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Magnetic reconnection structures in the boundary layer of an interplanetary magnetic cloud
引用本文:WEI Fengsi,LIU Rui,FENG Xueshang,ZHONG Dingkun & YANG FangKey Laboratory for Space Weather,Chinese Academy of Sciences,Beijing 100080,China. Magnetic reconnection structures in the boundary layer of an interplanetary magnetic cloud[J]. 中国科学E辑(英文版), 2004, 47(1): 6-14. DOI: 10.1360/02ye0241
作者姓名:WEI Fengsi  LIU Rui  FENG Xueshang  ZHONG Dingkun & YANG FangKey Laboratory for Space Weather  Chinese Academy of Sciences  Beijing 100080  China
作者单位:WEI Fengsi,LIU Rui,FENG Xueshang,ZHONG Dingkun & YANG FangKey Laboratory for Space Weather,Chinese Academy of Sciences,Beijing 100080,China
摘    要:An interplanetary magnetic diffusion region was detected by WIND during 0735-0850 UT on May 15, 1997 when the front boundary layer of a magnetic cloud passed through the spacecraft about 190 earth radii upstream of the earth. The main signals of magnetic reconnection processes are: (i) Flow reversal was detected at about 0810 UT. The counter-streaming flows have the speeds of about 65 and 41 km/s, respectively, with an angle of about 140 degree between them. (ii) Hall magnetic field was detected. The Hall fields -By and +By, perpendicular to the X-Z plane, with their magnitude up to -7.0 nT, are superposed upon a guide field about 12 nT. (iii) Alfvenic fluctuations are obviously intensified inside the reconnection region; at the front boundary of the reconnection region, a slow-mode-like discontinuity was detected.(iv) Ions are heated intensively inside the reconnection region, with their temperature three times higher than that ahead of the boundary layer; electrons are also heated, with a little enhan


Magnetic reconnection structures in the boundary layer of an interplanetary magnetic cloud
Wei Fengsi,Liu Rui,Feng Xueshang,Zhong Dingkun,Yang Fang. Magnetic reconnection structures in the boundary layer of an interplanetary magnetic cloud[J]. Science in China(Technological Sciences), 2004, 47(1): 6-14. DOI: 10.1360/02ye0241
Authors:Wei Fengsi  Liu Rui  Feng Xueshang  Zhong Dingkun  Yang Fang
Affiliation:Key Laboratory for Space Weather, Chinese Academy of Sciences, Beijing 100080, China
Abstract:An interplanetary magnetic diffusion region was detected by WIND during 0735-0850 UT on May 15, 1997 when the front boundary layer of a magnetic cloud passed through the spacecraft about 190 earth radii upstream of the earth. The main signals of magnetic reconnection processes are: (i) Flow reversal was detected at about 0810 UT. The counter-streaming flows have the speeds of about 65 and 41 km/s, respectively, with an angle of about 140 degree between them. (ii) Hall magnetic field was detected. The Hall fields -By and +By, perpendicular to the X-Z plane, with their magnitude up to -7.0 nT, are superposed upon a guide field about 12 nT. (iii) Alfvenic fluctuations are obviously intensified inside the reconnection region; at the front boundary of the reconnection region, a slow-mode-like discontinuity was detected.(iv) Ions are heated intensively inside the reconnection region, with their temperature three times higher than that ahead of the boundary layer; electrons are also heated, with a little enhancement in their temperature. The above observations indicate that magnetic reconnection processes could take place in interplanetary space.
Keywords:solar wind   interplanetary magnetic clouds   magnetic reconnection.
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