Correlations between atomic oxygen airglow and radio wave absorption in winter

Details Correlations between atomic oxygen airglow and radio wave absorption in winter Correlations between atomic oxygen airglow and radio wave absorption in winter

Apr 1980

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1980jatp...42..331w&link_type=abstract

Journal of Atmospheric and Terrestrial Physics, vol. 42, Apr. 1980, p. 331-337. Research supported by the Instituto Nacional de

Physics

Airglow, Electromagnetic Absorption, Electron Density Profiles, Oxygen Atoms, Radio Waves, Winter, Abnormalities, Data Correlation, Diurnal Variations, Radio Attenuation, Sporadic E Layer

Scientific paper

The correlation at latitude 37 deg N between zenith brightness of 557.7 nm atomic oxygen airglow and short wave radio wave absorption was investigated. A correlation seems to exist only when the amount of absorption is relatively low anddoes not exceed a certain critical value. Electron density profiles measured when the radio wave absorption was slightly below the critical value, slightly above it, and winter-anomalous show that the main contribution to absorption is shifted to lower heights when absorption increases and becomes winter-anomalous. Results of DC probe measurements suggest that the atmospheric temperature increases when this change occurs.

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