Physics
Scientific paper
Mar 1987
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1987jgr....92.2365s&link_type=abstract
Journal of Geophysical Research (ISSN 0148-0227), vol. 92, March 1, 1987, p. 2365-2376. Research supported by the Max-Planck-Ges
Physics
22
Auroral Zones, Earth Magnetosphere, Geomagnetic Tail, Interplanetary Magnetic Fields, Solar Wind, Auroral Electrojets, Electron Precipitation, Energetic Particles, Geos Satellites (Esa), International Sun Earth Explorers, Plasma Layers
Scientific paper
A set of coordinated measurements obtained on March 4, 1979 in the solar wind, in the magnetotail, at geostationary orbit, in the auroral ionosphere, and on the ground has been used to conduct a detailed study of the overall magnetospheric response to a southward turning of the IMF. The change of the IMF direction is found to be associated with a delay of less than about 5 min for increasing eastward and westward electrojets, and precedes by about 10 min the beginning of a taillike deformation of the B field geometry at geostationary orbit near midnight. After the IMF reversal and before the main substorm onset, the general motion of the westward electrojet is southward. At 6.6 R(E) in the nightside, the equatorially trapped high-energy particles adiabatically respond to the local change of the B field by moving earthward. Short-lived substorms occur soon after the IMF reversal.
Dandouras Jannis
Reme Henri
Saint-Marc A.
Sauvaud Jean-Andre
Treilhou J. P.
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