Air-Sea Enthalpy and Momentum Exchange at Major Hurricane Wind Speeds Observed during CBLAST

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Recent Developments in the Fluid Dynamics of Tropical Cyclones (2017, unknown): “This calculation assumes that C θ / C D = 1, but the latest ﬁeld observations and laboratory measurements synthesized in Bell et al. (2012) suggest a mean value of approximately C θ / C D = 0 .”
Effects of Surface Exchange Coefficients and Turbulence Length Scales on the Intensity and Structure of Numerically Simulated Hurricanes (2012, background): “However, recent observational and laboratory studies (e.g., Powell et al. 2003; Donelan et al. 2004; Drennan et al. 2007; Jeong 2008; Haus et al. 2010; Bell 2010) found that the most intense hurricanes probably have Ck ’ 1 3 1023 and Cd ’ 2 3 10 23 (although the uncertainty is considerably large).”
Structure of the airflow above surface waves (2016, background): “The development of extreme weather events (such as hurricanes) is dependent on the drag at the ocean surface (Powell et al., 2003; Donelan et al., 2004; Bell et al., 2012).”