V. M. Canuto and M. S. Dubovikov
Recent studies have shown that sub-mesoscales (SM, ~1 km) play an important role in mixed layer dynamics and have concluded that it has become necessary to include them in ocean global circulation models, OGCMs. In part A, we developed and assessed a parameterization of the vertical SM tracer flux for OGCMs that resolve mesoscales M but not SM. In the present paper, we derive a parameterization of the vertical SM tracer flux for OGCMs that do not resolve either M or SM, as those used in climate studies.
Received: 21 Jun 2010 – Discussion started: 12 Jul 2010
Publisher's note : Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this preprint. The responsibility to include appropriate place names lies with the authors.
V. M. Canuto and M. S. Dubovikov
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V. M. Canuto and M. S. Dubovikov
V. M. Canuto and M. S. Dubovikov
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