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• W2024994473 abstract "The seasonal variation of the eddy diffusion coefficient is deduced for a height of 94 km at 23°S on the basis of two independent methods of analysis. One of these methods, already used in the past, is related to indirect measurements of atomic oxygen, and the other one is a new method related to measurements of the density of upper atmospheric sodium. The results are mutually consistent, giving a maximum eddy diffusion coefficient during summer." @default.
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• W2024994473 date "1983-07-01" @default.
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• W2024994473 title "Eddy diffusion coefficients in the lower thermosphere" @default.
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• W2024994473 doi "https://doi.org/10.1029/ja088ia07p05765" @default.
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