interpretation by Hyder (1966) of the winking filament phenomenon in terms of a global mode of the prominence. This author modeled the eleven winking filament events reported by Ramsey and Smith (1965) as damped harmonic oscillators and obtained estimates of the vertical magnetic field strength in the range 2 – 30 G. More recent studies have also used large amplitude oscillations in filaments to deduce the magnetic field strength in these objects.
Vršnak et al. (2007) reported on Hα observations of periodical plasma motions along the axis of a filament. The motions were both large amplitude and large scale, with an initial displacement of 24 Mm, an initial velocity amplitude of 51 km s^{1}, a period of 50 min, and a damping time of 115 min. Oscillations were interpreted as a global mode of the system and the driver was thought to be the magnetic flux injection by magnetic reconnection at one of the filament legs. Although oscillatory motions along the prominence axis were also reported by Jing et al. (2003, 2006), the study by Vršnak et al. (2007) proposes an explanation for the triggering process and the restoring force, and performs diagnostics based on these interpretations.
The seismology analysis by Vršnak et al. (2007) is based on the fitting of the oscillation properties to a mechanical analogue model in terms of the classic damped harmonic oscillator equation. This analogue is first used to discard gas pressure as the restoring force, since it leads to sound speed values one order of magnitude larger than those corresponding to the typical temperature of prominence plasmas, and no signature of plasma at those temperatures was observed in TRACE EUV images. In this work a twisted flux rope model with both axial and azimuthal magnetic field components was considered and an excess azimuthal field at one of the prominence legs was assumed. This gives rise to a magnetic pressure gradient and a torque, which in turn drive a combined axial and rotational motion of the plasma. Next, an expression that relates the azimuthal Alfvén speed, v_{ Aϕ }, and the oscillatory period was obtained. From this relation, the Alfvén speed v_{ Aϕ } ∼ 100 km s^{1} was inferred. By further assuming that the number density of the prominence plasma is in the range 10^{10} – 10^{11} cm^{3}, the azimuthal magnetic field strength results in the range 5 – 15 G. By measuring the pitch angle, Vršnak et al. (2007) additionally determined the internal structure of the flux rope helical magnetic field, from which the axial magnetic field strength was estimated to be in the range 10 – 30 G.
The twisted flux rope model was also invoked by Pintér et al. (2008) in their analysis of SoHO EUV observations of large amplitude transverse oscillations in a polar crown filament previously studied by Isobe and Tripathi (2006). Oscillations were present along a foot belonging to a larger prominence structure and occurred prior to the eruption of the full structure. Wavelet analysis tools were used to shed light into the temporal and spatial behaviour of oscillations. The filament oscillated as a rigid body with a period of 2.5 h, that was constant along the filament, but decreased in time. The lineofsight velocity was estimated to be about a few tens of km s^{1}. The analysis of the spatial properties of the oscillations shows evidence of a global standing transverse oscillation, although some small scale oscillations within the structure cannot be discarded. Using the twisted flux rope model for the filament and based on the same scenario and analysis as Vršnak et al. (2007), the azimuthal Alfvén speed component was estimated to be v_{ Aϕ } = 49 km s^{1} and the axial magnetic field strength in the range 2 – 10 G. In this case, the pitch angle could not be measured. By assuming a mean value of 65°, Pintér et al. (2008) estimated that the axial component of the magnetic field must be in the range 1 – 5 G.
6.2 Seismology of prominence slabs
The MHD wave properties for slab models of prominences are described in Section 4.2. Two relevant studies have made use of some of these models to infer physical properties in prominences. Their methodology is based on the identification of observed oscillations with theoretical eigenmodes.
Régnier et al. (2001) consider the possible theoretical modes that can explain their observations of oscillations in an active region filament. The slab model with a uniform and inclined magnetic field by Joarder and Roberts (1993b) is used (see Figure 29). The dispersion relations for Alfvén modes and magnetoacoustic modes are considered. They provide the frequency of six fundamental modes: the symmetric Alfvén, slow and fast kink modes and the antisymmetric Alfvén, slow and fast sausage modes, as a function of the prominence parameters. Observations provide with estimates for the width (8000 km) and length (63,000 km) of the filament. Assumptions on other parameters, such as the temperature of the filament (8000 K) and of its environment (106 K), the density of the slab (10^{12} cm^{3}), the magnetic field strength (20 G) and for the angle between the magnetic field and the long axis of the slab (25°) are made. The dispersion relations are then solved by using these parameters and the corresponding periods are obtained and classified.
