Dual-spacecraft observations of standing waves in the magnetosheath

An unambiguous determination of the wave modes observed in plasma turbulenc e requires the determination of the dispersion characteristics of the wave. The method adopted for the determination of the wave dispersion relation i s based upon the study of the phase difference of the waves at two closely separated spacecraft [Balikhin and Gedalin, 1993]. It is applied to observa tions of waves in the magnetosheath magnetic field made by AMPTE UKS and AM PTE IRM, We show that the observed waves are propagating in the sunward dir ection but are convected toward the magnetopause by the plasma, flow. As a result, the observed waves are quasi-standing in the flow. These waves have been previously identified as either slow or mirror modes depending the pr ocedure adopted for their analysis. They may also be an experimental observ ation of the mirror and slow (MIAOW) waves identified near the magnetopause boundary in the hybrid simulations of Omidi and Winske[1995]. The observed waves possess short wavelengths (A) such that R-Bi/gimel approximate to 1 (where R-Bi is the ion Larmor radius). Thus they may only be studied analyt ically within the framework of the kinetic approximation. Both the nonlinea r amplitudes and possibly the strong underlying inhomogeneity are responsib le for the significant differences between the properties of the observed m odes and those resulting from linear homogeneous kinetic theory.