# \(\pi \pi \rightarrow K {\bar{K}}\) scattering up to 1.47 GeV with hyperbolic dispersion relations

## Abstract

In this work we provide a dispersive analysis of \(\pi \pi \rightarrow K{\bar{K}}\) scattering. For this purpose we present a set of partial-wave hyperbolic dispersion relations using a family of hyperbolas that maximizes the applicability range of the hyperbolic dispersive representation, which we have extended up to 1.47 GeV. We then use these equations first to test simple fits to different and often conflicting data sets, also showing that some of these data and some popular parameterizations of these waves fail to satisfy the dispersive analysis. Our main result is obtained after imposing these new relations as constraints on the data fits. We thus provide simple and precise parameterizations for the S, P and D waves that describe the experimental data from \(K{{\bar{K}}}\) threshold up to 2 GeV, while being consistent with crossing symmetric partial-wave dispersion relations up to their maximum applicability range of 1.47 GeV. For the *S*-wave we have found that two solutions describing two conflicting data sets are possible. The dispersion relations also provide a representation for *S*, *P* and *D* waves in the pseudo-physical region.

## 1 Introduction

The scattering of pions and kaons is interesting for several reasons: First, by itself, in order to test and understand the dynamics of these particles, which are the pseudo-Goldstone Bosons of the QCD spontaneous chiral symmetry breaking. Second, because these scattering processes are one of the main sources of information on the existence and parameters of several meson resonances. In particular, this is the case of light scalar mesons, whose very existence, nature and classification are still a matter of debate (see the note on light scalars in the review of particle properties (RPP) [1]). These resonances are very relevant for the identification of glueballs, tetraquaks or molecular states that lie beyond the ordinary meson states of the naive quark model. Finally, being the lightest mesons, final state interactions (FSI) of pions and kaons play an essential role in the description of many hadronic processes. The unprecedented statistical samples obtained in the last years on different hadronic experiments and the even more ambitious plans for future facilities have provoked a renovated interest for precise and rigorous analyses of existing meson-meson scattering data, superseding simple model descriptions.

Unfortunately, most of the data on meson-meson scattering [2, 3, 4, 5, 6, 7, 8, 9, 10] are extracted indirectly from meson-nucleon to meson-meson-nucleon reactions. This extraction is complicated, relying on some model assumptions, and for this reason it is affected with large systematic uncertainties, which can be estimated from the differences between data sets from different experiments (and for \(\pi \pi \) scattering even within data sets from the same experiment [2, 3]). Moreover, the description of these data is frequently done in terms of meson-meson models which can lead to artifacts and unreliable determinations of resonances and their parameters. It is for these reasons that dispersive techniques are required.

Dispersion relations are the mathematical expression of causality and crossing. They relate the amplitude at a given energy to integrals of the amplitude and can be used as consistency tests of the experimental data or as constraints on the fits. We will make both uses here. For dispersive integrals to be evaluated just over the physical region, crossing must be used and two main kinds of dispersion relations appear then: Forward Dispersion Relations (FDRs) and those for partial waves generically know as Roy or Roy–Steiner equations [11, 12, 13], depending on whether the scattering occurs among particles with equal or different masses. FDRs are rather simple and easily extended to arbitrary energies. They have been recently applied to constrain \(\pi \pi \) [14, 15, 16, 17] and \(K\pi \) [18] scattering amplitudes that will be used as input in some stages of the present work. Roy-like equations are a complicated system of coupled equations, limited in practice to energies of \(\mathcal {O}(1\, \mathrm{GeV})\) for meson-meson scattering. However, they provide a rigorous continuation to the complex plane that allows for a precise and model independent determination of resonances. Actually, it was only in 2012 that the RPP [1] considered settled the issue of the existence and parameters of the much debated scalar \(f_0(500)\) resonance [19], traditionally known as \(\sigma \)-meson, and to a very large extent this was due to the results of dispersive analyses of \(\pi \pi \) scattering amplitudes with versions of Roy equations [20, 21, 22]. Similarly, the scalar \(K_0^*(800)\) or \(\kappa \)-meson has also been obtained from \(\pi K\) scattering using unitarization and dispersive methods [23, 24, 25], the most reliable value [26] being the Roy–Steiner method based on hyperbolic dispersion relations [27], but according to the RPP this resonance still “needs confirmation” [1]. Roy–Steiner equations have also been applied recently to \(\pi N\) scattering [28] and for \(\gamma \gamma \rightarrow \pi \pi \) [29]. For meson-resonances beyond \(\sim \)1 GeV, Roy-like equations are not used in practice, but other analytic tools have been recently applied [30, 31, 32] to extract resonance poles from the description of amplitudes in the physical region constrained with dispersion relations, thus minimizing the model-dependence.

The purpose of this paper is to obtain a set of simple \(\pi \pi \rightarrow K{\bar{K}}\) scattering parameterizations satisfying Roy–Steiner dispersion relations that can be easily used later on both by theoreticians and experimentalists, as has already been the case of previous works for \(\pi \pi \) and \(\pi K\) scattering. The motivations to study \(\pi \pi \rightarrow K{\bar{K}}\) are the ones explained above for meson-meson scattering in general: (i) a rigorous \(\pi \pi \rightarrow K{\bar{K}}\) description is a necessary input for further studies of resonances (like scalars in the 1–1.6 GeV, range), in particular in order to compare their \(\pi \pi \) and \(K{\bar{K}}\) couplings, (ii) it is also an essential ingredient in the Roy–Steiner study of \(K\pi \) scattering and the determination of the controversial \(K^*_0(800)\)-meson (whose determination is one of the goals of a recent proposal at JLab [33]) (iii) the \(\pi \pi \rightarrow K{\bar{K}}\) amplitude also influences, via unitarity, the \(\pi \pi \rightarrow \pi \pi \) and \(\pi \pi \rightarrow NN\) amplitudes, and consequently those of *KN* and \({\bar{K}} N\) scattering. Finally \(\pi \pi \rightarrow K{\bar{K}}\) is a very relevant ingredient in the FSI of numerous hadron decays. For instance, the role of \(\pi \pi \rightarrow K{\bar{K}}\) re-scattering has gained a renewed interest due to the recent observation of a large CP violation in recent studies at LHCb [34, 35, 36], although the amplitude used for such studies has been approximated with simple models and the amplitudes obtained here could be used to avoid such assumptions in further studies which are under way. Finally, lattice calculations of the coupled channel \(\pi \pi \), \(K{\bar{K}}\), \(\eta \eta \) scattering have appeared very recently [37]. Although these calculations are performed still at relatively high pion masses, the physical point where one can compare with our actual \(\pi \pi \rightarrow K{\bar{K}}\) parameterizations could be accessible soon.

Dispersive studies of \(\pi \pi \rightarrow K{\bar{K}}\) scattering and its relation to \(\pi K\rightarrow \pi K\) scattering were first performed in the seventies [38, 39, 40, 41]. It was soon clear that the formalism of fixed-t dispersion relations combined with hyperbolic dispersion relations (HDR) for partial waves [12, 13] was best suited to study the physical regions of both channels simultaneously [39, 41]. However, \(\pi \pi \rightarrow K{\bar{K}}\) data was scarce and these analyses only allowed for crude checks of low-energy scalar partial waves, frequently focusing on threshold parameters and the non-physical region between the two-pion and the two-kaon thresholds (or at most up to 1100 MeV). For a review of the theoretical and experimental situation until 1978 we refer to [42].

The main experimental results on \(\pi \pi \rightarrow K{\bar{K}}\) partial waves, that will be thoroughly analyzed in this work, were obtained in the early eighties [7, 8], indirectly from \(\pi N\rightarrow K{\bar{K}} N'\) reactions. They extend from energies very close to the \(K{\bar{K}}\) threshold up to 1.6 GeV. Several models exist in the literature describing these \(\pi \pi \rightarrow K{\bar{K}}\) data [43, 44, 45, 46, 47, 48], in particular with unitarized chiral Lagrangians [23, 24, 49, 51, 53]. These works are of relevance for studies of \(f_0\) resonances and glueballs in that range.

