Topside Ionospheric Structure at Northern Mid-latitudes after Ground Sunset in Summer

Details Topside Ionospheric Structure at Northern Mid-latitudes after Ground Sunset in Summer Topside Ionospheric Structure at Northern Mid-latitudes after Ground Sunset in Summer

Jun 1969

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1969natur.222.1155a&link_type=abstract

Nature, Volume 222, Issue 5199, pp. 1155-1156 (1969).

Physics

Scientific paper

DURING the period between ground sunset and ionospheric sunset, the solar light is considerably filtered during its passage through the entire atmosphere before reaching still-illuminated ionospheric regions. Most of the ionizing radiation is absorbed before it reaches the illuminated regions, hence only some heating might be caused by the long-wavelength spectrum of the incident radiation. It seems reasonable, however, to expect that topside regions are thermally stable because they have been illuminated for a long period of time.

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