Abstract
The fluxes of momentum, energy, and water through the sea surface constitute the principal coupling between ocean and atmosphere. The momentum flux (wind stress) is a main driving force for oceanic motions, in particular for currents near the surface, along continental margins and in the main thermocline, whereas the fluxes of heat and freshwater drive the slower thermohaline component of the oceanic circulation.
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Willebrand, J. (1993). Forcing the Ocean by Heat and Freshwater Fluxes. In: Raschke, E., Jacob, D. (eds) Energy and Water Cycles in the Climate System. NATO ASI Series, vol 5. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-76957-3_9
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DOI: https://doi.org/10.1007/978-3-642-76957-3_9
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