Application of the E-ε turbulence model to the atmospheric boundary layer

In the E- epsilon turbulence model, an eddy viscosity is evaluated from turbulent kinetic energy E and energy dissipation epsilon . Although still a first-order closure method in its simpler form, the E- epsilon model yields eddy viscosity for complex turbulent flows without a prior prescription of...

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Veröffentlicht in:	Boundary-layer meteorology 1985-01, Vol.33 (2), p.113-133
Hauptverfasser:	DETERING, H. W, ETLING, D
Format:	Artikel
Sprache:	eng
Schlagworte:	Convection, turbulence, diffusion. Boundary layer structure and dynamics Earth, ocean, space Exact sciences and technology External geophysics Meteorology
Online-Zugang:	Volltext
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