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Substorm observations in the early morning sector with Equator-S and Geotail

Authors :
R. Nakamura
G. Haerendel
W. Baumjohann
A. Vaivads
H. Kucharek
B. Klecker
E. Georgescu
J. Birn
L. M. Kistler
T. Mukai
S. Kokubun
P. Eglitis
L. A. Frank
J. B. Sigwarth
Max-Planck-Institut für Extraterrestrische Physik (MPE)
Institute of Space Science [Bucharest-Măgurele] (ISS)
Los Alamos National Laboratory (LANL)
Space Science Center [Durham]
University of New Hampshire (UNH)
Institute of Space and Astronautical Science (ISAS)
Japan Aerospace Exploration Agency [Sagamihara] (JAXA)
Solar-Terrestrial Environment Laboratory [Nagoya] (STEL)
Nagoya University
Swedish Institute of Space Physics [Kiruna] (IRF)
Finnish Meteorological Institute (FMI)
Department of Physics and Astronomy [Hanover]
Dartmouth College [Hanover]
EGU, Publication
Source :
Annales Geophysicae, Vol 17, Iss 12, Pp 1602-1610 (0000), Scopus-Elsevier, Annales Geophysicae, Annales Geophysicae, European Geosciences Union, 1999, 17 (12), pp.1602-1610, Annales Geophysicae, Vol 17, Pp 1602-1610 (1999)
Publisher :
Copernicus Publications

Abstract

Data from Equator-S and Geotail are used to study the dynamics of the plasma sheet observed during a substorm with multiple intensifications on 25 April 1998, when both spacecraft were located in the early morning sector (03–04 MLT) at a radial distance of 10–11 RE. In association with the onset of a poleward expansion of the aurora and the westward electrojet in the premidnight and midnight sector, both satellites in the morning sector observed plasma sheet thinning and changes toward a more tail-like field configuration. During the subsequent poleward expansion in a wider local time sector (20–04 MLT), on the other hand, the magnetic field configuration at both satellites changed into a more dipolar configuration and both satellites encountered again the hot plasma sheet. High-speed plasma flows with velocities of up to 600 km/s and lasting 2–5 min were observed in the plasma sheet and near its boundary during this plasma sheet expansion. These high-speed flows included significant dawn-dusk flows and had a shear structure. They may have been produced by an induced electric field at the local dipolarization region and/or by an enhanced pressure gradient associated with the injection in the midnight plasma sheet.Key words. Magnetospheric physics (magnetospheric configuration and dynamics; plasma sheet; storms and substorms)

Details

Language :
English
ISSN :
14320576 and 09927689
Volume :
17
Issue :
12
Database :
OpenAIRE
Journal :
Annales Geophysicae
Accession number :
edsair.doi.dedup.....a433ac6a2b20461231c01801fa6b3281