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Riometer measurements of ionospheric radio wave absorption
Affiliation:1. Department of Earth Sciences, 1272 University of Oregon, Eugene, OR 97403, USA;2. Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences, Staromonetny per. 35, Moscow 109017, Russia;3. School of Earth and Environmental Sciences, University of St. Andrews, St. Andrews, Fife KY16 9AL, UK;4. Institute of Precambrian Geology and Geochronology, Russian Academy of Science, St. Petersburg 199035, Russia;1. University of Iowa, Dept. of Physics and Astronomy, Iowa City, IA 52242, USA;2. LESIA, Observatoire de Paris, CNRS, UPMC, Universit Paris Diderot, Meudon, France;3. Imperial College of Science, Technology and Medicine, Space and Atmospheric Physics Group, Department of Physics, London SW7 2BW, UK;4. University of Leicester, Department of Physics and Astronomy, Leicester LE1 7RH, UK;5. Central Arizona College, Department of Science, Coolidge, AZ 85128, USA;6. Jet Propulsion Laboratory, 4800 Oak Grove Drive, Pasadena, CA 91109, USA;7. Space Environment Technologies, Planetary and Space Science Division, 320 N. Halstead Street, Suite 110, Pasadena, CA 91107, USA;8. Laboratory for Atmospheric and Space Physics, University of Colorado Boulder, 1234 Innovation Drive, Boulder, CO 80303, USA
Abstract:Absorption was calculated at two height levels in the ionosphere, from different electron density profiles. The correlation between absorption and foF2 was studied. This study bears out theoretical results that riometer absorption occurs mainly in the D-layer and less in the upper parts of the ionosphere.
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