| Abstract: | ABSTRACT Evaporation is identified as having two additive components: natural evaporation in the absence of wind and forced evaporation in the presence of wind. An evaporation equation is obtained for an open body of water exposed at the atmosphere by conversion of standard horizontal flat plate heat transfer relationships to a mass transfer or evaporation equation. For an average air temperature of 68°F, the final equation for evaporative heat flux is  A comparison of numerical values predicted by the above equation is made with evaporation equations deduced from field measurements, and the agreement is favorable. The major differences between this equation and those previously developed are: a) the above equation was derived strictly from standard heat transfer expressions, and b) a dependency of average fetch and air temperature (through transport properties) is shown. This approach establishes the correct dependencies of the field parameters so that future experimental measurements will have a sound theoretical basis. |
