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Physical Oceanography

, 7:99 | Cite as

A simplified model for the transformation of the atmospheric planetary boundary layer overlying a thermal front in the sea

  • V. N. Kudryavtsev
Thermohydrodynamics of the Ocean

Abstract

This paper discusses a simplified model for the evolution of the atmospheric planetary boundary layer overlying a thermal front in the sea. The model provides local values of the friction/heat transfer geostrophic coefficients and the direction of surface wind stress, as well as the wind/temperature profiles at any point on the front. With the running over a warm front, the baroclinicity of the internal boundary layer leads to the generation of a near-surface current of air directed down the front. The model can be used to interpret radar imagery of the sea surface with the purpose of determining its mesoscale variability.

Keywords

Planetary Boundary Layer Geostrophic Wind Ekman Layer Internal Boundary Layer Thermal Wind 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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Copyright information

© VSP 1996

Authors and Affiliations

  • V. N. Kudryavtsev

There are no affiliations available

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