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Static diffusion models of the upper atmosphere with empirical temperature profiles
[book]
1965
unpublished
Preserved Fulltext
all the satellites analyzed in Jacchia and Slowey, 1963) we obtain temperature variations which are, on the average, smaller by 6 percent. It should be remembered, of course, that a comparison between temperatures becomes impossible in atmospheric regions where the density is nearly independent of temperature. This situation occurs for heights lower than
doi:10.5962/bhl.title.4246
fatcat:tozti3agm5c5rocmqzeidunwdi