The importance of atmospheric precipitation in storm-time relativistic electron flux drop outs

During the sudden decrease of geosynchronous electron flux (>2 MeV) of 17:10–17:20 UT, January 21, 2005 large‐scale precipitation into the atmosphere was observed. Estimates from ground‐based radio propagation experiments at L∼5 in the Northern and Southern hemispheres suggest that the atmospheri...

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Published in:Geophysical research letters 2006-01, Vol.33 (1), p.n/a
Main Authors: Clilverd, Mark A., Rodger, Craig J., Ulich, Thomas
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Language:English
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Earth sciences
Earth, ocean, space
Exact sciences and technology
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Ulich, Thomas
description During the sudden decrease of geosynchronous electron flux (>2 MeV) of 17:10–17:20 UT, January 21, 2005 large‐scale precipitation into the atmosphere was observed. Estimates from ground‐based radio propagation experiments at L∼5 in the Northern and Southern hemispheres suggest that the atmospheric precipitation was less than 1/10 of the flux apparently lost during this 10 minute period. However, continuing precipitation losses from 4 < L < 6, observed for the next 2.7 hours, provides about 1/2 of the total relativistic electron content lost.
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Earth, ocean, space
Exact sciences and technology
title The importance of atmospheric precipitation in storm-time relativistic electron flux drop outs
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