Statistical study of magnetotail flux ropes near the lunar orbit
Statistical study of magnetotail flux ropes near the lunar orbit作者机构:Shandong Provincial Key Laboratory of Optical Astronomy and Solar-Terrestrial Environment School of Space Science and PhysicsShandong University School of Physics Peking University School of Earth and Space Science Peking University
出 版 物:《Science China(Technological Sciences)》 (中国科学(技术科学英文版))
年 卷 期:2016年第59卷第10期
页 面:1591-1596页
核心收录:
学科分类:070802[理学-空间物理学] 07[理学] 0708[理学-地球物理学]
基 金:supported by the Scientific Research Foundation of Shandong Province Outstanding Young Scientist Award(Grant Nos.2013BSE27132&BS2013HZ001) the Research Fund for the Doctoral Program of Higher Education of China(Grant No.20130131120073) the National Natural Science Foundation of China(Grant Nos.41304129,41322031&41574157)
主 题:magnetotail flux rope TCR dawn-dusk asymmetry reconnection site
摘 要:Flux-rope/TCR events near the magnetotail lunar orbit (-67RE 〈 GSM X* 〈 -39RE) were studied using magnetic-field and plasma data measured by THEMIS B and C between January 2011 and March 2012. The aberrant coordinate GSM*, where the X* axis is rotated 4° relative to GSM-X, was used to count the occurrence rate. The number ratio of earthward to tailward events was about 3:5. Moreover, the event occurrence rate distribution showed a clear dawn-dusk asymmetry distribution, with dusk-side events accounting for 57.98%. A superposed epoch analysis of the flux-rope events showed that earthward events had a shorter duration in the leading than in the trailing part. Earthward events also displayed a lower temperature and a lower flow speed than tailward events. We studied the relationship between the event occurrence rate and geomagnetic activity level even further. The occurrence rate of tailward flux-rope/TCR events increases with increasing AE-index, whereas earthward events occur mainly in the relatively quiet period of geomagnetic activity (AE - 100-300 nT). Flux-rope/TCR events identi- fied within a 10 mm time frame were treated as belonging to a single reconnection event. By comparing the occurrence rates of earthward and tailward events along X*, we estimated the most likely location of the near-Earth reconnection site as X* = -36RE.