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首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Pattern of Latitudinal Distribution of Ionospheric Irregularities in the African Region and the Effect of March 2015 St. Patrick's Day Storm
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Pattern of Latitudinal Distribution of Ionospheric Irregularities in the African Region and the Effect of March 2015 St. Patrick's Day Storm

机译:非洲地区电离层违规行为的纬度分布与2015年3月效果

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This paper investigates the latitudinal distribution of quiet and storm time irregularities over the African ionosphere in the month of March 2015. The average rate of change in total electron content (TEC) index (ROTI_(ave)) calculated from Global Positioning System data is used as a proxy for the irregularities. The result during the quiet condition shows that irregularities are mostly observed between 19:00 and 00:00 LT regardless of the hemisphere. Its appearance in the Southern Hemisphere is earlier, though with less severity mainly around the equatorward edge of the equatorial anomaly peak. The peak of its development occurred at 21:00 LT, as it is observed in all the latitudes except those outside the equatorial region. The strength is found to be most severe at ~12° magnetic latitude (up to 1.10 TECU/min.) in the south. Beyond ~18° magnetic latitude, it is rarely noticed in the south. However, it is not observed around this latitude in the north, indicating a major hemispheric asymmetry in terms of the latitudinal boundary between the Northern and Southern Hemispheres. Furthermore, its disappearance is found to be most rapid around the poleward verge of the equatorial anomaly region particularly in the Southern Hemisphere. In contrast to quiet time observations, irregularities were absent in all latitudes during the storm days considered. This can be attributed to the local time of the storm's onset and the possible imposition of westward electric fields in the dusk period.
机译:本文调查了2015年3月在非洲电离层上安静和雨天时间违规行为的纬度分布。使用从全球定位系统数据计算的总电子含量(TEC)指数(ROTI_(AVE))的平均变化率作为违规行为的代理。在安静条件下的结果表明,无论半球如何,在19:00至00:00之间大多观察到不规则性。它在南半球的外观早期,但仍有较小的严重程度,主要是赤道异常峰的赤边缘。其开发的峰值发生在21:00,除了除赤道区域之外的所有纬度之外的所有纬度中观察到。在南方的〜12°磁纬度(高达1.10 tecu / min)中,发现强度最严重。超过〜18°磁纬度,南方很少注意到。然而,在北方的这种纬度周围没有观察到,表明北部和南半球之间的纬度边界方面的主要半球不对称。此外,它的消失是围绕赤道异常区域的极快边缘最迅速的最迅速。与安静的时间观察相比,在考虑的暴风雨日内,所有纬度都不存在违规行为。这可以归因于风暴发病的当地时间以及黄昏时期中的西方电场可能施加。

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