The location and rate of dayside reconnection during an interval of southward interplanetary magnetic field

被引:40
|
作者
Pinnock, M
Chisham, G
Coleman, IJ
Freeman, MP
Hairston, M
Villain, JP
机构
[1] British Antarctic Survey, Nat Environm Res Council, Cambridge CB3 0ET, England
[2] Univ Texas, Ctr Space Sci, Richardson, TX 75083 USA
[3] CNRS, LPCE, F-45071 Orleans, France
关键词
magnetospheric physics; magnetopause; cusp and boundary layers; magnetosphere-ionoshere interactions; space plasma physics; magnetic reconnection;
D O I
10.5194/angeo-21-1467-2003
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Using ionospheric data from the SuperDARN radar network and a DMSP satellite we obtain a comprehensive description of the spatial and temporal pattern of dayside reconnection. During a period of southward interplanetary magnetic field (IMF), the data are used to determine the location of the ionospheric projection of the dayside magnetopause reconnection X-line. From the flow of plasma across the projected X-line, we derive the reconnection rate across 7 h of longitude and estimate it for the total length of the X-line footprint, which was found to be 10 h of longitude. Using the Tsyganenko 96 magnetic field model, the ionospheric data are mapped to the magnetopause, in order to provide an estimate of the extent of the reconnection X-line. This is found to be similar to38 R(E)in extent, spanning the whole dayside magnetopause from dawn to dusk flank. Our results are compared with previously reported encounters by the Equator-S and Geotail spacecraft with a reconnecting magnetopause, near the dawn flank, for the same period. The SuperDARN observations allow the satellite data to be set in the context of the whole magnetopause reconnection X-line. The total potential associated with dayside reconnection was similar to150 kV The reconnection signatures detected by the Equator-S satellite mapped to a region in the ionosphere showing continuous flow across the polar cap boundary, but the reconnection rate was variable and showed a clear spatial variation, with a distinct minimum at 14:00 magnetic local time which was present throughout the 30-min study period.
引用
收藏
页码:1467 / 1482
页数:16
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