日冕洞,146兆赫辐射和地磁风暴

Zhao Xue-pu, Liu Xu-zhao
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引用次数: 0

摘要

我们对日冕洞和地磁风暴之间关系的分析支持了所谓的m区是面积较大的日冕洞的观点。对于两个典型的日冕洞,发现它们的赤道延伸为25-50°。地磁风暴的发生与日冕洞中央子午线通过之间的时间差与日冕洞的面积呈负相关。研究了密云站164mhz扇形波束干涉仪在日冕洞发生时的记录。总的来说,这些记录显示出有规律的变化,这意味着日冕洞的辐射减少,而且日冕洞跟随太阳的旋转。“中心带通量”的“叠加图分析”结果更清楚地证明了这些影响。探讨了利用射电资料和太阳黑子资料确定日冕洞CMP的可能性,并尝试利用周期性地磁暴资料估算高速太阳流的速度和日冕洞的大小。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Coronal holes, 146 MHz emissions and geomagnetic storms

Our analysis of the relationship between coronal holes and geomagnetic storms lends support to the idea that the so-called M-regions are coronal holes with large areas. For two typical coronal holes examined, their equatorial extensions are found to be 25–50°. The time lag between the onset of the geomagnetic storm and the central meridian passage of the coronal hole is inversely correlated with the area of the latter.

Records of the 164 MHz fan beam interferometer of our Miyun Station at the times of coronal holes are examined. in general, these records show a regular variation, implying a diminished emission from the coronal holes and that the holes follow the solar rotation. Results from a “superposed diagram analysis” of the “central strip flux” demonstrate these effects even more clearly.

The possibility of using radio and sunspot data to determine the CMP of coronal holes is investigated and an attempt is made to evaluate the speed of the high-velocity solar stream and the size of the coronal hole from data on recurrent geomagnetic storms.

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