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Distribution of X-type magnetic neutral lines in the magnetotail with Geotail observations

机译:利用Geotail观测法在磁尾中X型磁中性线的分布

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We obtained the distribution of the X-type magnetic neutral lines in the magnetotail from X_(GSM) = 0 to -210 R_E with Geotail observations. For the detection of the neutral lines, we adopted simultaneous reversals of magnetic field from north to south (south to north) and ion bulk velocity from earthward to tailward (tailward to earthward). In the near-tail region (0 greater than or equal X_(GSM)>-30 R_E), the occurrence rate of the reversal events had a peak at Y_(GSM) approximately equals +9 R_E and was characterized by a very asymmetric form in the YGSM direction. The region of the reversal events appeared to expand in the Y_(GSM) direction up to a 50 R_E width at X_(GSM) approximately equals -50 R_E. This width was maintained in the region further downtail (X_(GSM)<-50 R_E). The occurrence rate integrated in the Y_(GSM) direction was found to have a maximum at X_(GSM) approximately equals -60 R_E.
机译:我们通过Geotail观测获得了从X_(GSM)= 0到-210 R_E的磁尾中X型磁中性线的分布。为了检测中性线,我们同时采用了从北到南(南到北)的反向磁场和从大地到尾(从尾到大)的离子体积速度。在近尾区域(0大于或等于X_(GSM)>-30 R_E),反转事件的发生率在Y_(GSM)处具有约+9 R_E的峰值,并具有非常不对称的形式在YGSM方向上。反向事件的区域似乎在Y_(GSM)方向上扩展到X_(GSM)处的50 R_E宽度,大约等于-50 R_E。该宽度被保持在进一步降低的区域(X_(GSM)<-50 R_E)。发现在Y_(GSM)方向上积分的出现率在X_(GSM)处具有最大值,大约等于-60 R_E。

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