A renewed interest on dispersive analysis of \(\pi \pi \rightarrow K{\bar{K}}\) at the turn of the century was triggered by the need for precise determinations of threshold parameters and chiral perturbation theory low energy constants. Actually, sum rules for \(\pi K\) were obtained from a Roy–Steiner type of equations from HDR [52, 53] in which the \(\pi \pi \rightarrow K{\bar{K}}\) amplitude in the unphysical region was obtained as a solution of a dispersive Mushkelishvili–Omnés problem. The \(\pi \pi \rightarrow K{\bar{K}}\) partial-wave data of [7, 8] was used as input. However, no dispersive analysis of these data has been carried out beyond the \(K{{\bar{K}}}\) threshold, mostly due to the relatively low applicability limit of the HDR along the \(su=b\) hyperbolas used in those works. It was nevertheless shown that an extrapolation of the HDR solutions beyond their applicability region was fairly close to the data. Finally, in [27] a Roy–Steiner type of analysis was performed to obtain solutions for the \(\pi K\) elastic amplitudes, using once again as input the \(\pi \pi \rightarrow K{\bar{K}}\) amplitudes in the physical region. This study was the basis for confirming the existence of the \(K_0^*(800)\) meson through a dispersive analysis [26].

The aim of this work is then to provide a simple set of \(\pi \pi \rightarrow K{\bar{K}}\) parameterizations that describe the data up to 2 GeV while also satisfying dispersive constraints in the whole region from \(\pi \pi \) threshold up to 1.47 GeV. To this end, we will derive a new set of hyperbolic dispersion relations, along \((s-a)(u-a)=b\) hyperbolas, choosing the *a* parameter to maximize the applicability range which allows us to use them up to 1.47 GeV. This will also allow us to test different and often conflicting data sets and popular parameterizations.

The plan of the work is as follows: in Sect. 2 we will introduce the notation, in Sect. 3 we will present simple unconstrained fits to the different \(\pi \pi \rightarrow K{\bar{K}}\) data as well as a Regge formalism for the high energy part, taking particular care on the determination of uncertainties. In Sect. 4 we will derive our new set of HDR, i.e. Roy–Steiner like equations for partial waves, and formulate the Mushkelishvili–Omnés problem used for both the unphysical region below \(K {{\bar{K}}}\) threshold and the physical region up to 1.47 GeV. In Sect. 5 we will first use these equations as checks for the unconstrained parameterizations. Finally, in Sect. 6 we will impose the new relations on the data fits. This will lead to the desired constrained fits to data satisfying the analyticity requirements, which are the main results of this work. In Sect. 7 we will summarize our findings and conclude.

## 2 Kinematics and notation

Throughout this work we will be working in the isospin limit of equal mass for all pions, \(m_\pi =139.57\,\)MeV, and equal mass for all kaons, \(m_K=496\,\)MeV.

*s*,

*t*,

*u*for \(\pi K\) scattering, satisfying \(s+t+u=2(m_\pi ^2+m_K^2)\) and write

*t*-channels, which are customarily introduced to ensure good analytic properties for \(g_\ell (t)\) (see [54] in the \(\pi \pi \rightarrow N{\bar{N}}\) context). The scattering angles in the

*s*and

*t*channels are given by:

## 3 Unconstrained fits to data

### 3.1 The data

As we have already emphasized in the introduction we will explicitly choose very simple parameterizations to fit the data, so that they can be used easily later on. In this section we will just describe the data without imposing dispersion relations. These will be called unconstrained fits to data (UFD). In this way the fits to each wave are independent from each other. Later on we will impose the dispersion relations as constraints and obtain the constrained fits to data (CFD). This will correlate different waves.

The data we will fit are of four types. First, we will use data on the phases and modulus of the \(g^0_0, g^1_1\) partial waves extracted from \(\pi ^- p\rightarrow K^-K^+ n\) and \(\pi ^+ n\rightarrow K^-K^+ p\) at the Argonne National Laboratory [7] and from \(\pi ^- p\rightarrow K^0_sK^0_s n\) at the Brookhaven National Laboratory in a series of three works [8, 9, 10], that we will call Brookhaven-I, Brookhaven-II and Brookhaven-III, respectively. Second, for the tensor \(g^0_2\) wave, data for its modulus was given in Brookhaven-II and Brookhaven-III, although as we will see the old experimental parameterizations are not quite compatible with the present resonance parameters listed in the RPP. Third, for higher partial waves, which play a very minor role in the numerics, we use simple resonance parameterizations with their parameters as quoted in the RPP. Finally, for the high-energy range above 2 GeV we rely on recent updates [17, 18, 26], of Regge parameterizations [55] based on factorization and the phenomenological observations about Regge trajectories or the Veneziano model [56, 57, 58, 59].

### 3.2 Partial wave fits from \(K {{\bar{K}}}\) threshold to 2 GeV

We now describe our partial-wave parameterizations in the region from \(K{{\bar{K}}}\) threshold to 2 GeV. For all of them we define a modulus and a phase \(t^I_\ell =|t^I_\ell |e^{i\phi ^I_\ell }\). We will start with the waves that have less controversy on the data sets and that, as we will see later, satisfy best our Roy–Steiner-like equations, leaving for the end the most difficult one, which is that with \(\ell =0,I=0\). Note that since in the isospin limit all pions are identical particles, Bose statistics applies and \(\ell +I\) must be even.

#### 3.2.1 \(\ell =1,I=1\) partial wave

*C*and \(r_1\) are real, they do not contribute to the phase, nor \(\beta _1\) nor \(\gamma _1\), being multiplied by \({\hat{q}}_K^2\), so that the parameters \(m_\rho , \Gamma _\rho , \beta , \gamma \) are obtained from a fit to the dispersive analysis [17] of the \(\pi \pi \) phase shift in the elastic region. Indeed, in the lower panel of Fig. 1 it can be seen that our parameterization describes remarkably well the \(\pi \pi \) scattering data on the phase below \(K{{\bar{K}}}\) threshold.

Parameters of the \(g^1_1\) wave. Masses and widths are given in GeV whereas, *C*, \(\beta _1,\gamma _1\) and \(r_1\) are given in GeV\(^{-2}\)

Parameter | UFD | CFD |
---|---|---|

\(m_\rho \) | 0.7757 ± 0.0010 | 0.7749 ± 0.0010 |

\(\Gamma _\rho \) | 0.152 ± 0.001 | 0.153 ± 0.001 |

\(m_{\rho '}\) | 1.440 ± 0.015 | 1.438 ± 0.015 |

\(\Gamma _{\rho '}\) | 0.310 ± 0.029 | 0.309 ± 0.029 |

\(m_{\rho ''}\) | 1.72 | 1.72 |

\(\Gamma _{\rho ''}\) | 0.25 | 0.25 |

| 1.21 ± 0.11 | 1.23 ± 0.11 |

\(r_1\) | 3.95 ± 0.76 | 3.43 ± 0.76 |

\(\beta \) | \(-0.168\) ± 0.007 | \(-0.172\) ± 0.007 |

\(\beta _1\) | 0.37 ± 0.02 | 0.38 ± 0.02 |

\(\gamma \) | 0.10 ± 0.02 | 0.14 ± 0.02 |

\(\gamma _1\) | \(-0.06\) ± 0.06 | \(-0.17\) ± 0.06 |

The parameters of the \(\rho ''\) resonance are fixed for simplicity to those of the RPP [1], whereas those for the \(\rho '\) are allowed to vary within 1.5 standard deviations within the values listed in the PDG. Note that the ones determined by the CLEO Collaboration [61] are not compatible with our best fit, if one tries to fix those parameters to reproduce the \(\pi \pi \rightarrow K {{\bar{K}}}\) data the \(\chi ^2\) is increased by almost a factor of 2. Then we fit the rest of the parameters to describe the data in the physical and pseudophysical regions, the best result is shown in Fig. 1 and the parameters are given in Table 1. The fit has a total \(\chi ^2/dof=1.7\), but a slightly larger \(\chi ^2/dof=2.2\) is found in the physical region. Conservatively we use the square root of the latter to rescale the fit parameter uncertainties in the table.

