O/N2 morphology during quiet and moderate auroral activity and its relation to TEC

Details O/N2 morphology during quiet and moderate auroral activity and its relation to TEC O/N2 morphology during quiet and moderate auroral activity and its relation to TEC

Dec 2005

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2005agufmsa51a1115z&link_type=abstract

American Geophysical Union, Fall Meeting 2005, abstract #SA51A-1115

Physics

0355 Thermosphere: Composition And Chemistry, 2441 Ionospheric Storms (7949)

Scientific paper

TIMED/GUVI often detects large O/N2 depletions that extend to mid and low latitudes during weak and moderate auroral activity. Auroral particle and Joule heating as well as the background wind play major roles in redistributing the high-latitude O depleted air in the thermosphere. GUVI also detects O/N2 enhancements during periods around solstice in the winter hemisphere. We note that there are occasions when an apparent O/N2 increase appears to be correlated with an increase in TEC. We will investigate the apparent correlation between enhanced O/N2 and enhanced TEC.

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