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

  • Thermohydrodynamics of the Ocean
  • Published:
Physical Oceanography

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.

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Authors
  1. V. N. Kudryavtsev
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Translated by Vladimir A. Puchkin.

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Kudryavtsev, V.N. A simplified model for the transformation of the atmospheric planetary boundary layer overlying a thermal front in the sea. Phys. Oceanogr. 7, 99–125 (1996). https://doi.org/10.1007/BF02509814

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  • DOI: https://doi.org/10.1007/BF02509814

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