Physics
Scientific paper
Dec 2001
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001agufmsa21a..10b&link_type=abstract
American Geophysical Union, Fall Meeting 2001, abstract #SA21A-10
Physics
0355 Thermosphere: Composition And Chemistry, 0358 Thermosphere: Energy Deposition
Scientific paper
During geomagnetic storms, negative storm effects (decreases in electron density at the F2 peak) occur in the middle latitudes, particularly in the period from midnight until after dawn. These decreases in electron density are normally attributed to changes in neutral composition, the ion convection pattern and changes in temperature. In this presentation, a TING (Thermosphere-Ionosphere Nested Grid) model run that was made for a storm that occurred during the Space Weather Month period, September 12-17, 1999) is analyzed using postprocessors to study the time evolution of the processes that caused the negative storm effects during this event. Generally, the negative effects are dominated by increases in the molecular species resulting in increased recombination, but there is considerable local variation.
Burns Alan G.
Killeen Tim L.
Morin Pat
Roble Raymond G.
Wang Wenhong
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