The data and the results of our unconstrained fit to data (UFD) are shown in Fig. 1. Note that we plot the modulus from \(K{{\bar{K}}}\) threshold and that, as already commented, data only reaches up to 1.57 GeV. The shape above that energy is almost entirely given by the \(\rho ''\) resonance. Concerning the phase, from the two-pion threshold to the \(K {{\bar{K}}}\) threshold it is indistinguishable from that obtained from the \(\pi \pi \) dispersive analysis in [17]. In Fig. 1 our result below threshold can be compared to the data from elastic \(\pi \pi \) scattering [2, 4]. Note also the large uncertainty of both the data and the error bands in the region around 1.5 GeV, which is due to the fact that the modulus almost vanishes there. Fortunately, this will also make the contribution of that region to the dispersive integrals almost negligible.

#### 3.2.2 \(\ell =2,I=0\) partial wave

Contrary to the previous \(\ell =1,I=1\) case, where the \(\rho (770)\) resonance dominates the unphysical region, now the lowest resonance is well above the \(K{{\bar{K}}}\) threshold and therefore it does not dominate the unphysical region. Thus our \(\ell =2,I=0\) parameterization will have two pieces: one above \(K{{\bar{K}}}\) threshold and another one below.

In Eq. (15) above, \(T=1,2,3\) stands for the tensor \(f_2(1270)\), \(f'_2(1525)\) and \(f_2(1810)\) resonances, respectively. Since they decay predominantly to \(\pi \pi \), \({{\bar{K}}}K\) and \(\pi \pi \), respectively, we have set \(q_1(t)=q_3(t)=q_\pi (t)\), whereas \(q_2(t)=q_K(t)\). The mass \(M_T\) and width \(\Gamma _T\) of each resonance after the fit are given in Table 2. As can be seen in the Brookhaven-II and III fits in [9, 10], the \(f_2'(1525)\) was at odds with the present knowledge about this resonance parameters. Moreover, the parameters of the \(f_2(1810)\) vary within a huge range even when using almost the same data. As we have no data for the phase of the partial wave it is not possible to fix the position of the masses with accuracy, however, performing a coupled-channel analysis for the tensor partial wave is out of the scope of this work, mostly because we have no dispersive control over other channels apart from \(\pi \pi \rightarrow K {\bar{K}}\). For that reason we have included the masses of both the \(f_2(1270)\) and the \(f'_2(1525)\) as additional data for our fit. In particular, we take as input for the fit \(m_{f_2}=1.2755 \pm 0.0035\,\)GeV which is the average and standard deviation of the values used in the RPP’s own average [1]. This we do to have a more conservative estimate of the systematic uncertainty. For the \(f_2'\) we take directly the RPP average \(m_{f'_2}=1.525 \pm 0.005\,\)GeV. The inclusion of the \(f_2(1810)\) is purely phenomenological, following [9, 10], just to describe the final rise seen in the modulus, but this resonance still “needs confirmation” according to the RPP. We could have described this raise equally well with another functional form, although it is also clear that there exist some enhancements of the amplitudes and phases for \(\pi \pi \rightarrow \pi \pi \) and \(\pi \pi \rightarrow \eta \eta \). Its numerical effect on our dispersive integrals is rather small. In Table 2 we also provide the phases \(\phi _T\) resulting from the fit to data.

Parameters of the \(g^0_2\) wave

Parameter | UFD | CFD |
---|---|---|

\(m_{f_2(1270)}\) | 1.271 ± 0.0035 GeV | 1.271 ± 0.0035 GeV |

\(m_{f'_2(1525)}\) | 1.522 ± 0.005 GeV | 1.522 ± 0.005 GeV |

\(m_{f_2(1810)}\) | 1.806 ± 0.017 GeV | 1.802 ± 0.017 GeV |

\(\Gamma _{f_2(1270)}\) | 0.187 ± 0.009 GeV | 0.191 ± 0.009 GeV |

\(\Gamma _{f'_2(1525)}\) | 0.108 ± 0.016 GeV | 0.107 ± 0.016 GeV |

\(\Gamma _{f_2(1810)}\) | 0.201 ± 0.028 GeV | 0.198 ± 0.028 GeV |

\(\phi _{f_2(1270)}\) | \(-0.049\) ± 0.014 | \(-0.078\) ± 0.014 |

\(\phi _{f'_2(1525)}\) | 2.62 ± 0.16 | 2.59 ± 0.16 |

\(\phi _{f_2(1810)}\) | \(-0.72\) ± 0.16 | \(-0.82\) ± 0.16 |

\(B_0\) | 12.5 ± 0.4 | 12.4 ± 0.4 |

\(B_1\) | 10.3 ± 1.0 | 12.3 ± 1.0 |

| 1.82 ± 0.09 GeV\(^{-2}\) | 1.86 ± 0.09 GeV\(^{-2}\) |

\(r_2^2\) | 6.68 ± 0.72 GeV\(^{-4}\) | 6.78 ± 0.72 GeV\(^{-4}\) |

\(\beta \) | 0.070 ± 0.016 | 0.066 ± 0.016 |

\(\gamma \) | 0.093 ± 0.02 | 0.094 ± 0.02 |

Neither Brookhaven-I nor Argonne provide data for this wave, nor the models they used to parameterize it. Nevertheless Brookhaven-I shows a plot with the central value of their phase for this channel, which is later used to extract the \(g^0_0\) phase. As seen in Fig. 3 our phase is fairly compatible with the Brookhaven-I model between 1.25 and 1.54 GeV. However, also in that figure it can be seen that the Brookhaven-I model violates Watson’s Theorem at low energies, which our phase fully satisfies. In addition, above 1.6 GeV our phase, obtained by fitting the Brookhaven-II data [9] on the modulus with modern values for the \(f_2\) family of resonances, is rather different from the flat behavior of the Brookhaven-I model [8] up to 1.9 GeV. The reason is that the Brookhaven-I model used a simple smooth background to describe the 1.6–1.9 GeV region, instead of the \(f_2(1810)\) used in this work. Actually, we have checked that if we impose the phase of the Brookhaven-I model on our fit to the Brookhaven-II modulus, the resulting \(\chi ^2 /dof\) is \(\sim 5\), and thus strongly disfavored with respect to our phase. Even by deforming our fits by including more parameters, the best we have been able to achieve when imposing the phase of the Brookhaven-I model above 1.6 GeV, is \(\chi ^2/dof \sim 3\), but at the price of introducing contributions difficult to interpret in terms of resonance parameters. Both the violation of Watson’s Theorem and the use of such non-resonant background make the Brookhaven-I solution suspicious.

#### 3.2.3 \(\ell =0,I=0\) partial wave

- I.
Region I: From \(\sqrt{t_{min,I}}=2m_K\) up to \(\sqrt{t_{max,I}}=1.47\,\)GeV, where data from Argonne [7] and Brookhaven-I [8] coexist. Note that this region will lie within the applicability of Roy–Steiner equations and will be later constrained to satisfy dispersion relations.

