A global nonhydrostatic semi-Lagrangian atmospheric model with orography

(1) where Zs is the altitude of orography, ZT is the height of the top of the model atmosphere, z is the geometrical height above the sea level, and operating D/Dt on (1), the vertical velocity in the terrain-following coordinate may be expressed as follows: ... (7) Here, Ve is the angular velocity...

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Veröffentlicht in:	Monthly weather review 1998-03, Vol.126 (3), p.747-771
Hauptverfasser:	QIAN, J.-H, SEMAZZI, F. H. M, SCROGGS, J. S
Format:	Artikel
Sprache:	eng
Schlagworte:	Atmosphere Coordinate transformations Earth, ocean, space Exact sciences and technology External geophysics Geophysics. Techniques, methods, instrumentation and models Meteorology Noise Orography Studies
Online-Zugang:	Volltext
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