Observations and Fourier analysis of Doppler velocity time series enable Régnier et al. (2001) to detect intermediate (between 5 and 20 min in this case) and long (> 40 min) period oscillations. From the comparison between the observed and calculated frequencies, an identification method of the oscillation modes in the observed filament is presented. The method makes use of the fact that the frequency ratio of the fundamental even Alfvén mode to the fundamental odd Alfvén mode only depends on the ratio of the halfwith of the slab to the halflength of the filament. This quantity is measurable. The same applies to the frequency ratios involving the slow kink/sausage and fast kink/sausage modes. Parametric calculations for the frequencies as a function of the magnetic field strength and the inclination angle, while keeping the slab density constant, are next performed. A diagnostic of the observed filament is obtained by looking for the parameters values that enable the matching of theoretical and observed frequencies. By following this method, the angle between the magnetic field and the long axis of the slab is estimated to be 18°. Using this value, an algebraic relation for the magnetic field strength as a function of the slab density is derived.
A more involved and ambitious diagnostic, using the Joarder and Roberts (1993b) slab model, was performed by Pouget et al. (2006). The long duration and high temporal resolution observations with CDS/SoHO enable these authors to detect and measure the entire range of periodicities theoretically expected in a filament. In particular both the short (less that 10 min) and the long ones (more than 40 min) are detected.
The detailed analysis of three filaments is presented. The seismic inversion technique closely follows that by Régnier et al. (2001), in the sense that the first step towards the diagnostic is the use of frequency ratios between fundamental even/odd (kink/sausage) modes. These ratios only depend on the ratio of the filament halfwidth to its halflength. Once this ratio is measured, with a given uncertainty, Pouget et al. (2006) assume that their 16h long observation has allowed them to observe the six modes of interest, since the slowest mode is expected at a period of 5 h, for standard prominence parameters.
The inversion method first assigns a possible triplet of measured frequencies to the 3 odd fundamental frequencies (odd Alfvén, slow sausage, and fast sausage modes). The coherence of each choice is examined against two tests. The first requires to find three corresponding even frequencies, with the condition that the even/odd frequency ratios are consistent with the measured halfwidth to halflength ratio. The second involves the inferred values for the density, temperature, magnetic field inclination angle, and magnetic field strength to be consistent with typical values reported in the literature. For each test, if the test was negative, the full triplet was changed and the series started again. On the contrary, if the tests succeeded, Pouget et al. (2006) considered that the six fundamental modes were identified.
The three filament observations led to coherent diagnostics and a single possible set of frequencies was found for each observation. The importance of this study is its ability to simultaneously determine the values of the inclination angle, temperature, and Alfvén speed for the same prominence. The drawback is that the modeling, as in Régnier et al. (2001), does not permit to capture the highly inhomogeneous nature of prominences.
6.3 Seismology of propagating transverse thread oscillations
Transverse thread oscillations observed by Lin et al. (2009) and discussed in Section 3.6.4 show evidence of waves propagating along individual threads. Ten of the swaying threads were chosen by Lin et al. (2009) for further investigation, and for each selected thread two or three perpendicular cuts were made in order to measure the properties of the propagating waves. Periods and amplitudes of the waves, as well as their phase velocity, were derived for each thread. Lin et al. (2009) interpreted the observed events as propagating MHD kink waves supported by the thread body. This mode is the only one producing a significant transverse displacement of the cylinder axis. In addition, it also produces shortperiod oscillations of the order of minutes, compatible with the observed periods (see Section 4.4.1).