Concerning the phase \(\phi ^0_0\), it is clearly seen in Fig. 4 that from \(2m_K\) up to \(1.2\,\)GeV, the Argonne [7] and Brookhaven-I [8] sets are incompatible. Let us now recall that, by Watson’s Theorem, \(\phi ^0_0\) at \(K {\bar{K}}\) threshold should match the scalar-isoscalar \(\pi \pi \rightarrow \pi \pi \) phase shift \(\delta _0^{(0)}\). However, the \(\pi \pi \) scattering analyses with Roy and GKPY equations that extend up to or beyond \(K {{\bar{K}}}\) threshold [17, 63] find \(\delta _0^{(0)}>200^\circ \), which is consistent with the Argonne [7] phase, but much higher than the phase of Brookhaven-I [8]. In addition we have just seen that this phase was extracted using a \(g_2^0\) wave that also violates Watson’s Theorem. Therefore, for our fits we have discarded the phase of Brookhaven-I [8] below \(\sim \) 1.15 GeV, i.e. until it agrees with that of Argonne [7].

Concerning the data on \(\vert g_0^0\vert \), shown in Fig. 4, the Argonne and Brookhaven-I sets are consistent among themselves but not with the Brookhaven-II. However, the latter is consistent up to 1.2 GeV with the dip solution for the inelasticity favored from dispersive analyses of \(\pi \pi \rightarrow \pi \pi \) scattering [17, 63] (assuming that only \(\pi \pi \) and \(K{{\bar{K}}}\) states are relevant). Finally, the “dip” solution from \(\pi \pi \) scattering in the 1.2 GeV to 1.47 region has such large uncertainties that is roughly consistent with the three data sets.

- II.
In the region from \(\sqrt{t_{min,II}}=1.47\) GeV to \(\sqrt{t_{max,II}}=2\) GeV Roy–Steiner equations will not be applicable and thus this region will only be used as input for our dispersive calculations for lower energies. Note that here all experiments are roughly consistent, although the Argonne set only reaches up to \(\sim \) 1.5 GeV, Brookhaven-I up to \(\sim \) 1.7 GeV and only Brookhaven-II reaches up to 2 GeV.

*n*, \(p_n(1)=1\) and \(p_n(-1)=(-1)^n\), which is useful for matching the different pieces smoothly up to the first derivative.

Parameters of \(\phi ^0_0\)

Parameter | UFD | \(\hbox {CFD}_\text {B}\) | \(\hbox {CFD}_\text {C}\) |
---|---|---|---|

\(B_1\) | 23.6 ± 1.3 | 22.1 ± 1.3 | 22.9 ± 1.3 |

\(B_2\) | 29.4 ± 1.3 | 27.7 ± 1.3 | 28.4 ± 1.3 |

\(B_3\) | 0.6 ± 1.6 | 1.8 ± 1.6 | 1.1 ± 1.6 |

\(C_1\) | 34.3932 fixed | 35.3450 fixed | 34.51593 fixed |

\(C_2\) | 4.4 ± 2.6 | 4.3 ± 2.6 | 4.3 ± 2.6 |

\(C_3\) | \(-\,32.9\) ± 5.2 | \(-\,33.3\) ± 5.2 | \(-\,32.6\) ± 5.2 |

\(C_4\) | \(-\,16.0\) ± 2.2 | \(-\,16.5\) ± 2.2 | \(-\,16.0\) ± 2.2 |

\(C_5\) | 7.4 ± 2.4 | 7.2 ± 2.4 | 7.2 ± 2.4 |

Parameters of the \(\hbox {UFD}_\text {B}\) and CFD\(_{\mathrm{B}}\) fits to \(\vert g^0_0\vert \)

Parameter | \(\hbox {UFD}_\text {B}\) | \(\hbox {CFD}_\text {B}\) |
---|---|---|

\(D_0\) | 0.59 ± 0.01 | 0.60 ± 0.01 |

\(D_1\) | \(-\,0.38\) ± 0.01 | \(-\,0.35\) ± 0.01 |

\(D_2\) | 0.12 ± 0.01 | 0.13 ± 0.01 |

\(D_3\) | \(-\,0.09\) ± 0.01 | \(-\,0.12\) ± 0.01 |

\(F_1\) | \(-\,0.04329\) fixed | \(-\,0.04078\) fixed |

\(F_2\) | \(-\,0.008\) ± 0.009 | \(-\,0.007\) ± 0.009 |

\(F_3\) | \(-\,0.028\) ± 0.007 | \(-\,0.035\) ± 0.007 |

\(F_4\) | 0.026 ± 0.007 | 0.037 ± 0.007 |

Parameters of the \(\hbox {UFD}_\text {C}\) and CFD\(_{\mathrm{C}}\) fits to \(\vert g^0_0\vert \)

Parameter | \(\hbox {UFD}_\text {C}\) | \(\hbox {CFD}_\text {C}\) |
---|---|---|

\(D_0\) | 0.46 ± 0.01 | 0.46 ± 0.01 |

\(D_1\) | \(-\,0.27\) ± 0.01 | \(-\,0.25\) ± 0.01 |

\(D_2\) | 0.11 ± 0.01 | 0.11 ± 0.01 |

\(D_3\) | \(-\,0.078\) ± 0.009 | \(-\,0.087\) ± 0.009 |

\(F_1\) | \(-\,0.04153\) fixed | \(-\,0.03738\) fixed |

\(F_2\) | \(-\,0.010\) ± 0.008 | \(-\,0.013\) ± 0.008 |

\(F_3\) | \(-\,0.023\) ± 0.007 | \(-\,0.025\) ± 0.007 |

\(F_4\) | 0.021 ± 0.006 | 0.025 ± 0.006 |

#### 3.2.4 Partial waves with \(\ell >2\)

For higher partial waves we just use Breit–Wigner descriptions associated to the poles listed in the PDG. In particular, for the \(g^1_3(t)\) we include a single \(\rho _3(1690)\) resonance. The \(\ell =4\) partial wave, parametrized as an \(f_4(2050)\) Breit–Wigner resonance, is only included in the \(g^0_2(t)\) dispersive calculation due to its negligible contribution below 2 GeV for the \(g^0_0(t)\).

### 3.3 Higher energies

There is no high-energy experimental information on \(\pi \pi \rightarrow {{\bar{K}}}K\) nor \(\pi K\rightarrow \pi K\). However, the high energy behavior of both processes can be confidently modeled by applying factorization to Regge amplitudes obtained for other processes. In this work we will use, for the *s*-channel above 1.74 GeV the Regge model description presented in [55] and updated in [17, 18], whereas for the *t*-channel we will use the asymptotic forms of the Veneziano model [56, 57, 58, 59], with the updated parameters in [27], to describe the process above 2 GeV. The reasons to choose 2 GeV in this work are twofold: on the one hand data for the \(g_0^0\) and \(g_2^0\) waves reach above that energy, on the other hand, even if the \(g_1^1\) data end at 1.6 GeV, the \(\rho ''(1720)\) is well established in the RPP and with its 250 MeV width, reaches well above 2 GeV. Thus we rely on our partial-wave parameterizations up to 2 GeV, but not much more.

In what follows we provide the detail of these descriptions using the notation of this work.

