Vortex formation and vortex shedding in continuously stratified flows past isolated topography

The flow of a nonrotating atmosphere with uniform stratification and wind speed past an isolated three-dimensional topographic obstacle is investigated with a nonhydrostatic numerical model having a free-slip lower boundary. When the mountain is sufficiently high, the transient development of a quas...

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Veröffentlicht in:	Journal of the atmospheric sciences 1997-02, Vol.54 (4), p.534-554
Hauptverfasser:	SCHÄR, C, DURRAN, D. R
Format:	Artikel
Sprache:	eng
Schlagworte:	Atmosphere Earth, ocean, space Exact sciences and technology External geophysics Mathematical models Meteorology Other topics in atmospheric geophysics Turbulence Wind speed
Online-Zugang:	Volltext
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