Physics
Scientific paper
Dec 2011
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011agufmsa51a1927c&link_type=abstract
American Geophysical Union, Fall Meeting 2011, abstract #SA51A-1927
Physics
[2407] Ionosphere / Auroral Ionosphere, [2435] Ionosphere / Ionospheric Disturbances, [2437] Ionosphere / Ionospheric Dynamics, [2441] Ionosphere / Ionospheric Storms
Scientific paper
Tongue of ionization (TOI) events in both the northern and southern hemisphere have been identified with polar maps of total electron content (TEC) derived from the global network of GPS receivers. The TOI, as observed by GPS, extends through the dayside cusp, across the polar cap to the nightside, in both hemispheres. The TOI is a source of ionospheric irregularities and its distribution across the high latitude ionosphere is controlled by plasma convection. In the northern hemisphere, GPS maps show the development of TOI from mid-latitude plumes of ionization known as storm enhanced density (SED). The SED feature is observed to be magnetically conjugate, although data coverage is considerably more sparse in the southern hemisphere. In this talk, the focus is on southern hemisphere TOI observations using GPS and COSMIC TEC polar plots overlaid onto SuperDARN HF radar observations of the high-latitude convection pattern. Solar minimum and solar maximum TOI observations are compared, and the locations where HF scatter is observed in the presence of TOI plumes are examined. We explore the similarities between TOI events observed simultaneously in the two hemispheres and look especially for the impact of convection-induced asymmetries. Gradients, irregularities, and velocities are examined between the two hemispheres.
Baker Joseph B.
Coster Anthea J.
Ruohoniemi Michael J.
Thomas Gareth E.
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