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- W1569574832 abstract "Numerical weather prediction (NWP) models and atmospheric dispersion models rely on parameterizations of planetary boundary layer height. In the case of a stable boundary layer, errors in boundary layer height estimation can result in gross errors in boundary-layer evolution and in prediction of turbulent mixing within the boundary layer. We use large-eddy simulations (LES) of moderately stable boundary layers to characterize the effects of various physical processes on stable boundary layers. The stable boundary layer height is assumed to be a function of surface friction velocity, geostrophic wind, Monin-Obukhov length, and the strength of the temperature inversion atop the stable boundary layer. This temperature inversion induces gravity waves with a frequency determined by the strength of the temperature inversion." @default.
- W1569574832 created "2016-06-24" @default.
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- W1569574832 date "2004-08-06" @default.
- W1569574832 modified "2023-09-23" @default.
- W1569574832 title "Influences on the Height of the Stable Boundary Layer as seen in Large-Eddy Simulations" @default.
- W1569574832 hasPublicationYear "2004" @default.
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