Physics
Scientific paper
Feb 1965
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1965jatp...27..129b&link_type=abstract
Journal of Atmospheric and Terrestrial Physics, vol. 27, no. 2, pp. 129-132
Physics
2
Scientific paper
An assumption of diffusive equilibrium with variable scale height gives good global agreement with satellite Alouette observations of the topside F2-layer. The theory also gives information on the vertical variation of the scale height, and may be applied to topside data in reduced form, as given by Kinget al. (1964a). A recent criticism of the theory by Duncan (1964) is discussed.
Baxter Roger G.
Kendall Peter C.
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