Abstract
The global distribution of 1.27 μm O2 nightglow brightness observed by the TIMED/SABER satellite has been investigated to find the longitudinal structures for different seasons and latitudes. The results show that the O2 airglow is dominated by wave 4 structure at latitudes between equator and 20°S/N in both hemispheres during most seasons. At mid-latitudes around 40°S/N, the wave 1 structure is observed for most seasons with a small contribution of wave 2 during the June solstice. A comparison of the O2 and OH nightglows shows similarity in their global distributions which can be attributed to their similar photochemical mechanisms.
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Li Q, Xu J Y, Yue J, et al. Statistical characteristics of gravity wave activities observed by an OH airglow imager at Xinglong in northern China. Ann Geophys, 2011, 29: 1401–1410
Yuan W, Xu J Y, Ma R P, et al. First observation of mesospheric and thermospheric winds by a Fabry-Perot interferometer in China. Chin Sci Bull, 2010, 55: 4046–4051
Jiang G Y, Yuan W, Ning B Q, et al. A comparison of mesospheric winds measured by FPI and meteor radar located at 40N. Sci China Tech Sci, this special issue, 2012
Zhu Y J, Xu J Y, Yuan W, et al. First experiment of spectrometric observation of the Hydroxyl Emission and Rotational Temperature in the mesopause in China. Sci China Tech Sci, this special issue, 2012
Shepherd G G, Thuillier G, Solheim B H, et al. Longitudinal structure in atomic oxygen concentrations observed with WINDII on UARS. Geophys Res Lett, 1993, 20: 1303–1306
Zaragoza G, Taylor F W, López-Puertas M. Latitudinal and longitudinal behavior of the mesospheric OH nightglow layer as observed by the Improved Stratospheric and Mesospheric Sounder on UARS. J Geophys Res, 2001, 106: 80278033
Wang D Y, Ward W E, Solheim B H, et al. Longitudinal variations of green line emission rates observed by WINDII at altitudes 90–120 km during 1991–1996. J Atmos Solar-Terr Phys, 2004, 64: 1273–1286
England S L, Immel T J, Sagawa E, et al. Effect of atmospheric tides on the morphology of the quiet time, postsunset equatorial ionospheric anomaly. J Geophys Res, 2006, 111: A10S19
Xu J, Smith A K, Jiang G Y, et al. Strong longitudinal variations in the OH nightglow. Geophys Res Lett, 2010, 37: L21801
Gao H, Xu J Y, Chen G M, et al. Global distributions of OH and O2 (1.27 μm) nightglow emissions observed by TIMED satellite. Sci China Tech Sci, 2011, 54: 1–10
Shepherd G G, Roble R G, Zhang S P, et al. Tidal influence on midlatitude airglow: Comparison of satellite and ground-based observations with TIME-GCM predictions. J Geophys Res, 1998, 103: 14741–14751
Ward W E. A Simple Model of Diurnal Variations in the Mesospheric Oxygen Nightglow. Geophys Res Lett, 1999, 26: 3565–3568
Marsh D R, Smith A K, Mlynczak M G, et al. SABER observations of the OH Meinel airglow variability near the mesopause. J Geophys Res, 2006, 111: A10S05
Xu J Y, Smith A K, Liu H L, et al. Seasonal and QBO variations in the migrating diurnal tide observed by TIMED. J Geophys Res, 2009, 114: D13107
Yuan T, She C Y, Krueger D, et al. A collaborative study on temperature diurnal tide in the midlatitude mesopause region (41°N, 105°W) with Na lidar and TIMED/SABER observations. J Atmos Solar-Terr Phys, 2010, 72: 541–549
Hagan M E, Forbes J M. Migrating and nonmigrating diurnal tides in the middle and upper atmosphere excited by tropospheric latent heat release. J Geophys Res, 2002, 107: 4754–4768
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Gao, H., Nee, J. & Chen, G. Longitudinal distribution of O2 nightglow brightness observed by TIEMD/SABER satellite. Sci. China Technol. Sci. 55, 1258–1263 (2012). https://doi.org/10.1007/s11431-012-4802-0
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DOI: https://doi.org/10.1007/s11431-012-4802-0