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Interplanetary energetic ions and polar radio wave absorption

Journal Article · · Journal of Geophysical Research; (USA)
;  [1];  [2]; ;  [3]
  1. Univ. of Kansas, Lawrence (USA)
  2. Univ. of Calgary, Alberta (Canada)
  3. Univ. of Maryland, College Park (USA)
This is a study of the ionization input of interplanetary (including solar flare) energetic protons and alpha particles into the south polar ionosphere over the interval 1982-1985. It is well known that interplanetary ions have full and prompt access to the polar ionosphere. The incremental ionization produced at 20-120 km. altitudes causes enhanced radio wave absorption which is observed by riometers operated by the University of Maryland, at South Pole, Antarctica. The authors compute the expected absorption from the vertical structure of the ionization deposited by these energetic particles and compare the computed values with the observations. The contribution of the alpha particles is found to be quite small as a percentage of the absorption except at the peak of the day 35, 1983, event, when their contribution to the absorption is about 0.6 dB out of a total of 3.4 dB. The dominant contribution to absorption at 30 MHz usually arises from protons below 10 MeV, specifically in the 2- to 4-MeV interval. They have propagated the observed fluxes and energy spectra of protons and alpha particles through a seasonally adjusted slab model of the polar atmosphere. The atmospheric ionization resulting from the slowing and stopping of protons and alpha particles is used to estimate an equilibrium vertical ionization profile which is then convolved with an absorption efficiency profile to yield a calculated absorption. There is good agreement between the computed and observed absorption when the daily averaged absorption is above 0.1 dB; this shows that the interplanetary ions are the dominant contributors on those days.
OSTI ID:
5915564
Journal Information:
Journal of Geophysical Research; (USA), Journal Name: Journal of Geophysical Research; (USA) Vol. 94:A4; ISSN JGREA; ISSN 0148-0227
Country of Publication:
United States
Language:
English