Abstract
A mixing length model for air-water gas transfer is developed to include the effects of wave breaking. The model requires both the shear velocity induced by the wind and the integrated wave dissipation. Both of these can be calculated for tanks and oceans by a full spectrum wave model. The gas transfer model is calibrated, with laboratory tank measurements of carbon dioxide flux, and transported to oceanic conditions to yield air-sea transfer velocity versus wind speed.
Cite
CITATION STYLE
Donelan, M. A., & Soloviev, A. V. (2016). A mixing length model for the aqueous boundary layer including the effect of wave breaking on enhancing gas transfer. In IOP Conference Series: Earth and Environmental Science (Vol. 35). Institute of Physics Publishing. https://doi.org/10.1088/1755-1315/35/1/012001
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