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<br /> <br />-42- <br /> <br />EVAPORATION <br /> <br />Introduction <br /> <br />Evaporation is defined as.thephysical process 'by which water vapor <br />escapes from a water surface. The rate of evaporation depends funda- <br />mentally on many factors including ~adiation (both short- and long-wave)" <br />vapor pJ:'essure, air temperature, wind 'Movement and atmospheric pressure. <br />It is also affected by impurities such as'dust, films on the, water'surface, <br />and matter dissolved or suspended in the water. <br /> <br />This section will be restricted to discussion of methods for esti- <br />mating evaporation from a lake or reservoir (free-water surfaces), and <br />limitations of these methods. Knowledge of evaporation losses is highly <br />important in design of ,reservoirs and in, planning their most'efficient <br />operation for irrigation, hydro-electric power, water supply, or other <br />purpose. In the arid parts of the West, where evaporation greatly exceeds <br />precipitation, serious consideration must be given to the reduced water <br />yield which will resultfrcm the construction of a reservoir. It should <br />be emphasized that evaporation loss from the reservoir area is always <br />greater than the evapotranspiration loss under pre..,reservoir conditicns. <br />In humid areas, the increased loss may be of no consequence, but in arid <br />areas the utility of a regulated water supply must more than balance the <br />reduced water yield. <br /> <br />Methods of determination <br /> <br />Water budget <br /> <br />The simplest method for determining lake evaporation would seem to <br />be the water-budget method, which can be expressed by the volumetric <br />equation:. <br /> <br />E=P+I-O-.6,s <br /> <br />(1) <br /> <br />in which <br /> <br />E = lake evaporation <br />P = precipitation on lake surface <br />I = inflow, by streams or effluent ground water <br />o = outflow, by streams or influent ground water <br />S = increase in stored water <br /> <br />Reliability of the method depends on the accuracy to which each item <br />of the budget can be measured or estimated, also on the magnitude of each <br />item in relation to the evaporation. For each of the budget items, accept- <br />able percentage error diminishes about in inverse proportion to relative <br />magnitude of that particular item. Thus, unless evaporation is of about <br />the same magnitude as the largest of the budget items, its determination <br />by the water-budget method may not be reliable. <br />