Eddy diffusion coefficients in the lower thermosphere

Details Eddy diffusion coefficients in the lower thermosphere Eddy diffusion coefficients in the lower thermosphere

Jul 1983

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1983jgr....88.5765k&link_type=abstract

Journal of Geophysical Research (ISSN 0148-0227), vol. 88, July 1, 1983, p. 5765-5768. Sponsorship: Financiadora de Estudos e Pr

Other

11

Atmospheric Diffusion, Diffusion Coefficient, Thermosphere, Turbulent Diffusion, Annual Variations, Atmospheric Models, Atmospheric Turbulence

Scientific paper

The seasonal variation of the eddy diffusion coefficient is deduced for a height of 94 km at 23 deg 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.

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