Wave‐Related Reynolds Number Parameterizations of CO2 and DMS Transfer Velocities

Predicting future climate hinges on our understanding of and ability to quantify air‐sea gas transfer. The latter relies on parameterizations of the gas transfer velocity k, which represents physical mass transfer mechanisms and is usually parameterized as a nonlinear function of wind forcing. In an...

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Veröffentlicht in:	Geophysical research letters 2017-10, Vol.44 (19), p.9865-9875
Hauptverfasser:	Brumer, Sophia E., Zappa, Christopher J., Blomquist, Byron W., Fairall, Christopher W., Cifuentes‐Lorenzen, Alejandro, Edson, James B., Brooks, Ian M., Huebert, Barry J.
Format:	Artikel
Sprache:	eng
Schlagworte:	Aerodynamics air‐sea gas transfer Bubble barriers Carbon dioxide CO2 Covariance Dimethyl sulfide DMS Eddy covariance Empirical analysis Fluid flow Future climates Gas exchange Gases Hinges Mass transfer Mathematical models Oceanic analysis Reynolds number Sea state Solubility Statistical analysis Statistical methods Sulfides Sulphides Temperature (air-sea) Velocity Vortices Wave breaking wave‐related Reynolds numbers Wind speed wind waves
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