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Linear evolution of baroclinic waves in saturated air

✍ Scribed by Maurizio Fantini


Book ID
104576411
Publisher
John Wiley and Sons
Year
1999
Tongue
English
Weight
943 KB
Volume
125
Category
Article
ISSN
0035-9009

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✦ Synopsis


Abstract

A primitive‐equation model which includes a moisture parametrization that assumes that ascending air is always saturated, has been used to study the characteristics of moist baroclinic waves, exploring their dependence on the Richardson number, besides zonal and meridional wavelength. Growth rates are shown to increase, in consequence of latent‐heat release, in a larger measure for the meridionally structured waves than for the two‐dimensional ones. Approximate analytic relationships for the normal‐modes growth rates, based on the concept of a weighted average of dry and saturated parameters, compare favourably with the numerical results. Asymmetric horizontal structures, previously obtained in quasi‐geostrophic approximation, are shown to be consistent with potential‐vorticity generation by diabatic heating in the updraught.


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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