*P*(

*s*,

*t*) contribution and the \(f_2\) or \(P'(s,t)\) exchange:

*KK*-Reggeon vertex, whereas

*r*is related to the branching ratio of the \(f_2(1270)\) resonance to \({{\bar{K}}}K\). In addition

Regge parameters | Used both for UFD and CFD |
---|---|

\(s'\) | 1 GeV\(^{2}\) |

\({\hat{b}}\) | 2.4 ± 0.5 GeV\(^{-2}\) |

\(\alpha '_{P}\) | 0.2 ± 0.1 GeV\(^{-2}\) |

\(\alpha '_{P'}\) | 0.9 GeV\(^{-2}\) |

\(c_{P}\) | 0.6 ± 1 GeV\(^{-2}\) |

\(c_{P'}\) | \(-\,0.38\) ± 0.4 GeV\(^{-2}\) |

\(\beta _{P}\) | 2.50 ± 0.04 |

\(c_{P}(0)\) | 0 ± 0.04 |

\(\beta _{P'}\) | 0.80 ± 0.05 |

\(c_{P'}(0)\) | \(-\,0.4 \) ± 0.4 |

\(\alpha _{P'}(0)\) | 0.53 ± 0.02 |

\(\alpha _{\rho }(0)\) | 0.53 ± 0.02 |

\(\alpha '_{\rho }\) | 0.9 GeV\(^{-2}\) |

\(\alpha ''_{\rho }\) | \(-\,0.3\) GeV\(^{-4}\) |

\(d_{\rho }\) | 2.4 ± 0.5 GeV\(^{-2}\) |

\(e_{\rho }\) | 2.7 ± 2.5 |

\(\beta _{\rho }\) | 1.47 ± 0.14 |

In contrast, the determination of the parameters \(f_{K/\pi }\), *r* and \(g_{K/\pi }\) needs input from kaon interactions. In principle all them were determined in [55] from *KN* factorization and we take the \(f_{K/\pi }\) and *r* values from that reference. Concerning \(g_{K/\pi }\) we take the updated value from the forward dispersion relation study of \(\pi K\) scattering in [18] (we use the value from the CFD there). Their values can be found in Table 7. Since their determination involves kaon interactions, we will allow them to vary when constraining our fits with dispersion relations, i.e. from the UFD to the CFD sets. However, in the table it is seen that the change is minute.

For the *t*-channel, \(\pi \pi \rightarrow K{{\bar{K}}}\), we also need the exchange of strange Reggeons, for which we will assume that the dominant trajectories \(K^*_1(892)\) and \(K_2^*(1430)\) are degenerate, Thus we use for them a common trajectory \(\alpha _{K^ *}(s)=\alpha _{K^ *}+\alpha '_{K^ *}s\) whose parameters, listed in Table 7, are obtained from the linear Regge trajectories for strange resonances and therefore are kept fixed for both our UFD and CFD sets.

*a*,

*b*parameters in the above equation will be those defining the hyperbola \((s-a)(u-a)=b\) along which we will define our hyperbolic dispersion relations in the next section. For a given

*t*, \(s_b\) is the value of

*s*that lies in the previous hyperbola. In order to compare with the expressions in [27], where \(a=0\), we have kept just the first order in the

*b*/

*t*expansion, although its numerical effect is rather small.

Values of Regge parameters involving strangeness. They are all allowed to vary from our UFD to our CFD sets with the exception of \(\alpha _{K^*}\) and \(\alpha '_{K^*}\), since they are both determined from linear Regge trajectory fits to strange resonances

Regge | UFD | CFD |
---|---|---|

\(f_{K/\pi }\) | 0.66 fixed | 0.66 fixed |

\(g_{K/\pi }\) | 0.53 fixed | 0.53 fixed |

| 0.05 ± 0.010 | 0.052 ± 0.010 |

\(\alpha _{K^*}\) | 0.352 | 0.352 |

\(\alpha '_{K^*}\) | 0.882 GeV\(^{-2}\) | 0.882 GeV\(^{-2}\) |

\(\lambda \) | 11.0 ± 5.0 | 10.7 ± 5.0 |

A final remark on the size of Regge contributions is in order. As commented in the introduction, in the next sections we will obtain partial-wave dispersion relations by integrating hyperbolic dispersion relations. This is an integral over *b* for a family of \((s-a)(u-a)=b\) hyperbolas, while \(a=-10.8 M_\pi ^2\) is fixed to the value that maximizes the applicability region (see Appendix D). This means that the exponent \(\alpha _{K^*}+a \alpha '_{K^*}<\alpha _{K^*}\) and thus the Regge contribution to \(\pi \pi \rightarrow {{\bar{K}}}K\) in this work, for the same number of subtractions, is suppressed with respect to its size in [27], where \(a=0\). This will allow us to consider less subtractions without Regge contributions growing large.

## 4 Hyperbolic dispersion relations and sum rules

Our goal is to calculate a set of parameterizations that describe the data up to 1.47 GeV consistently with hyperbolic dispersion relations (HDR). As already advanced in the introduction, in this work we will consider a set of hyperbolas \((s-a)(u-a)=b\) and use *a* to maximize the energy domain where the hyperbolic dispersion relations hold. Note that the phenomenology of the \(\pi \pi \rightarrow K {\bar{K}}\) \(a=0\) case has been studied in detail in [27, 52, 53]. Moreover, HDR with \(a=0\) were also used for the study of the \(K_0^*(800)\) resonance [26].

In addition, we will use the smallest number of subtractions needed for each channel. This has the advantage that our equations for \(g_0^0\) and \(g_1^1\) are independent from one another. In contrast, in [27] they use more subtractions and the subtraction constants are constrained by means of sum rules that mix the dispersive representations of both waves.

### 4.1 Hyperbolic dispersion relations

*s*and

*u*on these hyperbolas are the following functions of

*t*:

*s*and

*u*that lie in the hyperbola \((s-a)(u-a)=b\) for a given value of

*t*. Now, we want to rewrite the subtraction constant

*h*(

*b*,

*a*) and for this we follow the procedure in [39, 52, 53]. We thus introduce the following fixed-

*t*dispersion relation

*c*(

*t*) and

*h*(

*b*,

*a*) are determined. Actually, Eq. (35) can be rewritten as:

*a*parameter to maximize the applicability region of the HDR once projected into partial waves, which we will do in the next subsection.

Before finishing this subsection, a comment on the high energy region is in order. We have three different kinds of contributions above 2 GeV, the first one is \(G^I(t',s'_b)\), which can be calculated from Eq. (29). The second kind is the evaluation of \(F^{\pm }(s',0)\): for the symmetric amplitude we just use Eq. (25), while for the anti-symmetric one we use Eq. (27). The last kind is for \(F^\pm (s',t'_b)\), which corresponds to an exotic exchange, so that its contribution is negligible.

### 4.2 Partial-wave hyperbolic dispersion relations

*a*parameter, we can now use it to maximize the applicability of the equations right above. Note there are constraints coming from the applicability of the HDR in Eqs. (33) and (37) as well as from the convergence of the partial-wave expansion. As shown in Appendix D, by setting \(a=-10.8m_{\pi }^2\) the applicability range of these equations is \(-0.286 \,\mathrm{GeV}^2\le t\le 2.19 \,\mathrm{GeV}^2\). In other words, we can study the physical region from the \(K {{\bar{K}}}\) threshold \(\simeq 0.992\,\mathrm{GeV}\) up to \(\simeq 1.47\,\mathrm{GeV}\). In contrast, the usual HDR projected into partial waves are only valid up to \(\simeq 1.3,\mathrm{GeV}\). Thus, with our choice of

*a*, the applicability of the dispersive approach in the physical region, where we can test or use data as input, has been extended by 55% in terms of the \(\sqrt{t}\) variable, or 67% in terms of

*t*.

As can be directly seen in Eq. (39) the \(g^1_1(t)\) partial wave does not have any scattering length as input parameter and its dominant contribution to the integral comes from its own imaginary part. Since it is not subtracted, the Regge contribution is not negligible, but we have already attached a conservatively large uncertainty to its residue and we will see that it barely changes when using the dispersive representation as a constraint on data. In the case of even partial waves, one subtraction is necessary to ensure the convergence, and hence the output is always influenced by the scattering lengths coming from \(\pi K \) scattering. In this work we fix them to the values obtained in [18], which are also compatible with the Roy–Steiner prediction in [27]. As already commented, an important advantage of using HDR with the smaller possible number of subtractions is to decouple odd and even partial waves. For example in [27] the Roy–Steiner equation for \(g^0_0\) uses \(g^1_1\) as input.

Finally, we want to remark that, as usual, the high energy part of the integrals in Eq. (39) is obtained by projecting into the corresponding partial-wave the high-energy part of the integrals in Eqs. (33) and (37), where Regge theory was used as input as explained in previous sections.

