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Nonlinear saturation of atmospheric gravity waves

✍ Scribed by A.K. Nekrasov


Book ID
113171962
Publisher
Elsevier Science
Year
1994
Tongue
English
Weight
605 KB
Volume
56
Category
Article
ISSN
0021-9169

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πŸ“œ SIMILAR VOLUMES


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The equations of motion of a moist-saturated, dissipative, stratified atmmphere are used in the case of small Schmidt number, to describe the propagation of iinearized gravity waves in deep cloudy atmosphere : as in dry air, the consequence of the dissipation is the diffusion and the damping of wave

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