Calculations of the evolution of the upper ocean based on the similarity theory
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Several schemes of turbulent mixing in the upper ocean are considered, including a modified scheme based on the modified Monin-Obukhov similarity theory. The schemes have been used for the calculation of the evolution of the upper ocean. The results are compared with the data of automated buoys. It is shown that the scheme based on the similarity theory gives a result not worse than the commonly used ones and has several advantages, which makes it the most appropriate for including in the ocean circulation models and climate models.
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- 1.Kitaigorodskii, S.A., Physics of the Interaction between the Atmosphere and the Ocean (Gidrometeoizdat, Leningrad, 1970) [in Russian].Google Scholar
- 7.M. F. Cronin, C. Meinig, C. L. Sabine, et al., “Surface Mooring Network in the Kuroshio Extension,” IEEE Syst. Spec. Iss. GEOSS 2(3), 424–430.Google Scholar
- 12.L. J. Mangum, H. P. Freitag, and M. J. McPhaden, “TOGA-TAO Array Sampling Schemes and Sensor Evaluations,” in OCEANS 94. Oceans Engineering for Today’s Technology and Tomorrow’s Preservation. Proceedings (1994), Vol. 2, pp. 402–406Google Scholar
- 17.R. C. Pacanovsky and G. Philander, “Parameterization of Vertical Mixing in Numerical Models of the Tropical Ocean,” J. Phys. Oceanogr. 11(11), 1442–1451 (1981).Google Scholar