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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />2476 <br /> <br />met by winter precipitation and irrigation water applied in excess of <br />field capacity. <br /> <br />1.3.2 Review of Evapotranspiration Methods <br /> <br /> <br />Methods for predicting evapotranspiration can be broadly classified <br /> <br /> <br />by the climatic variables used in their calculation. These are <br /> <br />temperature, radiation, and combination methods. <br /> <br />Radiation methods <br /> <br />use temperature and solar radiation while combination methods add an <br /> <br />advective energy transfer term to the radiation term. Temperature <br /> <br /> <br />methods considered in this review are the SCS modified Blaney- <br /> <br /> <br />Criddle method 2/ and FAO modified Blaney-Criddle method 2/. <br /> <br /> <br />Radiation methods considered in this review are the FAG modified <br /> <br /> <br />radiation method 2/,and four versions of the Jensen-Haise method. <br /> <br /> <br />These include the standard Jensen-Haise with and without elevation <br /> <br /> <br />correction ~/,and two modified Jensen-Raise equations calibrated <br /> <br /> <br />for conditions in northeast Utah, and the NIIP. The only combination <br /> <br /> <br />method considered is the FAO modified Penman equation ~/. <br /> <br />1.3.3 Temperature Methods <br />Temperature methods are the simplest and easiest to use of the <br />various ET prediction methods. The Blaney-Criddle formula is the <br />most popular of the temperature methods. The original form of the <br />equation as developed and later modified by H. F. Blaney and W. D. <br />Criddle in 1950 is not commonly used today. The Soil Conservation <br />Service version and the Food and Agriculture Organization of the <br /> <br />United Nations version are the most popular. <br /> <br />1- 13 <br />