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首页> 外文期刊>Annales Geophysicae >Interhemispheric observations of the ionospheric signature of tail reconnection during IMF-northward non-substorm intervals
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Interhemispheric observations of the ionospheric signature of tail reconnection during IMF-northward non-substorm intervals

机译:IMF-北非亚暴期间电离层尾部重新连接的电离层特征的半球观测

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This paper presents the first interhemispheric radar observations interpreted as the ionospheric response to tail reconnection during IMF-northward non-substorm intervals. SuperDARN measurements of plasma convection in the nightside ionospheres of both hemispheres, taken on 21-22 February and 26-27 April 2000, show bursts of flow in the midnight sector which are understood to be characteristic of such phenomena. Upstream interplanetary magnetic field data confirm that the field orientation at the dayside mag-aetopause was northwards, but with a significant IMF B_y component (negative during the first interval, positive during the second), for many hours prior to the bursts being observed. During the B_y-negative interval the bursts were directed westwards in the Northern Hemisphere and eastwards in the Southern Hemisphere; during the By-positive interval their directions were reversed. These two asymmetries between the different orientations of IMF B_y and between the two hemispheres are key to our understanding of the magne-tospheric phenomenon responsible for generating the bursts. They provide further evidence in support of the idea that the bursts are a result of reconnection in an asymmetric tail un-der the prolonged influence of IMF B_y. Concurrent data from ground magnetometers and geosynchronous satellites confirm that the bursts have no associated substorm charac-teristics, consistent with previous studies.
机译:本文介绍了首个半球间雷达观测结果,解释为电离层对IMF-北向非亚风暴间隔期间尾部重新连接的响应。 SuperDARN在2000年2月21-22日和4月26-27日对两个半球的夜间电离层中的对流进行了对流测量,结果表明午夜时分爆发是这种现象的特征。上游行星际磁场数据证实,在观测到爆发之前的许多小时里,日间岩浆绝经的磁场方向是向北的,但具有显着的IMF B_y分量(第一个间隔为负,第二个间隔为正)。在B_y负间隔期间,突发在北半球向西定向,在南半球向东定向;在“正”间隔期间,其方向相反。 IMF B_y的不同方向之间以及两个半球之间的这两个不对称性是我们理解负责产生爆发的磁-球现象的关键。他们提供了进一步的证据来支持这种观点,即在IMF B_y的长期影响下,突发是不对称尾部重新连接的结果。来自地面磁力计和地球同步卫星的并发数据证实,这些爆发没有相关的亚暴特征,这与以前的研究一致。

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