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A one-dimensional model of the seasonal thermocline: II. The general theory and its consequences

  • Kraus E
  • Turner J
Tellus A: Dynamic Meteorology and Oceanography (1967) 19(1) 98
DOI: 10.3402/tellusa.v19i1.9753
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Abstract

Abstract A theory of the layer formation due to surface processes is presented, which is more general than that used in the preceding paper I. Convection due to heating at depth and cooling at the surface is included, as well as the mechanical stirring due to wind action. ...

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Kraus, E. B., & Turner, J. S. (1967). A one-dimensional model of the seasonal thermocline: II. The general theory and its consequences. Tellus A: Dynamic Meteorology and Oceanography, 19(1), 98. https://doi.org/10.3402/tellusa.v19i1.9753

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