Surface-Layer Flux–Gradient Relationships over Inclined Terrain Derived from a Local Equilibrium, Turbulence Closure Model

Derivation of surface-layer flux–gradient relationships from a local-equilibrium, turbulence-closure model for a forced flow over inclined terrain is presented. Results are shown as a generalization of Monin–Obukhov universal functions respesenting non-dimensional wind and temperature gradients.

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Bibliographische Detailangaben
Veröffentlicht in:	Boundary-layer meteorology 2014-03, Vol.150 (3), p.469-483
1. Verfasser:	Lobocki, Lech
Format:	Artikel
Sprache:	eng
Schlagworte:	Analysis Atmospheric Protection/Air Quality Control/Air Pollution Atmospheric Sciences Boundaries Boundary layer Computational fluid dynamics Convection, turbulence, diffusion. Boundary layer structure and dynamics Derivation Earth and Environmental Science Earth Sciences Earth, ocean, space Equilibrium Exact sciences and technology External geophysics Fluid flow Geophysics. Techniques, methods, instrumentation and models Meteorology Numerical weather forecasting Surface chemistry Temperature gradient Temperature gradients Terrain Turbulence Turbulence models Turbulent flow
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Beschreibung
Zusammenfassung:	Derivation of surface-layer flux–gradient relationships from a local-equilibrium, turbulence-closure model for a forced flow over inclined terrain is presented. Results are shown as a generalization of Monin–Obukhov universal functions respesenting non-dimensional wind and temperature gradients.
ISSN:	0006-8314 1573-1472
DOI:	10.1007/s10546-013-9888-9