Dynamics of the inner magnetosphere near times of substorm onsets

被引:128
作者
Maynard, NC
Burke, WJ
Basinska, EM
Erickson, GM
Hughes, WJ
Singer, HJ
Yahnin, AG
Hardy, DA
Mozer, FS
机构
[1] BOSTON UNIV, CTR SPACE PHYS, BOSTON, MA 02215 USA
[2] PHILLIPS LAB, BEDFORD, MA 01731 USA
[3] UNIV CALIF BERKELEY, SPACE SCI LAB, BERKELEY, CA 94720 USA
[4] NOAA, SPACE ENVIRONM LAB, BOULDER, CO 80303 USA
[5] POLAR GEOPHYS INST, APATITY 184200, RUSSIA
关键词
D O I
10.1029/95JA03856
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
The electrodynamics of the inner magnetosphere near times of substorm onsets have been investigated using CRRES measurements of magnetic and electric fields, energetic electron fluxes, in conjunction with ground-based observations. Six events were studied in detail, spanning the 2100 to 0000 MLT sector and L values from 5 to 7. In each case the dawn-dusk electric field was enhanced over typical background electric fields, and significant, low-frequency pulsation activity was observed. The amplitudes of the pulsations were larger than the background electric fields. Dusk-dawn excursions of the cross-tail electric field often correlated with changes in currents and particle energies at CRRES and with ULF wave activity observed on the ground. Variations of the electric field and Poynting vectors with periods in the Pi 2 range are consistent with bouncing Alfven waves that provide electromagnetic communication between the ionosphere and plasma sheet. Magnetic signatures of field-aligned current filaments directed away from the ionosphere, presumably associated with the substorm current wedge, were observed during three orbits. In all cases, ground signatures of substorm expansion were observed at least 5 min before the injection of electrons at CRRES. Field-aligned fluxes of counter-streaming, low-energy electrons were detected after three of the injections. We develop an empirical scenario for substorm onset. The process grows from ripples at the inner edge of the plasma sheet associated with dusk-dawn excursions of the electric field, prior to the beginning of dipolarization. Energy derived from the braking of the inward plasma convection flows into the ionosphere in the form of Poynting flux. Subsequently reflected Poynting flux plays a crucial role in the magnetosphere-ionosphere coupling. Substorms develop when significant energy (positive feedback?) hows in both directions, with the second cycle stronger than the initial. Pseudobreakups occur when energy flow in both directions is weak (negative feedback?). ''Explosive-growth-phase'' signatures occur after onset, early in the substorm expansion phase. Heated electrons arrive at the spacecraft while convection is earthward, during or at the end of electromagnetic energy flow away from the ionosphere.
引用
收藏
页码:7705 / 7736
页数:32
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