V. M. Canuto1,2 and M. S. Dubovikov1,3
V. M. Canuto and M. S. Dubovikov
V. M. Canuto1,2 and M. S. Dubovikov1,3
1 NASA, Goddard Institute for Space Studies, 2880 Broadway, New York, NY, 10025, USA 2 Dept. Applied Physics and Math., Columbia University, New York, NY, 10027, USA 3 Center for Climate Systems Research, Columbia University, New York, NY, 10025, USA
1 NASA, Goddard Institute for Space Studies, 2880 Broadway, New York, NY, 10025, USA 2 Dept. Applied Physics and Math., Columbia University, New York, NY, 10027, USA 3 Center for Climate Systems Research, Columbia University, New York, NY, 10025, USA
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Received: 21 Jun 2010 – Accepted for review: 28 Jun 2010 – Discussion started: 12 Jul 2010
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
Interactive discussion
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Status: closed
AC : Author comment | RC : Referee comment | SC : Short comment | EC : Editor comment
Interactive discussion
Status: closed
Status: closed
AC : Author comment | RC : Referee comment | SC : Short comment | EC : Editor comment
V. M. Canuto and M. S. Dubovikov
V. M. Canuto and M. S. Dubovikov
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