The formation of a thin horizontal layer by the interaction of a gravity wave with a wind shear as investigated by numerical methods

Details The formation of a thin horizontal layer by the interaction of a gravity wave with a wind shear as investigated by numerical methods The formation of a thin horizontal layer by the interaction of a gravity wave with a wind shear as investigated by numerical methods

Oct 1992

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992adspr..12..193a&link_type=abstract

Advances in Space Research, Volume 12, Issue 10, p. 193-197.

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An internal gravity wave critical layer problem in a stably stratified isothermal atmosphere is treated numerically by the Chebyshev spectral collocation method. The processes involved give rise to nearly horizontal layers similar to those observed in the real atmosphere. Observation of the temporal behavior of the vertical component of the wind field carried out with the EISCAT VHF radar is compared with the simulations and there is qualitatively a striking similarity between the observed data and the results of the simulations. The evolution of the wind, temperature and Richardson number Ri fields are considered.

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