### 4.3 The unphysical region and the Muskhelishvili–Omnès problem

*t*lies in the real axis above the \(\pi \pi \) threshold, a principal value must be understood on each integral. In addition, between \(\pi \pi \) threshold and \(t_m\) on the left hand sides the amplitude is reduced to its modulus (since by construction the Omnés function removes the phase), whereas above \(t_m\) it is reduced to its real part.

Since in the next sections we will choose \(t_m\) with \(\phi ^0_0(t_m)\ge \pi \) we have introduced one subtraction for the \(g^0_0(t)\) Omnès solution in order to ensure the convergence when \(t\rightarrow t_m\). The subtraction constant \(\alpha \) will be obtained by imposing numerically a no-cusp condition on \(t_m\) for \(g^0_0(t)\).

The interest of these equations is that for a given \(g^I_\ell (t)\), the integrals *in the unphysical region* only make use of the phases and the \(\Delta ^I_\ell \). But thanks to Watson’s Theorem the former are known from \(\pi \pi \) scattering, which we take from the dispersive analysis of [17], and the latter do not involve \(g^I_\ell (t)\) itself, but only partial waves with \(\ell '-\ell \ge 2\). These higher partial waves are suppressed in the unphysical region with respect to that with \(\ell \). We also need input from \(K \pi \) scattering that is known and we take it from our recent dispersive data analysis in [18]. Thus we can directly solve \(g^1_1(t)\) and \(g^0_2(t)\), for which we have explicitly checked that the \(\ell =3\) and \(\ell =4\) contributions are small and negligible, respectively. Once we have \(g^0_2(t)\) we can use it as input to solve Eq. (45) for \(g^0_0(t)\).

It is worth noticing here that, in purity, for the Regge contributions to \(\Delta ^I_\ell (t)\), one has to subtract the projection of the Regge amplitude itself into the desired \(I,\ell \) partial wave. Fortunately this projection is negligible, and our solutions do not depend on this procedure.

We still have to discuss the choice of \(t_m\), which is always above the \(K {{\bar{K}}}\) threshold. It is important to recall that the derivation of the above equations implies that \(g_{output}(t_m)=g_{input}(t_m)\). This condition will always be forced into the output no matter if the data at that energy is in good or bad agreement with dispersion relations. If the data at that energy region were not close to the dispersive solution, the output would be forced to describe it and the result could be strongly distorted in other regions. In particular the \(g^0_0\) wave is the most sensitive to this instability, the effect is more moderate on the \(g^0_2\) and negligible for the \(g^1_1\) because it is already very consistent for any \(t_m\) choice. Thus, we have studied what energy region is the most consistent for \(g^0_0\) when changing \(t_m\) and we have found that there are two regions that yield systematically rather consistent results between input and output: one around \(\sqrt{t_m}=1.2\, \mathrm{GeV}\), which is also valid for \(g_2^0\), and another one around \(\sqrt{t_m}=1.47\, \mathrm{GeV}\). However, if we chose the latter, we find that the uncertainty in the dispersive result between \(K {{\bar{K}}}\) and 1.2 GeV is so large that there is no dispersive constraint in practice, having larger uncertainties could even produce both \(g^0_0(t)\) solutions to be compatible between them. Moreover by looking at Eqs. (45), (46) and (47) one can notice that \(t_m\) marks the energy above which \(\vert g_\ell ^I\vert \) is used as input for its own equation. Since we are actually trying to test the data parameterizations, within our approach we would like to maximize that region and choose the smaller possible \(t_m\). All in all, we have made the final choice \(\sqrt{t_m}=1.2\, \mathrm{GeV}\) for all partial waves. This is a point above \(K{{\bar{K}}}\) threshold where there are no cusps coming from the two most important inelasticities (\(K{{\bar{K}}}\), \(\eta \eta \)). In particular, the \(g^0_2\) is well controlled at this energy since its largest contribution comes from the \(f_2(1270)\), a very well-known resonance very close to \(t_m\).

## 5 Consistency check of unconstrained fits

As we explained before, Eqs. (45), (46), (47) yield the modulus of the partial wave below \(t_m\) and the real part above. However, in order to simplify our plots and calculations, we will just display the modulus. In particular by “input” we will understand the modulus of the partial wave on the left hand side of Eqs. (45), (46), (47), i.e. as obtained directly from our fits. Similarly, by “output” we will always mean the modulus of the dispersive representation. Note that for \(t<t_m\) this modulus is obtained from the right hand side of those equations with principal values on each integral. However, for \(t>t_m\) only the real part is obtained from the integrals and the modulus is reconstructed by adding the imaginary part from the direct parameterizations.

With the above definition we can study the consistency of each partial-wave dispersion relation. It will be well satisfied on the average if its corresponding \(d^2\le 1\). In case of disagreement it is also relevant to check whether it comes from a particular energy region and for this we will show figures comparing the input and output as a function of \(\sqrt{t}\).

### 5.1 \(g^1_1\) UFD check

As can bee seen in Fig. 5 the dispersion relation in Eq. (46) is remarkably well satisfied, with a total \(d^2=1\). Such a nice agreement was expected since it has a large contribution from the \(\rho (770)\) that dominates \(\pi \pi \) scattering in this channel below \(K {{\bar{K}}}\) threshold, and our input from [18] is already consistent with \(\pi \pi \) data and dispersion relations. Let us now recall that the \(\pi \pi \rightarrow K {{\bar{K}}}\) data we use as input show large uncertainties and fluctuations (see Fig. 1). Our UFD description does not follow visually all these fluctuations but, roughly speaking, it averages them and rises softly and monotonously. Still, our UFD is remarkably consistent with the dispersive representation. Actually we have checked that parameterizations with more oscillations may describe the central values of the data points better, but satisfy worse the dispersive representation than our UFD fit. In the \(\pi \pi \rightarrow K {{\bar{K}}}\) physical region we had also included resonant shapes for the \(\rho '\) and \(\rho ''\) resonances in our UFD. As seen from our results, the parameters and shape of the \(\rho '\), which for a good part lies within the applicability region of our equations, are fairly consistent with dispersion relations. As commented in Sect. 3.2.1 the \(\rho ''\) was used just as a simple form to parameterize the amplitude at energies beyond the reach of our dispersive representation where scattering data do not exist.

One could also be worried that, since the \(g^1_1\) dispersion relation has no subtractions, it may require some tuning on the Regge asymptotics and the \(\lambda \) parameter we estimated with the Veneziano model and degeneracy in Sect. 3.3. However the nice fulfillment of the dispersion relation yields strong support for our \(\lambda \) estimations.

### 5.2 \(g^0_2\) UFD check

### 5.3 \(g^0_0\) UFD check

Finally, for the scalar-isoscalar dispersion relation in Eq. (45), we need both the \(g^0_0(t)\) and \(g^0_2(t)\). In this case, partial waves with \(\ell \ge 4\) are totally negligible below 2 GeV. In Fig. 7 we show the results of the \(g^0_0(t)\) dispersion relation when using either the \(\hbox {UFD}_\text {B}\) or \(\hbox {UFD}_\text {C}\) parameterizations as input. In both cases the agreement is poor, particularly due to the results in the region 10–20 MeV above \(K{{\bar{K}}}\) threshold, where the dispersive solution increases rapidly. This feature is common to both the \(\hbox {UFD}_\text {B}\) and \(\hbox {UFD}_\text {C}\) and is due to the influence of the \(f_0(980)\). The respective \(d^2=5.6\) and \(d^2=2.7\) are dominated by this near threshold region. There is a clear need for improvement, that we will achieve by imposing dispersion relations as constraints in the next section, although in both cases the disagreement in the region very near threshold will linger on. However, we will see that for both solutions a very good consistency with dispersion relations can be achieved except for the very near threshold region.

