TEMPORAL AND SPATIAL VARIATIONS OF PLASMA AND NEUTRAL VELOCITIES DURING SUBSTORM PERIODS

LIU Ding-Wei, WANG Hui, HUANG Tao, CAO Xue, ZHANG Ke-Deng
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Abstract

This study statistically investigates the temporal and spatial variations of plasma convection velocity (Vy) and thermospheric zonal wind velocity (Uy) in the range of –4 hour (h) and +2 h MLT relative to substorm onsets (MLT onset) with both CHAMP and DMSP (F13, F15) satellites observations from 2001 to 2005. It shows that Vy increase significantly in all MLT sectors and the latitudes of the peak values move equatorward in 1.5 h after substorm onsets. In the subsequent 1.5 h Vy decrease in intensity and the peaks retreat poleward, which shows that the onsets of substorm can enhance the plasma convection velocity dramatically. The relative increase of Vy is largest from –2 h to MLT onset, which indicates that the substorm mainly affects the thermosphere in the westward 0∼2 h MLT sector. Uy increases steadily in 3 hours after substorm onsets, with a 1.5 h delay relative to Vy in response to the substorm onsets.

亚暴期间等离子体和中性速度的时空变化
利用CHAMP卫星和DMSP卫星(F13、F15)对2001 ~ 2005年-4 h和+2 h MLT范围内的等离子体对流速度(Vy)和热层纬向风速(y)相对于亚暴发生(MLT)的时空变化进行了统计研究。结果表明,在次暴发生后1.5 h,各MLT扇区的Vy显著增加,峰值纬度向赤道方向移动。在随后的1.5 h内,辐射强度减弱,峰值向极地方向后退,表明亚暴的发生可以显著提高等离子体对流速度。从0 ~ 2 h到MLT开始,Vy的相对增加最大,说明次暴主要影响MLT西侧0 ~ 2 h扇区的热层。在次暴发生后的3小时内,y值稳步上升,相对于y值有1.5 h的延迟。
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