Application of a New Spectral Theory of Stably Stratified Turbulence to the Atmospheric Boundary Layer over Sea Ice
A new spectral closure model of stably stratified turbulence is used to develop a K-D*e model suitable for applications to the atmospheric boundary layer. This K-D*e model utilizes vertical viscosity and diffusivity obtained from the spectral theory. In the D*e equation, the Coriolis parameter-depen...
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| Veröffentlicht in: | Boundary-layer meteorology 2005-11, Vol.117 (2), p.231-257 |
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| creator | Sukoriansky, Semion Galperin, Boris Perov, Veniamin |
| description | A new spectral closure model of stably stratified turbulence is used to develop a K-D*e model suitable for applications to the atmospheric boundary layer. This K-D*e model utilizes vertical viscosity and diffusivity obtained from the spectral theory. In the D*e equation, the Coriolis parameter-dependent formulation of the coefficient C suggested by Detering and Etling is generalized to include the dependence on the Brunt-Vaeisaelae frequency, N. The new K-D*e model is tested in simulations of the ABL over sea ice and compared with observations from BASE as simulated in large-eddy simulations by Kosovic and Curry, and observations from SHEBA. |
| doi_str_mv | 10.1007/s10546-004-6848-4 |
| format | Article |
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| subjects | Atmospheric boundary layer Atmospheric turbulence Boundary layers Marine Sea ice |
| title | Application of a New Spectral Theory of Stably Stratified Turbulence to the Atmospheric Boundary Layer over Sea Ice |
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