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首页> 外文期刊>Annales Geophysicae >Afternoon mid-latitude current system and low-latitude geomagnetic field asymmetry during geomagnetic storms
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Afternoon mid-latitude current system and low-latitude geomagnetic field asymmetry during geomagnetic storms

机译:下午中纬度洋流系统和地磁暴期间的低纬度地磁场不对称

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For four geomagnetic storms of middleintensity the relationship between the low-latitude magnetic field asymmetryusing ASY indices and the intensity of the auroral eastward and westwardelectrojet was considered. It was asked whether there exists a connectionbetween ASY and the eastward electrojet. To answer this question equivalentcurrent systems were estimated in mid-latitudes. It was found that theobservations obviously show no correlative relationship between the low-latitudemagnetic-field asymmetry and the eastward electrojet, whereas one exists betweenASY and the westward electrojet. To explain the generally accepted commonthree-dimensional current system between the partial ring current and theeastward electrojet, a condensor model of the three-dimensional current systemwas developed. It could be shown that the short periodic variations of thepartial ring current are shielded by the condensor and cannot influence theeastward-electrojet current.
机译:对于四次中等强度的地磁风暴,考虑了使用ASY指数的低纬度磁场不对称性与极光向东和向西电喷强度之间的关系。有人问ASY和东电喷之间是否存在联系。为了回答这个问题,在中纬度地区估计了等效电流系统。研究发现,低纬度磁场的不对称性与东向电喷之间显然没有相关关系,而在ASY和西向电喷之间存在相关关系。为了解释部分环电流和向东电喷之间公认的通用三维电流系统,建立了三维电流系统的冷凝器模型。可以证明,部分环电流的短暂周期性变化被冷凝器屏蔽,并且不会影响向东的电喷流。

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