Timing of magnetic reconnection initiation during a global magnetospheric substorm onset

被引:99
作者
Baker, DN
Peterson, WK
Eriksson, S
Li, X
Blake, JB
Burch, JL
Daly, PW
Dunlop, MW
Korth, A
Donovan, E
Friedel, R
Fritz, TA
Frey, HU
Mende, SB
Roeder, J
Singer, HJ
机构
[1] Univ Colorado, LASP, Boulder, CO 80309 USA
[2] Aerosp Corp, El Segundo, CA 90245 USA
[3] SW Res Inst, San Antonio, TX 78284 USA
[4] Max Planck Inst, Katlenberg, Lindau, Germany
[5] Univ London Imperial Coll Sci Technol & Med, London SW7 2AZ, England
[6] Univ Calgary, Calgary, AB T2N 1N4, Canada
[7] Los Alamos Natl Lab, Los Alamos, NM 87545 USA
[8] Boston Univ, Ctr Space Phys, Boston, MA 02215 USA
[9] Univ Calif Berkeley, Space Phys Lab, Berkeley, CA 94720 USA
[10] NOAA, Space Environm Ctr, Boulder, CO 80307 USA
关键词
D O I
10.1029/2002GL015539
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
[1] We have used a unique constellation of Earth-orbiting spacecraft and ground-based measurements in order to study a relatively isolated magnetospheric substorm event on August 27, 2001. Global ultraviolet images of the northern auroral region established the substorm expansion phase onset at 0408: 19 (+/-1 min) UT. Concurrent measurements from the GOES-8, POLAR, LANL, and CLUSTER spacecraft allow us to construct a timeline which is consistent with magnetic reconnection on the closed field lines of the central plasma sheet near X-GSM similar to -18 R-E some 7 minutes prior to the near-earth and auroral region times of substorm expansion phase onset. This suggests that magnetic reconnection (i.e., the substorm neutral line) in this case formed in the mid-tail region substantially before current disruption, field dipolarization near geostationary orbit, or auroral substorm onsets occurred. Thus, the magnetic reconnection process is interpreted as the causative driver of dissipation in this well-observed case.
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收藏
页码:43 / 1
页数:4
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