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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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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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Microgravity Change During the 2008–2018 Kı̄lauea Summit Eruption: Nearly a Decade of Subsurface Mass Accumulation
Results from nine microgravity campaigns from Kı̄lauea, Hawaiʻi, spanning most of the volcano's 2...
M Koymans, E de Zeeuw‐van Dalfsen, L Evers, M Poland | Journal: Journal of Geophysical Research: Solid Earth | Volume: 127 | Year: 2022 | doi: 10.1029/2022JB024739
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