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On the two components of wind-driven ocean surface stress with extension to scalar fluxes
Authors:Mellor  George
Institution:1.Program in Atmospheric and Oceanic Sciences, Sayre Hall, Princeton University, Princeton, NJ, 08544, USA
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Abstract:Ocean Dynamics - When coping with numerical models of ocean surface waves and circulation, one should differentiate between wind-driven drag due to turbulent skin friction and form drag, but how to...
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