Gv. Khazanov et al., EFFECT OF ANISOTROPIC THERMAL-CONDUCTIVITY ON THE TEMPERATURE STRUCTURE OF THE IONOSPHERE-PLASMASPHERE SYSTEM, J GEO R-S P, 101(A6), 1996, pp. 13399-13406
Anisotropic plasma hydrodynamics makes use of two heat fluxes represen
ting the transfer of field-aligned and transverse (with respect to the
external magnetic field) energies to describe thermal energy transfer
. This is a considerably more complex treatment than isotropic plasma
hydrodynamics in which only one heat flux component is considered. The
present work analyzes the heal flux structure within the framework of
anisotropic hydrodynamics and examines the effect of the anisotropic
heat fluxes on the thermal plasma distribution both in the ionosphere
and in the magnetically connected plasmasphere. The dependence of heat
conductivities on the anisotropy parameter a=T-perpendicular to/T-par
allel to is studied (T-perpendicular to and T-parallel to are transver
se and field-aligned temperatures, respectively). The heat conductivit
ies increase with field-aligned temperature (with decreasing value of
a), thereby enhancing the thermal energy transfer. The analytical solu
tion obtained for the heat conduction equation is used to examine the
effect of the electron energy distribution anisotropy on the electron
temperature in the plasmasphere. The dependence of heat conductivity o
n the parameter a has been shown to result in a variation of electron
temperature compared with the isotropic case (a=1). The calculated pla
smaspheric temperature values rise when a > 1 and fall when a < 1. The
strongest effect of the temperature anisotropy on the derived value o
f the electron temperature occurs at high altitudes along a flux tube
in the vicinity of the equatorial plane. Predictions of this simplifie
d analytical model are compared to observations of temperature anisotr
opies in the ionosphere. Basic agreement in the magnitude and sense of
the electron temperature anisotropy between the model and observation
s is found.