Study of Ardmore, Oklahoma, storm clouds. I. Convective storm cloud initiation and development based on the remote sensing gravity-wave-induced convection

Convective instability can be induced by unstable vertical temperature profiles and can be supported by the release of latent heat of water vapour provided by a large quantity of moisture in the air. It can also be released by the presence of gravity waves. Large amplitude gravity waves have been li...

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Veröffentlicht in:	International journal of remote sensing 1991, Vol.12 (5), p.831-862
Hauptverfasser:	HUNG, R. J., TSAO, Y. D.
Format:	Artikel
Sprache:	eng
Schlagworte:	Ardmore Convection, turbulence, diffusion. Boundary layer structure and dynamics Earth, ocean, space Exact sciences and technology External geophysics Meteorology Oklahoma
Online-Zugang:	Volltext
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