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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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摘要

This paper presents the first interhemispheric radar observationsinterpreted as the ionospheric response to tail reconnection duringIMF-northward non-substorm intervals. SuperDARN measurements of plasmaconvection in the nightside ionospheres of both hemispheres, taken on21–22 February and 26–27 April 2000, show bursts of flow in the midnight sectorwhich are understood to be characteristic of such phenomena. Upstreaminterplanetary magnetic field data confirm that the field orientation at thedayside magnetopause was northwards, but with a significant IMF Bycomponent (negative during the first interval, positive during the second),for many hours prior to the bursts being observed. During theBy-negative interval the bursts were directed westwards in theNorthern Hemisphere and eastwards in the Southern Hemisphere; during theBy-positive interval their directions were reversed. These twoasymmetries between the different orientations of IMF By and betweenthe two hemispheres are key to our understanding of the magnetosphericphenomenon responsible for generating the bursts. They provide furtherevidence in support of the idea that the bursts are a result of reconnectionin an asymmetric tail under the prolonged influence of IMF By.Concurrent data from ground magnetometers and geosynchronous satellitesconfirm that the bursts have no associated substorm characteristics,consistent with previous studies.>Keywords. Ionosphere (Plasma convection; Ionospheremagnetosphereinteractions) – Magnetospheric Physics(Magnetotail)
机译:本文介绍了首个半球间雷达观测结果,解释为IMF-北非亚风暴间隔期间电离层对尾部重新连接的响应。 2000年2月21日至22日和4月26日至27日对两个半球的夜间电离层的对流进行SuperDARN测量,结果表明午夜时分爆发是这种现象的特征。上行行星际磁场数据证实,在白天的磁层顶,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),在观察到爆裂之前持续了几个小时。在 B y 负间隔期间,爆发在北半球向西定向,在南半球向东定向。在 B y 阳性间隔期间,它们的方向相反。 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层现象的关键。他们提供了进一步的证据,证明了爆发是在IMF B y 的长期影响下在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> 关键词。电离层(等离子对流;电离层-磁层相互作用)–磁层物理(磁尾)

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