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Conjugacy of rapid motions and small-scale deformations of discrete auroras by all-sky TV observations

机译:全天空电视观测的快速运动和离散极光的小尺度变形的共轭

摘要

Simultaneous observations of discrete auroras were made on 26 September 1984 by means of all-sky TV cameras at a geomagnetically conjugate pair of sites : Syowa Station in Antarctica and Husafell in Iceland. A comparison of the data obtained at the two places gives the following characteristics regarding the conjugacy of discrete auroras under a geomagnetically weakly disturbed condition (ΔH=-50nT) : Before the onset of a small substorm conjugate faint discrete auroras were identified in both conjugate areas despite a small displacement (0.5°) in invariant latitude (the southern aurora is 0.5° higher than the northern one). A striking dissimilarity of the conjugate auroras is noted in small-scale structures within the auroras. That is, the northern discrete aurora was rather homogeneous, whereas the southern one was a rayed aurora. During the substorm the east-west movement and/or extension of discrete auroras was quite conjugate and simultaneous. However, the vortexlike structures such as folds on the discrete auroras were not always simultaneously observed at the both places. Even if they appeared simultaneously, their sizes seemed to be different between the conjugate regions. These results would suggest that the large-scale structures and their movements are mainly controlled by some conditions in the magnetosphere, perhaps near the equatorial region, but the small-scale structures such as vortices are greatly due to local acceleration processes between the magnetosphere and the ionosphere.
机译:1984年9月26日,通过全天候电视摄像机在地磁共轭对站点(南极洲的Syowa站和冰岛的Husafell)同时观测了离散的极光。在两个地方获得的数据的比较给出了关于在地磁弱扰动条件下(ΔH= -50nT)的离散极光的共轭性的以下特征:在小亚暴爆发之前,在两个共轭区域都识别出了微弱的离散极光。尽管不变纬度的位移很小(0.5°)(南部的极光比北部的高0.5°)。在极光内部的小规模结构中发现了共轭极光的惊人差异。也就是说,北部的离散极光是相当均匀的,而南部的是射线极光。在亚暴期间,离散的极光的东西向运动和/或延伸是共轭的和同时的。但是,并非总是在两个地方同时观察到涡状结构,例如离散极光上的褶皱。即使它们同时出现,它们的大小似乎在共轭区域之间也不同。这些结果表明,大型结构及其运动主要受磁层中某些条件的控制,也许是在赤道区域附近,但是诸如涡旋之类的小型结构很大程度上是由于磁层与磁层之间的局部加速过程所致。电离层。

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