Finally, let us remark that the \(g_0^0\) partial-wave dispersion relation in Eq. (45) depends on the \(\pi K\) scattering length \(a^+_0\). We have checked that the dispersion relation would be better satisfied if we used a somewhat lower value of \(a^+_0\) than that obtained in our previous work [18] (which was also compatible with Roy–Steiner determinations [27]). Since in this work we are considering \(\pi K\) scattering amplitudes as fixed input, we keep the value from the \(\pi K\) constrained fit, but this result could be relevant for future re-analysis of \(\pi K\) scattering data.

## 6 Constrained fits to data

Therefore, we have just seen that the data on the \(g_2^0\) and even more so on the \(g_0^0\) do not satisfy very well the dispersive representation. There is clear room for improvement. Thus, in this section we will impose the dispersion relations in Eqs. (45), (46), (47) as constraints of the fits. In this way we will obtain a set of constrained fits to data (CFD) which fulfillment of the dispersive representation will be much improved. In this section we use the same functional forms for the amplitudes that we used in Sect. 3, but the parameters change from the UFD to the CFD sets. In general the difference between the UFD and CFD parameters is small, with a few exceptions. Nevertheless, due to large correlations in the parameters, even if some CFD parameters deviate from the UFD set, the resulting UFD and CFD curves are typically consistent with one another at the 1 or 1.5 \(\sigma \) level. Only for the constrained analysis of the \(\hbox {UFD}_\text {C}\), the \(\hbox {CFD}_\text {C}\) \(g_0^0\) partial wave deviates by about 2 \(\sigma \) in the region from 1.25 to 1.45 GeV, but it still compatible with the upper error bars of the data. Hence the CFD description of data is still rather good.

*k*th data point for the modulus and the phase, respectively, and \(\delta |g^I_\ell |_{exp,k},\delta (\phi ^I_\ell )_{exp,k}\) are their corresponding errors. The weights \(W_1^2\), \(W^2_2=W'^2N/(N+N')\), \(W^2_3=W'^2N'/(N+N')\) are used to roughly take into account the degrees of freedom needed to parameterize the curves that describe the modulus and the phase. For simplicity we have chosen the same \(W_1^2=5\) and \(W'^2=12\) value for all partial waves as an average value of their degrees of freedom. Note that we actually minimize the sum of this function over the three partial waves of interest \((I,\ell )=(0,0),(1,1)\) and (0, 2). In addition, recall that, as explained in Sect. 3.2.2, we have added two points to the \(\chi ^2\)-function to take into account the experimental mass of the \(f_2\) and \(f_2'\) resonances.

Let us remark that in previous works our procedure was slightly different: we defined a similar \(\chi ^2\)-like function but in terms of the unconstrained fit parameters, which were not allowed to vary much from their unconstrained best values. In contrast, in Eq. (49) we define our \(\chi ^2\)-like function directly in terms of data, not the unconstrained fit parameters. The reason is that in this work the onset of Regge parameterizations is 2 GeV and thus we use our partial-wave parameterizations to describe data from \(K {{\bar{K}}}\) threshold up to 2 GeV. However, the dispersion relations are only applicable up to 1.47 GeV. If we constrained only the fit parameters with the dispersion relations, which affect only the lower-energy data, we would obtain large artificial deviations in the description of the higher-energy data. With the procedure we use here, and contrary to what happened in previous works, if there are some strongly correlated parameters, we can see that their constrained values can deviate appreciably from their unconstrained best values but still the constrained and unconstrained curves look very similar. As the uncertainty variation is of second order, and parameters that are not compatible with old values deviate by a small number of sigmas at most, we still maintain their uncertainties as they are a reliable and almost unchanged estimate of the error, as one can see in the final uncertainty band plotted in the figures for the CFD parameterizations.

### 6.1 Constrained \(g^ 1_1(t)\) partial wave

Let us recall that the UFD \(I=1,\ell =1\) wave from \(K{{\bar{K}}}\) threshold up to 1.47 was already consistent with the dispersive representation. By imposing our dispersion relations \(d^2\) decreases just from 1 to 0.6. The difference between the constrained input and dispersive output for the \(g^1_1\) wave can be seen in Fig. 8.

The new CFD parameters can be found in Table 1 where it can be checked that the CFD values are remarkably consistent with the UFD ones: only two are beyond one standard deviation but not more than 2 \(\sigma \). As we are using a non-subtracted HDR to study the odd angular momentum partial waves, the small improvement in the description of this partial wave comes mostly from the slight variation of the Regge parameters. Nevertheless, as it can be seen in Table 7, our CFD result for the \(\lambda \) Regge parameter is compatible with its UFD value, thus supporting the degeneracy between the \(\rho \) and \(K^*\) families.

### 6.2 Constrained \(g^0_2(t)\) partial wave

For this wave the agreement was not as good as for the \(I=1\) and \(\ell =1\) partial wave, particularly in the threshold region. After minimization the overall agreement has improved considerably, from \(d^2=1.6 \) down to 1.1. However, as seen in Fig. 11, our CFD parameterization still shows some small discrepancy with its dispersive output near threshold, although the deviation has improved substantially in that region compared to the unconstrained case.

This improvement is achieved without changing much the CFD parameterization with respect to the UFD. The CFD parameters change little from their previous UFD values, as seen in Table 2. In addition, in Fig. 12 we can see that the deviations from the UFD to the CFD modulus are almost imperceptible. There are some differences near threshold but, unfortunately, when plotting the modulus together with data, the resulting curves look almost identical due to a \(q(s)^5\) factor. In contrast, we can see in Fig. 13 some small difference between the UFD and CFD phase \(\phi ^0_2\). This change is actually the one mostly responsible for the improvement in the \(d^2\).

We have also checked that the values obtained at the \(K {{\bar{K}}}\) threshold still fulfill Watson’s Theorem when using the \(\pi \pi \) scattering values obtained from dispersion relations [17, 62]. One should be careful not to force too much the fit in the threshold region because, as commented in the UFD case, this could spoil the \(f_2(1270)\) mass, which is very well established from different experiments, not just scattering. That is why we considered the \(f_2\) and \(f'_2\) masses as additional data points when fitting the \(\pi \pi \rightarrow K {{\bar{K}}}\) data. We have also added this extra contribution when minimizing the \(\chi ^2\) to obtain the CFD set.

Finally, let us note that this dispersion relation has some sensitivity to \(\pi K\) scattering, in particular to the scalar partial wave. A more thorough study would require allowing the \(\pi K\) scattering amplitude to vary when imposing the hyperbolic dispersion relations as constraints, but that is well beyond the scope of this work dedicated to \(\pi \pi \rightarrow K {{\bar{K}}}\), where we have taken \(\pi K\) scattering as fixed input.

### 6.3 Constrained \(g^0_0(t)\) partial wave

The scalar partial wave \(g^0_0\) is the most interesting in this work, given that we are dealing with two incompatible sets of experimental data for the modulus and also because neither of them are consistent with the dispersive representation.

As seen in Sect. 3, on the one hand we have the Brookhaven-II [9] data and, on the other hand, the data of Brookhaven-I [8] and Argonne [7]. From these two sets we obtained the \(\hbox {UFD}_\text {B}\) and \(\hbox {UFD}_\text {C}\) parameterizations, respectively. For the phase we had a single UFD parameterization. Let us recall that the overall \(\hbox {UFD}_\text {C}\) agreement with its dispersive output up to 1.47 GeV is poor, with \(d^2=2.7\), whereas the \(\hbox {UFD}_\text {B}\) is even more inconsistent with \(d^2=5.6\). In that respect the \(\hbox {UFD}_\text {B}\) parameterization may seem disfavored. However, the \(\hbox {UFD}_\text {C}\) modulus is clearly incompatible with the value that would be obtained from the inelasticity of \(\pi \pi \) scattering obtained from dispersion relations [17] assuming two coupled channels, \(\pi \pi \) and \(K{{\bar{K}}}\). For that reason we will study here both \(\hbox {UFD}_B\) and \(\hbox {UFD}_C\) and will obtain a fit to each data set constrained with our dispersion relation in Eq. (45). We will see that after this process both constrained solutions will be equally acceptable with respect to their consistency regarding dispersion relations.

