Energy flux in the Earth's magnetosphere: Storm - Substorm relationship

被引:4
|
作者
Alexeev, II [1 ]
机构
[1] Moscow MV Lomonosov State Univ, Scobeltsyn Inst Nucl Phys, Moscow 119992, Russia
关键词
magnetospheric energy; solar wind-magnetosphere interactions;
D O I
10.1023/A:1025519622160
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Three ways of the energy transfer in the Earth's magnetosphere are studied. The solar wind MHD generator is an unique energy source for all magnetospheric processes. Field-aligned currents directly transport the energy and momentum of the solar wind plasma to the Earth's ionosphere. The magnetospheric lobe and plasma sheet convection generated by the solar wind is another magnetospheric energy source. Plasma sheet particles and cold ionospheric polar wind ions are accelerated by convection electric field. After energetic particle precipitation into the upper atmosphere the solar wind energy is transferred into the ionosphere and atmosphere. This way of the energy transfer can include the tail lobe magnetic field energy storage connected with the increase of the tail current during the southward IMF. After that the magnetospheric substorm occurs. The model calculations of the magnetospheric energy give possibility to determine the ground state of the magnetosphere, and to calculate relative contributions of the tail current, ring current and field-aligned currents to the magnetospheric energy. The magnetospheric substorms and storms manifest that the permanent solar wind energy transfer ways are not enough for the covering of the solar wind energy input into the magnetosphere. Nonlinear explosive processes are necessary for the energy transmission into the ionosphere and atmosphere. For understanding a relation between substorm and storm it is necessary to take into account that they are the concurrent energy transferring ways.
引用
收藏
页码:141 / 148
页数:8
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