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The substructure of a flux transfer event observed by the MMS spacecraft

机译:MMS航天器观测到的通量传输事件的子结构

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摘要

On 15 August 2015, MMS (Magnetospheric Multiscale mission), skimming the dusk magnetopause, detected an isolated region of an increased magnetic strength and bipolar B-n, indicating a flux transfer event (FTE). The four spacecraft in a tetrahedron allowed for investigations of the shape and motion of the FTE. In particular, high-resolution particle data facilitated our exploration of FTE substructures and their magnetic connectivity inside and surrounding the FTE. Combined field and plasma observations suggest that the core fields are open, magnetically connected to the northern magnetosphere from which high-energy particles leak; ion "D" distributions characterize the axis of flux ropes that carry old-opened field lines; counterstreaming electrons superposed by parallel-heated components populate the periphery surrounding the FTE; and the interface between the core and draped regions contains a separatrix of newly opened magnetic field lines that emanate from the X line above the FTE.
机译:2015年8月15日,MMS(磁层多尺度飞行任务)掠过黄昏的磁层顶,检测到一个孤立的区域,该区域的磁场强度和双极B-n值增加,表明发生了磁通转移事件(FTE)。四面体中的四个航天器可以研究FTE的形状和运动。特别是,高分辨率的粒子数据有助于我们探索FTE子结构及其在FTE内部和周围的磁连通性。结合磁场和等离子体的观察结果表明,核心磁场是开放的,与北部的磁层电磁连接,高能粒子从北部的磁层漏出。离子“ D”的分布表征了载有过时打开的磁力线的助焊绳的轴线;由平行加热的成分叠加的逆流电子在FTE周围形成了外围。核心区域和悬垂区域之间的界面包含一个分离线,该分离线是从FTE上方的X线发出的新打开的磁场线。

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