Observation of a Sharp Negative Dipolarization Front in the Reconnection Outflow Region
ZHOU Meng1,2,4**, HUANG Shi-Yong3, DENG Xiao-Hua1,3, PANG Ye1,4
1Institute of Space Science and Technology, Nanchang University, Nanchang 330031 2Sate Key Laboratory of Space Weather, Chinese Academy of Sciences, Beijing 100190 3School of Electronics and Information, Wuhan University, Wuhan 430072 4Institute of Astronomy, Nanchang University, Nanchang 330031
Observation of a Sharp Negative Dipolarization Front in the Reconnection Outflow Region
ZHOU Meng1,2,4**, HUANG Shi-Yong3, DENG Xiao-Hua1,3, PANG Ye1,4
1Institute of Space Science and Technology, Nanchang University, Nanchang 330031 2Sate Key Laboratory of Space Weather, Chinese Academy of Sciences, Beijing 100190 3School of Electronics and Information, Wuhan University, Wuhan 430072 4Institute of Astronomy, Nanchang University, Nanchang 330031
摘要A sharp dipolarization front (DF) has recently been detected in the Earth's magnetotail and is associated with complex kinetic effects. We present one event where a tailward propagating negative DF (with Bz decreasing sharply to negative value) was observed near a reconnection region. The thickness of the negative DF is comparable with the local ion gyro-radius/inertial length. There is a strong field-aligned current at the front. Electromagnetic whistler wave enhancements are observed around the front, associated with counter-streaming electron beams. We further compare the features of the observed negative DF with the recent kinetic simulation results, as well as the Earthward propagating DFs observed by the THEMIS spacecraft.
Abstract:A sharp dipolarization front (DF) has recently been detected in the Earth's magnetotail and is associated with complex kinetic effects. We present one event where a tailward propagating negative DF (with Bz decreasing sharply to negative value) was observed near a reconnection region. The thickness of the negative DF is comparable with the local ion gyro-radius/inertial length. There is a strong field-aligned current at the front. Electromagnetic whistler wave enhancements are observed around the front, associated with counter-streaming electron beams. We further compare the features of the observed negative DF with the recent kinetic simulation results, as well as the Earthward propagating DFs observed by the THEMIS spacecraft.
ZHOU Meng;**;HUANG Shi-Yong;DENG Xiao-Hua;PANG Ye;
. Observation of a Sharp Negative Dipolarization Front in the Reconnection Outflow Region[J]. 中国物理快报, 2011, 28(10): 109402-109402.
ZHOU Meng, **, HUANG Shi-Yong, DENG Xiao-Hua, PANG Ye,
. Observation of a Sharp Negative Dipolarization Front in the Reconnection Outflow Region. Chin. Phys. Lett., 2011, 28(10): 109402-109402.
[1] Lui A T Y 1996 J. Geophys. Res. 101 13067
[2] Shiokawa K, Baumjohann W and Haerendel G 1997 Geophys. Res. Lett. 24 1179
[3] Ohtani S, Shay M A and Mukai T 2004 J. Geophys. Res. 109 A03210
[4] Sitnov M I, Swisdak M and Divin A V 2009 J. Geophys. Res. 114 A04202
[5] Runov A et al 2009 Geophys. Res. Lett. 36 L14106
[6] Zhou M et al 2009 Geophys. Res. Lett. 36 L20107
[7] Deng X et al 2010 J. Geophys. Res. 115 A09225
[8] Balogh A et al 1997 Sp. Sci. Rev. 79 65
[9] Rème H et al 2001 Ann. Geophys. 19 1303
[10] Gustafson G et al 1997 Space Sc. Rev. 79 137
[11] Johnstone A D et al 1997 Space Sci. Rev. 79 351
[12] Wilken B et al 2001 Ann. Geophys. 10 1355
[13] Cornilleau-Wehrlin N et al 2003 Ann Geophys. 21 437
[14] Paschmann G, and Daly P W 1998 Analysis Methods for Multi-Spacecraft Data ISSI (Paris: ESA)
[15] Runov A et al 2008 J. Geophys. Res. 113 A07S27
[16] Chen C X and Wolf R A 1993 J. Geophys. Res. 98 21409
[17] Sergeev V A et al 1996 J. Geophys. Res. 101 10 817
[18] Zhou M et al 2011 J. Geophys. Res. 116 A06222