首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Cluster observations near reconnection X lines in Earth's magnetotail current sheet
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Cluster observations near reconnection X lines in Earth's magnetotail current sheet

机译:地球磁尾电流表中重新连接的X线附近的聚类观测

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Magnetic reconnection is an efficient way to convert magnetic energy into particle energy. In this paper, we use Cluster thermal electron and ion measurements in the vicinity of a reconnection X line to delineate the structure of the reconnection current sheet. Multispacecraft observations made by Cluster on 18 August 2002 indicate that an X line drifted close to the spacecraft, about 3.4 R_E earthward of the position where another X line had been observed earlier. Comparison of the Hall magnetic and electric field geometry and the observed properties of energetic electron beams streaming along the separatrix between the Cluster spacecraft indicates that the second X line formed within 20 s of the observation of the first X line. Repeated flow reversals and Hall field geometry together with the presence of a magnetic island embedded in the outflow region downstream of the first X line suggest that the initial current sheet was unstable, perhaps to the tearing mode. We identify a region with a thickness of 0.72 ion inertial lengths (29 electron inertial lengths, d_e) of super-Alfvénic electron outflow (greater than the ion in-flow Alfvén speed) during the period when the spacecraft was in the vicinity of the neutral sheet. Slightly below the neutral sheet, Cluster observed asymmetric counter-streaming electrons with a loss of axisymmetry in the electron (V_(⊥1),V_(⊥2)) distribution functions over a thin boundary with a thickness of several d _e. This electron-scale transition layer was embedded in a much wider region where both the ion and electron Walén tests failed, and the electron super-Alfvénic bulk outflow jets with high-energy electron beams were detected. Those phenomena provide details of the substructure of the reconnection current sheet and suggest that the spacecraft traversed or skimmed the tailward edge of an elongated electron current layer. We also note that this event differs from a previously reported reconnection event in that strong electron temperature anisotropy (T_∥>T_⊥) is observed both in the inflow region and in the exhaust, where the anisotropy appears to be associated with the elongated electron outflow jets.
机译:磁重连接是将磁能转换为粒子能的有效方法。在本文中,我们在重连X线附近使用簇热电子和离子测量来描绘重连电流表的结构。群集在2002年8月18日进行的多宇宙飞船观测表明,一条X线向航天器附近漂移,距较早观测到另一条X线的位置大约3.4 R_E地球。比较霍尔磁场和电场的几何形状以及在簇状航天器之间沿着分离线流动的高能电子束的观察特性,表明第二X线在观察第一X线的20 s内形成。重复的流动逆转和霍尔场几何形状以及嵌入在第一条X线下游的流出区域中的磁岛的存在表明,最初的电流表不稳定,可能对撕裂模式是不稳定的。我们确定了航天器处于中性附近期间超Alfvénic电子流出(大于离子流入Alfvén速度)的厚度为0.72离子惯性长度(29电子惯性长度,d_e)的区域片。在中性薄板的正下方,Cluster观察到不对称的逆流电子,其电子分布(V_(⊥1),V_(⊥2))的轴对称性损失在厚度为d _e的薄边界上起作用。这个电子尺度的过渡层嵌入了一个更大的区域,在该区域中离子和电子Walén测试均失败了,并且检测到了具有高能电子束的电子超级Alfvénic整体流出射流。这些现象提供了重新连接电流片的子结构的细节,并表明航天器横穿或掠过了细长电子流层的尾端。我们还注意到,该事件与先前报告的重新连接事件的不同之处在于,在流入区域和排气中均观察到强烈的电子温度各向异性(T_∥>T_⊥),其中各向异性似乎与伸长的电子流出有关喷气机。

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