RADIAL PROFILES OF QUIET TIME MAGNETOSPHERIC PARAMETERS

被引:172
作者
LUI, ATY [1 ]
HAMILTON, DC [1 ]
机构
[1] UNIV MARYLAND, DEPT PHYS & ASTRON, COLLEGE PK, MD 20742 USA
关键词
D O I
10.1029/92JA01539
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Magnetospheric plasma parameters during geomagnetically quiet conditions are studied with ion measurements covering energies from approximately 1 keV to approximately 4 MeV from the Charge Composition Explorer. It is found that the observed quiet time plasma pressure in the midnight sector is comparable (within a factor of 2) to that deduced by Spence et al. (1989) and Kan et al. (1992) from inverting the magnetic field models of Tsyganenko and Usmanov (1982) and Tsyganenko (1987). The radial profile of the total plasma pressure shows a peak generally at L almost-equal-to 3 to 4 and decreases from L almost-equal-to 4 to L almost-equal-to 9 rather monotonically. No large-scale earthward decrease in plasma pressure occurs in these outer L shells, contrary to some theoretical expectation for the magnetospheric closure of the region 2 field-aligned current system. The plasma pressure within L approximately 9 is generally anisotropic with a larger pressure component perpendicular to the magnetic field than parallel to the field. This anisotropy tends to increase with smaller L. While the anisotropy is always below the fire hose instability threshold during all quiet time passes studied, it is near the mirror instability threshold in the midnight sector at large L shells due mostly to the large value of plasma beta (>1) there. The radial profile of the azimuthal volume current density is also computed, with the result suggesting that the current density associated with the quiet time ring current population is distributed broadly over the L shells between L almost-equal-to 3.5 and L almost-equal-to 7 with average values in the range of approximately 1 to 4 nA/m2 and peak values in the range of approximately 4 to 8 nA/m2. Another current region situated beyond L almost-equal-to 7, which may be related to the inner portion of the quiet time cross-tail current, is also apparent and has average and peak current density values similar to those of the ring current.
引用
收藏
页码:19325 / 19332
页数:8
相关论文
共 18 条
[1]   AVERAGE PLASMA PROPERTIES IN THE CENTRAL PLASMA SHEET [J].
BAUMJOHANN, W ;
PASCHMANN, G ;
CATTELL, CA .
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 1989, 94 (A6) :6597-6606
[2]   THE IONOSPHERE AS A FULLY ADEQUATE SOURCE OF PLASMA FOR THE EARTHS MAGNETOSPHERE [J].
CHAPPELL, CR ;
MOORE, TE ;
WAITE, JH .
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 1987, 92 (A6) :5896-5910
[3]   PLASMA CLOUDS IN MAGNETOSPHERE [J].
DEFOREST, SE ;
MCILWAIN, CE .
JOURNAL OF GEOPHYSICAL RESEARCH, 1971, 76 (16) :3587-+
[4]   THE CHARGE-ENERGY MASS SPECTROMETER FOR 0.3-300 KEV/E IONS ON THE AMPTE CCE [J].
GLOECKLER, G ;
IPAVICH, FM ;
STUDEMANN, W ;
WILKEN, B ;
HAMILTON, DC ;
KREMSER, G ;
HOVESTADT, D ;
GLIEM, F ;
LUNDGREN, RA ;
RIECK, W ;
TUMS, EO ;
CAIN, JC ;
MASUNG, LS ;
WEISS, W ;
WINTERHOF, P .
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 1985, 23 (03) :234-240
[5]  
HASEGAWA A, 1975, PLASMA INSTABILITIES, P94
[6]   LARGE-SCALE CHARACTERISTICS OF MAGNETOSPHERIC EQUATORIAL CURRENTS [J].
IIJIMA, T ;
POTEMRA, TA ;
ZANETTI, LJ .
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 1990, 95 (A2) :991-999
[7]   ISOTROPIZED MAGNETIC-MOMENT EQUATION OF STATE FOR THE CENTRAL PLASMA SHEET [J].
KAN, JR ;
BAUMJOHANN, W .
GEOPHYSICAL RESEARCH LETTERS, 1990, 17 (03) :271-274
[8]   A HYBRID EQUATION OF STATE FOR THE QUASI-STATIC CENTRAL PLASMA SHEET [J].
KAN, JR ;
SUN, W ;
BAUMJOHANN, W .
GEOPHYSICAL RESEARCH LETTERS, 1992, 19 (04) :421-424
[9]   ON THE POSSIBILITY OF QUASI-STATIC CONVECTION IN THE QUIET MAGNETOTAIL [J].
KIVELSON, MG ;
SPENCE, HE .
GEOPHYSICAL RESEARCH LETTERS, 1988, 15 (13) :1541-1544
[10]   MAGNETIC STORM OF SEPTEMBER 4, 1984 - A SYNTHESIS OF RING CURRENT SPECTRA AND ENERGY DENSITIES MEASURED WITH AMPTE CCE [J].
KRIMIGIS, SM ;
GLOECKLER, G ;
MCENTIRE, RW ;
POTEMRA, TA ;
SCARF, FL ;
SHELLEY, EG .
GEOPHYSICAL RESEARCH LETTERS, 1985, 12 (05) :329-332