If an infinitely long, straight, cylindrical thread model, with the tube fully filled with cool and dense material (Figure 31), is assumed, a comparison between the observed wave properties and the theoretical prediction can be made. This enabled Lin et al. (2009) to obtain estimates for some physical parameters of interest, namely the Alfvén speed and the magnetic field strength in the studied threads. To this end, the observed phase velocity was directly associated to the kink speed
where Equation (22) for the kink frequency has been used. In this expression v_{Ap} is the Alfvén speed in the prominence thread and ζ = ρ_{p}/ρ_{c} is the density contrast. Both quantities are unknown, hence no unique solution to Equation (37) can be obtained from the observed period alone. In the limit of high density contrast, typical of prominence plasmas, the ratio ρ_{p}/ρ_{c} is very large and the ratio c ^{2}_{k} /v ^{2}_{Ap} is almost independent from it (see Figure 63a). The kink speed can then be approximated by
Lin et al. (2009) assumed that thread oscillations observed from the Hα sequences were the result of a propagating kink mode, which implies that the measured phase velocity, c_{p}, is equal to the kink speed. Then, the thread Alfvén speed can be computed from
The inferred values of v_{Ap} for the ten selected threads are displayed in Table 2 in Lin et al. (2009). The results show a strong dispersion, suggesting that the physical conditions in different threads were very different in spite of belonging to the same filament. This result clearly reflects the highly inhomogeneous nature of solar prominences. Once the Alfvén speed in each thread was determined, the magnetic field strength could be computed after a value for the thread density was assumed. For the analyzed events, and considering a typical value ρ_{p} = 5 × 10^{11} kg m^{3}, magnetic field strengths in the range 0.9 – 3.5 G were obtained (see Figure 63b).
6.4 Seismology of damped transverse thread oscillations
A feature clearly observed by Lin et al. (2009) is that the amplitudes of the waves passing through two different cuts along a thread are notably different. Apparent changes can be due to damping of the waves in addition to noise in the data. The damping of prominence oscillations is a common feature in many observed events and damping timescales provide an additional source of information that can be used when performing parameter inference using seismology inversion techniques, once a physical model that provides an explanation is available. Among the different damping mechanisms described in Section 5, resonant absorption in the Alfvén continuum seems a very plausible one and has been used to perform prominence thread seismology, using the damping as an additional source of information. In the context of coronal loop seismology, the use of damping rates in combination with oscillatory periods gives information about the transverse density structuring of coronal loops (Goossens et al., 2002; Arregui et al., 2007a; Goossens, 2008; Goossens et al., 2008).
The model considered here is an infinitely long thread of radius a surrounded by a thin transition sheath of thickness l in which a smooth transition from the thread to the coronal density takes place (see Figure 50). For standing kink waves, and without using the thin tube and thin boundary approximation, the normal mode period and damping ratio are functions of the relevant equilibrium parameters,
with v_{Ap} the prominence thread Alfvén speed. Note that in the thin tube and thin boundary approximations (Equation (23) for P and Equation (30) for the damping ratio), the period does not depend on l/a and the damping ratio is independent of the wavelength. This is not true in the general case (Arregui et al., 2008b). The period is a function of the longitudinal wavenumber, k_{ z }, the transverse inhomogeneity lengthscale, l/a, and the internal Alfvén speed. Similarly for the damping ratio, except for the fact that it cannot depend on any timescale. The long wavelength approximation further eliminates the k_{ z } dependence of the damping ratio. In the case of coronal loop oscillations, an estimate for k_{ z } can be obtained directly from the length of the loop and the fact that the fundamental kink mode wavelength is twice this quantity. For prominence threads, the wavelength of oscillations needs to be measured. Relations (40) indicate that, if no assumption is made on any of the physical parameters of interest, there are infinite different equilibrium models that can equally well explain the observations (namely the period and damping ratio). The parameter values that define these valid equilibrium models are displayed in Figure 64a, where the analytical algebraic expressions in the thin tube and thin boundary approximations by Goossens et al. (2008) have been used to invert the problem. It can be appreciated that, even if an infinite number of solutions is obtained, they define a rather constrained range of values for the thread Alfvén speed. Because of the insensitiveness of the damping rate with the density contrast for the typically large values of this parameter in prominence plasmas, the obtained solution curve displays an asymptotic behaviour for large values of ζ. This makes possible to obtain precise estimates for the thread Alfvén speed, v_{Ap} ≃ 12 km s^{1}, and the transverse inhomogeneity length scale, l/a ≃ 0.16. Note that these asymptotic values can directly be obtained by inverting Equations (23) and (30) for the period and the damping rate in the limit ζ → ∞. The computation of the magnetic field strength from the obtained seismological curve requires the assumption of a particular value for either the filament or the coronal density. The resulting curve for a typical coronal density is shown in Figure 64b. Precise values of the magnetic field strength cannot be obtained, unless the density contrast is accurately known.
