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首页> 外文期刊>Plasma physics reports >Effect of the global topology of the interplanetary magnetic field on the properties of impulsive acceleration processes in distant regions of the earth's magnetospheric tail
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Effect of the global topology of the interplanetary magnetic field on the properties of impulsive acceleration processes in distant regions of the earth's magnetospheric tail

机译:行星际磁场的整体拓扑结构对地球磁层尾部遥远区域中脉冲加速过程特性的影响

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The paper is devoted to a statistical study of high-speed ion beams (beamlets) observed by the Interball-1 and Interball-2 satellites in the boundary region of the plasma sheet of the geomagnetic tail and in the high-latitude auroral regions of the Earth's magnetosphere. Beamlets result from nonlinear acceleration processes occurring in the current sheet in the distant regions of the geomagnetic tail. They propagate toward the Earth along the magnetic field lines and are detected in the boundary region of the plasma sheet and near the high-latitude boundary of the plasma sheet in the auroral region in the form of short (with a duration of 1-2 min) bursts of high-energy (with energies of about several tens of keV) ions. The sizes of the latitudinal zones where the beamlets are localized in the tail and in the auroral region are determined using the epoch superposition method. The relationship between the frequency of beamlet generation in the boundary region of the plasma sheet and the prehistory of the direction of the interplanetary magnetic field (the magnitude of a clock angle) is investigated. It was established that this direction exerts a global effect on the beamlet generation frequency; moreover, it was found that the beamlet generation frequency in the midnight local time sector of the tail and at the flanks depends differently on the direction of the interplanetary magnetic field. In the midnight sector, the beamlets are observed at almost all directions of the interplanetary field, whereas the frequency of their generation at the flanks is maximal only when the interplanetary magnetic field has a large y component. (c) 2005 Pleiades Publishing, Inc.
机译:这篇论文致力于对Interball-1和Interball-2卫星在地磁尾部等离子体层边界区域和高纬度极光区域中观察到的高速离子束(子束)的统计研究。地球的磁层。子束是由地磁尾部遥远区域中当前工作表中发生的非线性加速过程导致的。它们沿着磁场线向地球传播,并在短波的形式(持续时间为1-2分钟)中在等离子片的边界区域和极光区域中等离子片的高纬度边界附近被检测到。 )爆发高能离子(能量约为几十keV)。使用历元叠加法确定子束位于尾部和极光区域中的纬度区域的大小。研究了在等离子体片的边界区域中的子束产生的频率与行星际磁场的方向的史前时间(钟角的大小)之间的关系。可以确定的是,这个方向对子束的产生频率产生了整体影响。此外,已经发现,在尾部的午夜本地时间段和在侧面的子束产生频率取决于行星际磁场的方向。在午夜部分,子束几乎在行星际磁场的所有方向上都被观测到,而只有在行星际磁场具有较大的y分量的情况下,在侧面的子束的生成频率才最大。 (c)2005年Pleiades Publishing,Inc.

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