Abstract
Thermospheric wind observations from high to mid latitudes are compared with the
newly developed Multiscale Atmosphere Geospace Environment (MAGE) model for the Nov 3–4
geomagnetic storm. The observation and simulation comparison shows a very good agreement
and is better at high latitudes in general. We were able to identify a thermospheric
poleward wind reduction possibly linked to a northward turning of the Interplanetary
Magnetic Field (IMF) at ~22 UT on Nov 3 and an enhancement of the poleward wind to a
southward turning near 10 UT on Nov 4 at high latitudes. An IMF southward turning may
have led to an enhancement of equatorward winds at Boulder, Colorado near midnight.
Simultaneous occurrence of aurora may be associated with an IMF By turning negative. The
MAGE model wind simulations are consistent with observations in these cases. The results
show the model can be a very useful tool to further study the magnetosphere and
ionosphere coupling on short time scales.
Publisher
The Korean Space Science Society
Subject
General Earth and Planetary Sciences,General Physics and Astronomy
Cited by
2 articles.
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