Let us note that we now use as input the \(g^0_2\) CFD parameterization obtained in the previous subsection. The consistency test of the constrained \(g^0_0\) results can be found in Fig. 14. It can be seen that we obtain an equally good consistency for both the \(\hbox {CFD}_\text {B}\) and \(\hbox {CFD}_\text {C}\) parameterizations except for the region very close to threshold. The behavior in this region is controlled by the \(f_0(980)\) shape in the elastic region of \(\pi \pi \) scattering and thus is out of the scope of this work, since we consider it input. The rest of the energy region up to 1.47 GeV has values of \(d^2\) below one.

In Fig. 15 we also compare both CFD parameterizations against their respective UFD parameterizations and the data. There one can see that the UFD and CFD phases are almost identical, except in the 1.1–1.2 GeV region where the CFD is higher by more than one standard deviation, and in the 1.9 GeV region where the CFD phase is again higher but well within uncertainties. Actually there are two \(\hbox {CFD}_\text {B}\) and \(\hbox {CFD}_\text {C}\) phases but they are totally indistinguishable.

Concerning the modulus, the \(\hbox {UFD}_\text {C}\) and \(\hbox {CFD}_\text {C}\) are compatible, whereas the \(\hbox {CFD}_\text {B}\) is slightly lower than the \(\hbox {UFD}_\text {B}\) in the 1.05–1.15 region, but clearly higher in the 1.3–1.45 region. These differences go above the 2-\(\sigma \) level, so that they lie still reasonable close to the data, but prefer to cross the top of the experimental uncertainty bars.

Note that the “dip” structure in the inelasticity from \(\pi \pi \) scattering occurs around 1.1 GeV, whereas the biggest difference between the in \(\hbox {UFD}_\text {B}\) and the \(\hbox {CFD}_B\) is found above 1.25 GeV, so that we conclude that such a dip is not the cause of the deviation for the \(\hbox {UFD}_\text {B}\) set. The dip structure favored by \(\pi \pi \) scattering dispersive analyses can therefore be accommodated also with the hyperbolic dispersive representation of \(\pi \pi \rightarrow K {{\bar{K}}}\).

Therefore we conclude that the data most commonly used in the literature (Argonne [7]) is not necessarily the only acceptable solution and that one does not have to ignore the Brookhaven-II data. Actually, we have shown that with the \(\hbox {CFD}_B\) solution the Brookhaven-II data can also be fairly well described while being consistent with \(\pi \pi \rightarrow K {{\bar{K}}}\) dispersion relations and with the dispersive determination of the inelasticity in \(\pi \pi \) scattering that, in contrast, is not consistent with the Argonne data. In this sense the \(\hbox {CFD}_\text {C}\) is disfavored against the \(\hbox {CFD}_\text {B}\) set.

## 7 Conclusions and outlook

In this work we have performed a dispersive study of \(\pi \pi \rightarrow K{{\bar{K}}}\) scattering by means of partial-wave dispersion relations of the Roy–Steiner type, i.e. based on hyperbolic dispersion relations. While other studies with similar equations used dispersion theory to obtain information on the sub-threshold region, we have also used them for the first time in the physical region. Moreover, we have derived a set of equations based on \((s-a)(u-a)=b\) hyperbolae in which we have obtained the value of *a* that maximizes the applicability range of these hyperbolic dispersion relations. Compared to the existing \(a=0\) case we have increased the applicability range of the hyperbolic partial-wave dispersion relations in the physical region by 67% in the *t* variable. This has allowed us to study dispersively the existing data sets on \(\pi \pi \rightarrow K{{\bar{K}}}\) up to 1.47 GeV.

In particular, on a first step we have obtained a set of unconstrained fits to data (UFD) for each partial wave \(g_\ell ^I(t)\), where \(\ell \) and *I* are the angular momentum and isospin, respectively. For the case of the scalar-isoscalar wave \(g_0^0\) we have provided two alternative fits, called \(\hbox {UFD}_\text {B}\) and \(\hbox {UFD}_\text {C}\), to differentiate between fits to two conflicting sets of data. In addition, we have provided high energy parameterizations for \(\pi \pi \rightarrow K {{\bar{K}}}\) scattering, based on factorization and Regge theory, that we need for the high energy part of our dispersive integrals. We have then tested these UFD parameterizations against our dispersion relations. We have found that the *P* wave UFD is very consistent with dispersion relations. Also, the *D* wave is crudely consistent with these equations, although there is clear room for improvement. In contrast, we have found that the unconstrained fits to both solutions of the scalar-isoscalar wave show a significant inconsistency with the dispersive representation, particularly, but not only, near threshold. These deviations are not related to the high energy input, and thus they become a first warning to the phenomenological use of simple fits to the existing data.

Next, we have provided a new set of fits to data using the hyperbolic partial-wave dispersion relations as constraints. For the *P* and *D* waves, these constrained fits to data (CFD) satisfy their dispersion relations within uncertainties while describing very well the experimental data. There is only some relatively small tension in the D-wave threshold region. In particular we have shown that a simple description of the D-wave threshold region with a simple Breit–Wigner parameterization of the nearby \(f_2(1270)\) resonance is not acceptable.

We have also found that, with the exception of the region very close to threshold, both constrained parameterizations of the \(g_0^0\) wave, labeled \(\hbox {CFD}_\text {B}\) and \(\hbox {CFD}_\text {C}\), satisfy well the dispersion relations, while still describing reasonably well their respective sets of data. Nevertheless some systematic deviations from the data central values are needed in order to satisfy the dispersive representation, particularly for the \(\hbox {UFD}_\text {B}\) in the region between 1.25 and 1.45 GeV. This becomes a second warning towards considering only the most popular data set described by \(\hbox {UFD}_\text {C}\): the data on which the \(\hbox {UFD}_\text {C}\) set is based can be also described consistently with hyperbolic partial-wave dispersion relations, and is favored by previous \(\pi \pi \) scattering dispersive analysis. This second set should definitely not be discarded, if not directly favored against the most popular one.

In conclusion, our constrained data fits provide reliable, precise and simple parameterizations of data on S, P and D partial waves up to 2 GeV, which are consistent with the hyperbolic dispersive representation up to its maximum applicability limit of 1.47 GeV.

As an outlook for this work, our constrained parameterizations could be used by both the theoretical and experimental hadron communities as input for other processes. Actually, in the near future we plan to use them for further studies. For example: to implement re-scattering effects in CP violating decays involving pions and kaons, or to study the much debated \(f_0(1370)\) and \(f_0(1500)\) resonance by means of model-independent methods based on analyticity, or combined with \(\pi \pi \) scattering determinations, to obtain a precise determination of the \(a_0^\pm \) scattering lengths from sum rules. Finally, we will use them as input for a similar dispersive analysis of \(K \pi \) scattering data and the rigorous and precise determination of light-strange resonance parameters. In particular, this input will be very useful for a precise determination of the elusive \(K_0^*(800)\), by analyzing data using hyperbolic partial-wave dispersion relations of the type derived here.

**Note Added in Proof** While completing the publication of this manuscript we have become aware that the \(K_0^*(800)\) resonance it is now called \(K_0^*(700)\) in the new edition of the Review of Particle Physics [71].

## Notes

### Acknowledgements

JRP and AR are supported by the Spanish project FPA2016-75654-C2-2-P. AR would also like to acknowledge the financial support of the Universidad Complutense de Madrid through a predoctoral scholarship. We would also like to thank B. Moussallam and J. Ruiz de Elvira for fruitful discussions, as well as J. Miranda for her comments and corrections.

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