Characteristics of acoustic-gravity waves in a diffusively separated atmosphere

Details Characteristics of acoustic-gravity waves in a diffusively separated atmosphere Characteristics of acoustic-gravity waves in a diffusively separated atmosphere

May 1979

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1979jgr....84.1865d&link_type=abstract

Journal of Geophysical Research, vol. 84, May 1, 1979, p. 1865-1879. Research supported by the Aerospace Corp.;

Physics

2

Acoustic Propagation, Atmospheric Physics, Gravity Waves, Wave Propagation, Heat Transfer, Momentum Transfer, Planetary Atmospheres, Upper Atmosphere

Scientific paper

The effects of wave-induced diffusion on the characteristics of plane acoustic gravity waves in the earth's thermosphere are investigated by means of a two fluid model atmosphere in diffusive equilibrium. At wave periods greater than the shortest characteristic diffusion time for the minor gas, diffusion induced by the wave is considered to act to eliminate amplitude and phase differences between the wave-induced density fluctuations of individual gases and restore the perturbed fluid to diffusive equilibrium. Vertical diffusion is most important at large scale sizes, but horizontal diffusion dominates for horizontal wavelengths of less than several hundred kilometers. As a result of wave-induced diffusion, AE-C satellite measurements of neutral density fluctuations of thermospheric constituents are only compatible with relatively small scale internal gravity waves. Velocity and temperature differences for acoustic-gravity waves are greatest at periods near the mean collision time and diffusion time and lead to the dissipation of wave energy. The predictions of the theory are consistent with a high latitude, low altitude source for the medium scale waves and a more localized random source for the waves observed by AE-C.

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