Thermospheric neutral wind at -39 deg azimuth during the daytime sector at Sondrestrom

Details Thermospheric neutral wind at -39 deg azimuth during the daytime sector at Sondrestrom Thermospheric neutral wind at -39 deg azimuth during the daytime sector at Sondrestrom

Sep 1984

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1984georl..11..927w&link_type=abstract

Geophysical Research Letters (ISSN 0094-8276), vol. 11, Sept. 1984, p. 927-930.

Mathematics

Logic

7

Meteorological Radar, Neutral Atmospheres, Thermosphere, Wind Measurement, Daytime, Electron Density (Concentration), Ion Density (Concentration), Ion Motion, Ohmic Dissipation, Particle Precipitation, Resistance Heating

Scientific paper

Measurements with the Sondrestrom radar have been used to examine the daytime thermospheric neutral wind and to relate that wind to other geophysical parameters. Ion drag is found to be particularly important for determining the wind pattern. However, evidence is presented that the wind pattern is significantly influenced by soft particle precipitation and, possibly, by Joule heating.

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