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反向赤道电集流与极盖驱动势
引用本文:沈长寿,资民筠.反向赤道电集流与极盖驱动势[J].北京大学学报(自然科学版),1995,31(5):609-613.
作者姓名:沈长寿  资民筠
作者单位:北京大学地球物理系,中国艺术研究院
摘    要:一般认为反向赤道电集流是一种“非”常态现象,其起因可能是潮汐风波模的特殊组合,或赤道上空局地垂直风切或重力波的作用结果,本文表明,在中性大气和水平风经验模式给出的磁静日中低纬平均条件下,CEJ应“正常”地出现。磁层-电离层耦合产生的极盖区边界驱动势(或对流电场)同昌CEJ消失的可能机制。

关 键 词:赤道电集流  磁层  耦合  极盖驱动势  电离层

The Equatorial Counter Electrojet and the Electrostatic Potential Across the Polar Cap
SHEN Changshou.The Equatorial Counter Electrojet and the Electrostatic Potential Across the Polar Cap[J].Acta Scientiarum Naturalium Universitatis Pekinensis,1995,31(5):609-613.
Authors:SHEN Changshou
Abstract:Up to now , the equatorial counter electrojet (CEDis considered as an unusual phenomenon , which is caused by a special combination of tidal modes,or by a local vertical wind shear or a gravity-wave at ionospheric height above the e-quator.This paper shows, however,under an average state given by the empirical models of IRI-90, MSIS-90 and HwM-90 for middle-and low-latitude ionospheres on geomagnetically quiet days, the CEJ occurs frequently. On the other hand , the CEJ disappears under the effect of the electrostatic potential across the polar cap(the dawn-dusk electic field) driven by the magnetosphere-ionosphere coupling.
Keywords:equatorial electrojet  magnetosphere-ionosphere coupling  electrostatic potential across the polar cap
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