The exchange coefficients are close to beds and ball and well above the blades.
2.
The image below shows the equations used for calculating the exchange coefficients and fluxes, with u * as the frictional velocity.
3.
From the known variables the exchange coefficients can be easily calculated, and thus, the fluxes can be easily calculated as well.
4.
Where T _ s is the temperature of the sea surface, T _ o is the temperature of the outflow ( [ K ] ), \ Delta k is the enthalpy difference between the surface and the overlying air ( [ J / kg ] ), and C _ k and C _ d are the surface exchange coefficients ( dimensionless ) of enthalpy and momentum, respectively.
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