By G T Csanady,NetLibrary, Inc.
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This transfer law is again of the same form as other simplified laws of scalar transfer via molecular conduction or diffusion, except that the Resistance is now predominantly on the water side. Air-side and water-side boundary layers again characterize the concentration distributions on the two sides of the interface, but the water-side layer is much thinner, the concentration difference across it much greater. That difference for all practical purposes equals the total Force driving the transfer, χw − Sχa , leaving concentration changes negligible on the entire air side, as well as underneath the diffusion boundary layer on the water side.
67 is an approximate relationship of roughness parameters (subject to notoriously high scatter) derived from data on a single The Transfer Laws of the Air-Sea Interface 40 cooperative experiment, HEXOS. As Yelland et al. (1998) have shown, the shoaling of waves have influenced the HEXOS data on momentum flux – they may also have influenced heat and vapor transfer. Nevertheless, earlier observations already established that the scalar roughness length was much smaller than z 0 (Donelan, 1990; Smith, 1988), and that it at least did not increase with u ∗ .
1996). 2 × 10−3 within the range of the HEXOS data. 67. The slow increase of the neutral heat or vapor flux coefficient with wind speed is in fact a slightly better representation of the data than a constant C E , or C T . 67 is an approximate relationship of roughness parameters (subject to notoriously high scatter) derived from data on a single The Transfer Laws of the Air-Sea Interface 40 cooperative experiment, HEXOS. As Yelland et al. (1998) have shown, the shoaling of waves have influenced the HEXOS data on momentum flux – they may also have influenced heat and vapor transfer.
Air-sea interaction: laws and mechanisms by G T Csanady,NetLibrary, Inc.