Abstract:Ocean surface turbulent fluxes of momentum, heat, and water vapor respond to and determine the coupling between the atmosphere and the ocean and are excellent indicators of air-sea interactions at most temporal and spatial scales. These fluxes can be determined from bulk properties at the sea surface. By combining satellite observations of bulk properties such as sea surface temperature, wind, and humidity, estimates of these fluxes are available globally. The bulk aerodynamic formulations of these fluxes are … Show more
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