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首页> 外文期刊>Annales Geophysicae >Dual-spacecraft reconstruction of a three-dimensional magnetic flux rope at the Earth's magnetopause
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Dual-spacecraft reconstruction of a three-dimensional magnetic flux rope at the Earth's magnetopause

机译:地球磁层顶的三维磁通绳的双飞船重建

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We present the first results of a data analysis method, developed by Sonnerupand Hasegawa (2011), for reconstructing three-dimensional (3-D),magnetohydrostatic structures from data taken as two closely spacedsatellites traverse the structures. The method is applied to a magnetic fluxtransfer event (FTE), which was encountered on 27 June 2007 by at leastthree (TH-C, TH-D, and TH-E) of the five THEMIS probes near the subsolarmagnetopause. The FTE was sandwiched between two oppositely directedreconnection jets under a southward interplanetary magnetic field condition,consistent with its generation by multiple X-line reconnection. Therecovered 3-D field indicates that a magnetic flux rope with a diameter of~ 3000 km was embedded in the magnetopause. The FTE flux ropehad a significant 3-D structure, because the 3-D field reconstructed fromthe data from TH-C and TH-D (separated by ~ 390 km) betterpredicts magnetic field variations actually measured along the TH-E paththan does the 2-D Grad–Shafranov reconstruction using the data from TH-C(which was closer to TH-E than TH-D and was at ~ 1250 km fromTH-E). Such a 3-D nature suggests that the field lines reconnected at thetwo X-lines on both sides of the flux rope are entangled in a complicatedway through their interaction with each other. The generation process of theobserved 3-D flux rope is discussed on the basis of the reconstructionresults and the pitch-angle distribution of electrons observed in and aroundthe FTE.
机译:我们介绍了Sonnerupand Hasegawa(2011)开发的数据分析方法的第一个结果,该方法用于从两个紧密间隔的卫星穿过的数据中重建三维(3-D)静磁静力结构。该方法适用于磁通量传输事件(FTE),该事件在2007年6月27日被近地下电磁绝经附近的五个THEMIS探针中的至少三个(TH-C,TH-D和TH-E)遇到。 FTE被夹在两个朝相反方向的重连射流之间,处于向南行星际磁场条件下,这与多次X线重连产生的结果一致。发现的3-D磁场表明直径为〜3000 km的磁通绳嵌入了磁层顶。 FTE磁通绳具有显着的3-D结构,因为从TH-C和TH-D的数据(相距约390 km)重建的3-D场比沿着TH-E路径实际测量的磁场变化能更好地预测2 -D Grad–Shafranov使用TH-C的数据进行重建(该数据比TH-D更接近TH-E,距TH-E约1250公里)。这种3-D性质表明,在通量绳两侧的两条X线处重新连接的场线通过它们彼此的相互作用以复杂的方式纠缠在一起。根据重建结果和在FTE内部及周围观察到的电子的俯仰角分布,讨论了观察到的3D通量绳的产生过程。

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