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首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Statistical study of effect of solar wind dynamic pressure enhancements on dawn-to-dusk ring current asymmetry
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Statistical study of effect of solar wind dynamic pressure enhancements on dawn-to-dusk ring current asymmetry

机译:统计研究太阳风动态的影响在黎明到黄昏环压力增强电流不对称

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In this paper, we statistically investigate the effect of solar wind dynamic pressure enhancements on the dawn-to-dusk ring current asymmetry by examining disturbances of the ASY-H index and low-latitude and midlatitude ground asymmetric perturbations in the north-south (H) component of the geomagnetic field during 186 events occurring from 1 June 2003 to 30 September 2004. Both storm time and nonstorm time events are included. It is found that a pressure enhancement further intensifies the ring current asymmetry provided that the ring current is already asymmetric at the time of the onset of the pressure enhancement. This effect strongly depends on the IMF Bz conditions prior to the pressure enhancement. Generally, for negative IMF Bz, pressure enhancements further increase the ring current asymmetry. This effect also depends on the strength of the pressure enhancement. Under the same IMF Bz conditions, the stronger the pressure enhancement is, the stronger the intensification of the asymmetric ring current is. The IMF Bz conditions during a pressure enhancement play a similar role to that of the IMF Bz preconditioning. The results further show that midlatitude H perturbations around the local noon or midnight region as well as the ASY-H index often include significant contribution from field-aligned currents, e.g., the region 1 (R1) or region 2 (R2) currents or the substorm current wedge.
机译:在本文中,我们统计调查太阳风动压力的影响增强在黎明到黄昏环电流不对称通过检查ASY-H的干扰指数和低纬度和观测的地面在南北不对称扰动(H)在186年组成部分地磁场从2003年6月1日到9月30日发生的事件2004. 是包括在内。增强进一步加剧了环电流不对称环电流提供已经不对称发病的时候增强的压力。取决于前国际货币基金组织商务条件增强的压力。进一步增加,压力增强环电流不对称。在压力的强度增强。在IMF Bz相同条件下,越强增强的压力越强强化的不对称环电流是多少。增强扮演类似的角色国际货币基金组织的Bz预处理。这中间纬度H扰动在当地中午和午夜地区以及ASY-H从指数通常包括重大贡献field-aligned电流,例如,区域1 (R1)或地区2 (R2)电流或电流亚暴楔。

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