| http://www.w3.org/ns/prov#value | - Because of this, k{sub L} is usually estimated from empirical parameterizations for k{sub L} in terms of wind speed, U. The linear relation between F and k{sub L} at a constant {delta}C implies that the accuracy of the parameterization of k{sub L} in terms of U is critical in calculating F. This is especially true when U is large, since experiments in wind tunnels, lakes, and the ocean suggest tha
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