‘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–ε model suitable for applications to the atmospheric boundary layer. This K–ε model utilizes vertical viscosity and diffusivity obtained from the spectral theory. In the ε equation, the Coriolis parameter-dependent f...

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Bibliographic Details
Published in:Boundary-Layer Meteorology
Main Authors: Sukoriansky, Semion, Galperin, Boris, Perov, Veniamin
Format: Article in Journal/Newspaper
Language:unknown
Published: Digital Commons @ University of South Florida 2005
Subjects:
Atmospheric boundary layer
Spectral theories
Stable stratification
Turbulence
Life Sciences
Sea ice
Online Access:https://digitalcommons.usf.edu/msc_facpub/1486
https://doi.org/10.1007/s10546-004-6848-4
Description
Summary:A new spectral closure model of stably stratified turbulence is used to develop a K–ε model suitable for applications to the atmospheric boundary layer. This K–ε model utilizes vertical viscosity and diffusivity obtained from the spectral theory. In the ε equation, the Coriolis parameter-dependent formulation of the coefficient C 1 suggested by Detering and Etling is generalized to include the dependence on the Brunt-Väisälä frequency, N. The new K–ε 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.

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