Dynamics of a differentially-heated geophysical boundary layer
An analytical two-layer model consisting of a time-dependent stratified boundary layer topped by stratified free flow is developed in order to study atmospheric boundary layer production of vertical motion. To avoid use of a constant eddy viscosity, the boundary layer equations are layer-integrated...
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| Language: | en_US |
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2012
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| Online Access: | http://hdl.handle.net/1957/28877 |