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Comments on “Oscillatory Bottom Boundary Layers”
Publisher: American Meteorological Society
Comments on “Turbulence Closure, Steady State, and Collapse into Waves”
Publisher: American Meteorological Society
Abstract: Two-equation models are being increasingly used to model turbulence in geophysical flows. A salient aspect of these flows is the stable gravitational stratification, which implies that turbulent fluctuations can generate ...
On an Improved Model for the Turbulent PBL
Publisher: American Meteorological Society
Abstract: Cheng, Canuto, and Howard have presented a second-moment closure PBL model that appears to overcome some of the shortcomings of the existing Mellor and Yamada?type closure models. This note demonstrates that with a slight ...
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Publisher: American Meteorological Society
A Data-Assimilative Numerical Model of the Northern Indian Ocean
Publisher: American Meteorological Society
Abstract: A primitive equation, three-dimensional, baroclinic circulation model has been configured for use in the North Indian Ocean. After having been spun up by climatological winds, the model was used to generate a hindcast for ...
Turbulent Kinetic Energy and Its Dissipation Rate in the Equatorial Mixed Layer
Publisher: American Meteorological Society
Abstract: The authors apply a one-dimensional mixed layer model, based on second moment closure of turbulence, to study the characteristics of turbulence in the equatorial mixed layer. In particular, they focus on characteristics ...
A Diagnostic Calculation of the General Circulation in the South Atlantic Bight
Publisher: American Meteorological Society
Abstract: A diagnostic calculation that involves integration of the geostrophic equations for total transport along contours of constant planetary potential vorticity (f/H) is described and applied to the South Atlantic Bight. The ...
The Behavior of the Bulk – Skin Sea Surface Temperature Difference under Varying Wind Speed and Heat Flux
Publisher: American Meteorological Society
Abstract: The observed and predicted response of the bulk ? skin sea surface temperature difference (δT) to changes in the wind speed and net heat flux is analyzed. Observations of δT from the northern Atlantic and tropical Pacific ...