HR: 14:55h
AN: SA42B-06
TI: The Response of the Magnetosphere to an Interplanetary Shock: Ground-based Observations
of the Sudden Impulse on September 24, 1998
AU: Zesta, E
EM:
AF: Institute of Geophysics and Planetary Physics,
University of California Los Angeles, CA 90095-1567 United States
AU: * Chi, P J
EM: pchi@igpp.ucla.edu
AF: Institute of Geophysics and Planetary Physics,
University of California Los Angeles, CA 90095-1567 United States
AU: Russell, C T
EM:
AF: Institute of Geophysics and Planetary Physics,
University of California Los Angeles, CA 90095-1567 United States
AU: Raeder, J
EM:
AF: Institute of Geophysics and Planetary Physics,
University of California Los Angeles, CA 90095-1567 United States
AU: Le, G
EM:
AF: Institute of Geophysics and Planetary Physics,
University of California Los Angeles, CA 90095-1567 United States
AU: Yumoto, K
EM:
AF: Department of Earth and Planetary Sciences,
Kyushu University 33,
6-10-1 Hakozaki Fukuoka, 812-8581 Japan
AU: Kawano, H
EM:
AF: Department of Earth and Planetary Sciences,
Kyushu University 33,
6-10-1 Hakozaki Fukuoka, 812-8581 Japan
AU: Kitamura, K
EM:
AF: Department of Earth and Planetary Sciences,
Kyushu University 33,
6-10-1 Hakozaki Fukuoka, 812-8581 Japan
AU: Angelopoulos, V
EM:
AF: Space Sciences Laboratory,
University of California Berkeley, CA 94720 United States
AU: Moldwin, M
EM:
AF: Florida Institute of Technology,
Physics and Space Sciences,
150 W. University Blvd Melbourne, FL 32901 United States
AB: The strong interplanetary shock wave that
intersected the magnetosphere at about 2344 UT
on September 24, 1998, launched a compression
of the magnetosphere that was followed around
the globe by a new generation of magnetometers
with rapid sampling and precise GPS-synchronized
timing. Magnetometers of these chains included
those in the Circum-pan Pacific Magnetometer
Network (CPMN), those in the IGPP/LANL array,
those in the MEASURE array and those in the MACCS
array. The event exhibited all the classical
signatures of an SI including the preliminary
decrease before the main increase in the
H-component. A preceding depression of the magnetic
field with an amplitude of 1--2 nT also occurred
approximately 40 seconds prior to the preliminary
impulse at some low-latitude stations near local
noon. Properties of the SI signatures on the ground,
including the propagation of the preliminary
impulse, will be presented. The ability to model
this event and its induced ionospheric currents
using an MHD code allows us to compare the
compression as it is seen in the magnetosphere
with the response of the ionospheric currents.
DE: 2139 Interplanetary shocks
DE: 2740 Magnetospheric configuration and dynamics
DE: 2784 Solar wind/magnetosphere interactions
SC: SA
MN: 1999 Spring Meeting