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Parameterization of the depth of the upper quasi-homogeneous layer based on measurements in the North Atlantic (Section along 53° N)

  • Marine Physics
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Oceanology Aims and scope

Abstract

The dependence of the variation in the depth of the upper mixed layer (MLD) on the governing parameters (the momentum flux, the buoyancy fluxes at the ocean surface, and the density gradient in the pycnocline) is considered. It is shown that, in the spring storm season, wind mixing dominates over convective mixing. In this case, the MLD is linearly correlated with the Ekman scale calculated from the friction velocity observed approximately 12 h before the measurement of the MLD.

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Original Russian Text © I.D. Lozovatsky, S.M. Shapovalov, 2006, published in Okeanologiya, 2006, Vol. 46, No. 3, pp. 325–330.

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Lozovatsky, I.D., Shapovalov, S.M. Parameterization of the depth of the upper quasi-homogeneous layer based on measurements in the North Atlantic (Section along 53° N). Oceanology 46, 299–304 (2006). https://doi.org/10.1134/S0001437006030015

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  • DOI: https://doi.org/10.1134/S0001437006030015

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