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Evaluation study of the Kain-Fritsch convection scheme
Cumulus clouds occur on spatial scales that are too small to be explicitly resolved by state of t...
Sander Jonkers | Year: 2004 | Pages: 69
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Salmon's Hamiltonian approach to balanced flow applied to a one-layer isentropic model of the atmosphere
Salmon's Hamiltonian approach is applied to formulate a balanced approximation to a hydrostatic o...
WTM Verkley | Status: published | Journal: Quart. J. Royal Meteorol. Soc. | Volume: 127 | Year: 2000 | First page: 579 | Last page: 600
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Vertical profiles of the structure parameter of refractive index and the structure parameter of temperature in the earth 's atmosphere
Vertical profiles of the structure parameter of temperature CT2 in the stable, nocturnal boundary...
J.W.M. Cuijpers | Year: 1987 | Pages: 64
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Central Sudan surface wind data and climate characteristics
Since the last decade the modelling of the tropical boundary layer is an outstanding problem, due...
E.H. Abu Bakr | Year: 1988 | Pages: 54
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Detailstucturen in depressies : een analytisch model
An integrated two-parameter model has been used, based on the quasi-geostrophic vorticity and the...
L.C. Heijboer | Year: 1981 | Pages: 38
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