The transverse inhomogeneity length scale of an oscillating thread could also be estimated by using observations of spatial damping of propagating kink waves and theoretical results described in Section 5.4.2. In the context of coronal loops, Terradas et al. (2010) have shown that the ratio of the damping length to the wavelength, due to resonant damping of propagating kink waves, has the same dependence on the density contrast and transverse inhomogeneity lengthscale as the ratio of the damping time to the period for standing kink waves. Similar inversion techniques to the ones explained here for the temporal damping of oscillations could be applied to the spatial damping of propagating waves.
The main downside of the technique just described is the use of thread models in which the full magnetic tube is filled with cool and dense plasma. The solution to the forward problem in the case of twodimensional thread models is discussed in Section 5.5. The analytical and numerical results obtained by Soler et al. (2010a) using these models indicate that the length of the thread and its position along the magnetic tube influence the period and damping time of transverse thread oscillations. On the contrary, the damping ratio is rather insensitive to these model properties.
Going back to the inversion curve displayed in Figure 64a, we notice that a change in the period produces a vertical shift of the solution curve, hence the period influences the inferred values for the Alfvén speed. On the other hand, the damping ratio determines the projection of the inversion curve onto the (ζ, l/a)plane. We can conclude that ignorance of the length of the thread or the length of the supporting magnetic flux tube will have a significant impact on the inferred values for the Alfvén speed (hence magnetic field strength) in the thread. On the contrary, because of the smaller sensitivity of the damping ratio to changes in the longitudinal density structuring, seismological estimates of the transverse density structuring will be less affected by our ignorance about the longitudinal density structuring of prominence threads.
An example of the inversion of physical parameters for different values of the thread length was presented by Soler et al. (2010a). When partially filled threads, i.e., with the dense part occupying a length L_{p} shorter than the total length of the tube L, are considered, one curve is obtained for each value of the length of the thread. The solutions to the inverse problem are shown in Figure 65a for a set of values of L_{p}. Even if each curve gives an infinite number of solutions, again each of them defines a rather constrained range of values for the thread Alfvén speed. The figure shows that the ratio L_{p}/L is a fundamental parameter in order to perform an accurate seismology of prominence threads, since different curves produce different estimates for the prominence Alfvén speed, as anticipated above. Because of the insensitiveness of the damping ratio with respect to the length of the thread, all solution curves for different lengths of the threads produce the same projection onto the (ζ, l/a)plane. Hence, the same precise estimates of the transverse inhomogeneity length scale obtained from infinitely long thread models are valid, irrespective of the length of the thread. The computation of the magnetic field strength from the obtained seismological curve requires the assumption of a particular value for either the filament or the coronal density. The resulting curves for a typical coronal density and several values of L_{p}/L are shown in Figure 65b. Here again, precise values of the magnetic field strength cannot be obtained, unless the density contrast is accurately known.
6.5 Seismology using period ratios of thread oscillations
The widespread use of the concept of period ratios as a seismological tool has been remarkable in the context of coronal loop oscillations (see Andries et al., 2009, for a review). The idea was first put forward by Andries et al. (2005) and Goossens et al. (2006) as a means to infer the coronal density scale height using multiple mode oscillations in coronal loops embedded in a vertically stratified atmosphere. In coronal loop seismology, the ratio of the fundamental mode period to twice that of its first overtone in the longitudinal direction (P_{1}/2P_{2}) mainly depends on the density structuring along magnetic field lines. It can therefore be used as a diagnostic tool for the coronal density scale height.
In the context of prominence seismology, a similar approach was proposed by Díaz et al. (2010) to obtain information about the density structuring along prominence threads using the piecewise longitudinally structured thread model by Díaz et al. (2002) (see Figure 41). These authors showed that the nondimensional oscillatory frequencies of the fundamental kink mode and the first overtone are almost independent of the ratio of the thread diameter to its length. Thus, the dimensionless oscillatory frequency depends, basically, on the density ratio of the prominence to the coronal plasma, ρ_{p}/ρ_{c}, and the nondimensional length of the thread, W/L,
Here we follow the notation of Díaz et al. (2010), who use 2W for the thread length, rather than that of Soler et al. (2010a), who denote this length by L_{p}. In order to determine the dimensional frequency when comparing to observations, two additional parameters are needed, namely the Alfvén velocity in the corona or in the prominence (involving some knowledge of the magnetic field strength and density) and the length of the magnetic tube, 2L. Note, however, that the nondimensional frequencies of the fundamental mode and its first overtone can be cast as
so that the dependence on the length of the tube and the thread Alfvén speed can be removed by considering the period ratio,
Equation (44) can be used for diagnostic purposes, once reliable measurements of multiple mode periods are obtained. The curves in Figure 66 display the solution to the inverse problem in the (ρ_{p}/ρ_{c}, W/L) parameter space for several values of the period ratio. Given the period ratio from an observation, it only depends on W/L in first approximation. Once W/L has been obtained, one can estimate the value of the magnetic field length 2L, since the thread length, 2W, can be determined quite accurately from the observations.
