Geomagnetic storm time studies using Digisonde data

Details Geomagnetic storm time studies using Digisonde data Geomagnetic storm time studies using Digisonde data

Jan 1997

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1997adspr..20.1679s&link_type=abstract

Advances in Space Research, Volume 20, Issue 9, p. 1679-1688.

Computer Science

1

Scientific paper

The initial, main and recovery stages of three magnetic storms that occurred during March 1990, June 1991 and November 1993 are discussed in terms of the response of the ionosphere as measured by Digisondes in the polar, high latitude and equatorial regions. The results show that during increased geomagnetic activity, convection velocities at high latitudes and polar regions increase, while during the main phase of intense storms the ExB vertical drift in the equatorial region is reduced. Comparison of the three storm periods indicates seasonal differences in the response of the ionosphere to increased magnetic activity.

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