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Ocean Science An interactive open-access journal of the European Geosciences Union
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Preprints
https://doi.org/10.5194/osd-7-1289-2010
© Author(s) 2010. This work is distributed under
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/osd-7-1289-2010
© Author(s) 2010. This work is distributed under
the Creative Commons Attribution 3.0 License.

Submitted as: research article 12 Jul 2010

Submitted as: research article | 12 Jul 2010

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This preprint was under review for the journal OS but the revision was not accepted.

Mixed layer sub-mesoscale parameterization – Part 2: Results for coarse resolution OGCMs

V. M. Canuto1,2 and M. S. Dubovikov1,3 V. M. Canuto and M. S. Dubovikov
  • 1NASA, Goddard Institute for Space Studies, 2880 Broadway, New York, NY, 10025, USA
  • 2Dept. Applied Physics and Math., Columbia University, New York, NY, 10027, USA
  • 3Center for Climate Systems Research, Columbia University, New York, NY, 10025, USA

Abstract. 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.

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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