The use of the period ratio technique needs the unambiguous detection of two periodicities in the same oscillating prominence thread. Díaz et al. (2010) pointed out two main difficulties in this respect. From a theoretical point of view, the overtone with period P_{2} is an antisymmetric mode in the longitudinal direction, with a node in the center of the thread and two maxima located outside it. Only for sufficiently long threads, with W/L ∼ 0.1, the antinodes of the overtone are located inside the thread and could hence be measured in the part of the tube visible in, e.g., Hα. From an observational point of view, no conclusive measurement of the first overtone period has been reported so far in the literature, although there seem to be hints of its presence in some observations by, e.g., Lin et al. (2007), who reported on the presence of two periods, P_{1} = 16 min and P_{2} = 3.6 min in their observations of a prominence region. Díaz et al. (2010) used the period ratio from these observations to infer the value for the length of the thread ratio W/L = 0.12. Although it is difficult to estimate the length of the particular thread under consideration, assuming a value of 13,000 km, as for other threads analyzed by Lin et al. (2007), results in a magnetic tube length L ∼ 130, 000 km.
This new seismological information can be now used to obtain further information about the physical conditions in the oscillating thread. Using analytical approximations for the dimensionless frequency of the first overtone, the following expression for the prominence Alfvén speed as a function of the length of the thread is obtained,
Once the length of the tube is known, an estimate for the prominence Alfvén speed can be inferred from Equation (45). In the example shown by Díaz et al. (2010), the high density contrast limit was used to infer the value v_{Ap} ∼ 160 km s^{1}.
6.6 Seismology of flowing and oscillating prominence threads
Mass flows in conjunction with phase speeds, oscillatory periods, and damping times might constitute an additional source of information about the physical conditions of oscillating threads. The first application of prominence seismology using Hinode observations of flowing and transversely oscillating threads was presented by Terradas et al. (2008), using observations obtained in an active region filament by Okamoto et al. (2007) discussed in Section 3.6.4.
The observations show a number of threads that flow following a path parallel to the photosphere while they oscillate in the vertical direction. The relevance of this particular event is that the coexistence of waves and flows can be firmly established, so that there is no ambiguity about the wave or flow character of a given dynamic feature: both seem to be present in this particular event. However, other interpretations for the apparent motion in the plane of the sky could be also possible, for instance, an ionization wave or a thermal front. Okamoto et al. (2007) analyzed 6 threads whose relevant measured properties are displayed in Table 1.
In their seismological analysis of these oscillations Terradas et al. (2008) started by neglecting the mass flows. Then, they interpreted these events in terms of the standing kink mode of a finitelength thread in a magnetic flux tube (see Figure 41 and Section 4.5). By using theoretical results by Díaz et al. (2002) and Dymova and Ruderman (2005) (see Section 4.5), Terradas et al. (2008) found that, although it is not possible to univocally determine all the physical parameters of interest, a onetoone relation between the thread Alfvén speed and the coronal Alfvén speed could be established. This relation comes in the form of a number of curves relating the two Alfvén speeds for different values of the length of the magnetic flux tube and the density contrast between the filament and coronal plasma. Figure 68 shows these curves for the selection of six threads made by Okamoto et al. (2007). An interesting property of the obtained solution curves is that they display an asymptotic behaviour for large values of the density contrast, which is typical of filament to coronal plasmas and, hence, a lower limit for the thread Alfvén speed can be obtained. Take for instance thread #6. Considering a magnetic flux tube length of 100 Mm, a value of 120 km s^{1} for the thread Alfvén speed is obtained.
