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首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >High‐density O~+ in Earth's outer magnetosphere and its effect on dayside magnetopause magnetic reconnection
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High‐density O~+ in Earth's outer magnetosphere and its effect on dayside magnetopause magnetic reconnection

机译:量密度高O ~ +在地球的磁气圈外及其影响的光面磁层磁场重新连接

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摘要

The warm plasma cloak is a source of magnetospheric plasma that contain significant O~+. When the O~+ density in the magnetosphere near the magnetopause is >0.2 cm~(‐3) and the H+ density is20% due to mass‐loading only about 2% to 4% of the time. However, during geomagnetic storms, O~+ dominates the mass density of the warm plasma cloak and these mass densities are very high. Therefore, a separate study is conducted to determine the effect of the warm plasma cloak on magnetopause reconnection during geomagnetically disturbed times. This study shows that the warm plasma cloak reduces the reconnection rate significantly about 25% of the time during disturbed conditions.
机译:温暖的等离子体斗篷的来源包含重要的磁性层的等离子体O ~ +。在磁层> 0.2厘米~(3)应承担的H +密度是 20%加载只有约2%至4%的时间。O ~ +主宰着温暖的质量密度等离子体斗篷,这些质量密度非常高。因此,一个单独的研究进行确定温暖的等离子体斗篷的效果磁重联过程中眼睛干扰。等离子体斗篷降低了重联率大约25%的时间干扰的条件。

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