Abstract
Under a wide variety of meteorological conditions in a coastal environment, 250 cases were studied to determine the typical influences of moisture in calculating the gradient Richardson number stability and the fluxes of heat, humidity, and momentum with the profile method. Although the stability calculation was altered in some cases up to 95% by the moisture correction, the typical influence in computing the fluxes was found to be less than 10% when the humidity flux was upward and less then 25% when the humidity flux was downward.
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