Terradas et al. (2008) next incorporated mass flows into their analysis (see Figure 67). First a simple approximation was made by taking into account that the flow velocity along the cylinder, v_{0}, enters the linear MHD wave equations through the differential operator
The terms coming from the equilibrium flow can, in a first approximation, be ignored because, as noted by Dymova and Ruderman (2005), inside the cylinder the terms with derivatives along the tube are much smaller than those with radial or azimuthal derivatives. By following this approach the problem reduces to solving a timedependent problem with a varying density profile, ρ(z, t), representing a dense part moving along the tube with the flow speed. By using the flow velocities in Table 1 and after solving the twodimensional wave equations, Terradas et al. (2008) found that the flow velocities measured by Okamoto et al. (2007) result in slightly shorter kink mode periods than the ones derived in the absence of flow. Differences are small, however, and produce period shifts between 3 and 5%. As a consequence, the curves in Figure 68 can be considered a good approximation to the solution of the inverse problem.
Finally, a more complete approach to the problem was followed by Terradas et al. (2008), who considered the numerical solution of the nonlinear, ideal, lowβ MHD equations with no further approximations, that is, the thin tube approximation was not used and the flow was maintained in the equations. The numerical results confirm the previous approximate results regarding the effect of the flow on the obtained periods and, therefore, on the derived Alfvén speed values. We must note that in this case, and because of the small value of the flow speeds measured by Okamoto et al. (2007) in this particular event, there are no significant variations of the wave properties and, hence, of the inferred Alfvén speeds, although larger flow velocities may have more relevant consequences on the determination of physical parameters in prominence threads.
In most of the examples shown here, the number of unknowns is larger that that of observed parameters. This makes difficult to obtain a unique solution that reproduces the observations. Furthermore, the inversions are performed with information that is incomplete and uncertain. The use of statistical techniques, based on bayesian inference, can help to overcome these limitations, as shown by Arregui and Asensio Ramos (2011).
7 Open Issues
Solar prominences are among the most complicated structures in the solar corona. A full understanding of their formation, magnetic structure, and disappearance has not been reached yet, and a lot of physical effects remain to be included in prominence models. For this reason, theoretical models set up to interpret small amplitude oscillations are still poor. Highresolution observations of filaments suggest that they are made of threads whose thickness is at the the limit of the available spatial resolution. Then, one may wonder whether future improvements of the spatial resolution will provide with thinner and thinner threads or, on the contrary, there is a lower limit for thickness and we will be able to determine it in the future. The presence of these long and thin threads together with the place where they are anchored and the presence of flows along them suggest that they are thin flux tubes filled with continuous or discontinuous cool material.
This cool material is probably subject to cooling, heating, ionization, recombination, motions, etc., which, altogether, makes very difficult a proper theoretical treatment. For instance, in the case of the considered thermal mechanisms, up to now only optically thin radiation has been taken into account, while the inclusion of optically thick effects would probably be more realistic; the prominence heating mechanisms taken usually into account are tentative and “ad hoc”, while true prominence heating processes are still deeply unknown. An important step ahead would be to couple radiative transfer with magnetohydrodynamic waves as a mean to establish a relationship between velocity, density, magnetic field, and temperature perturbations, and the observed signatures of oscillations like spectral line shift, width and intensity. Partial ionization is another topic of interest for prominence oscillations since, apart from influencing the behaviour of magnetohydrodynamic waves, it poses an important problem for prominence equilibrium models since crossfield diffusion of neutral atoms can give place to flows and drain prominence material.
Another issue which still remains a mystery is the triggering mechanism of small amplitude oscillations. In the case of large amplitude oscillations, observations provide with information about the exciting mechanism, but the available observations of small amplitude oscillations show no signature of their exciting mechanism. Are these oscillations of chromospheric or photospheric origin? Are they generated inside prominence magnetic structures by small reconnection events? Are they produced by weak external disturbances coming from far away in the solar atmosphere?
The presence of flows adds another ingredient to be taken into account in the study of prominence oscillations and, up to now, we can only obtain one or twodimensional information about the flow behaviour. It would be of great interest to collect information about the threedimensional structure of flows and, probably, in the near future we could acquire this information by means of IRIS (http://iris.lmsal.com/).
The physical changing conditions of prominence plasmas suggest that for an indepth theoretical study of prominence oscillations more complex models together with numerical simulations are needed. Therefore, and as a step ahead, in the next future numerical studies of the time evolution of magnetohydrodynamic waves in partially ionized flowing inhomogeneous prominence plasmas, subject to different physical processes such as ionization, recombination, etc., should be undertaken. However, a full threedimensional dynamical prominence model involving magnetic equilibrium, radiative transfer, etc., whose oscillatory behaviour could be studied seems to be still far away in the future.
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