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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 /> <br />I <br />I <br /> <br />I <br />I <br />I <br />I <br />I <br /> <br />2480 <br /> <br />FAD Radiation <br /> <br />The FAD Radiation method is an adaptation of earlier work by G. F. <br /> <br />Makkink i/. Air temperature, sunshine, and cloudiness or <br /> <br />radiation data are required along with general levels of <br /> <br />humidity and wind. The recommended relationship is: . <br /> <br />ETp = c (W x Rs) (16) <br /> <br />in which: <br /> <br />ETp is grass based reference crop ET in mm/day, <br /> <br />Rs is solar radiation in equivalent evaporation in mm/day, <br /> <br />W is a weighting factor depending on temperature and <br />altitude, and <br /> <br />c is an adjustment factor depending on mean relative humidity <br />and daytime wind. <br /> <br />Tables and graphical solutions are presented in the original <br /> <br />document <br /> <br />to <br /> <br />determine <br /> <br />recently, <br /> <br />adjustment <br /> <br />factors. More <br /> <br />polynomial equations have been developed to speed calculation of <br /> <br />coefficients for all FAD methods using hand calculators or <br /> <br />programmable computers 12/. Equations are given in Appendix A-l.2 <br /> <br />for each method. <br /> <br />1.3.5 Combination MethOds <br /> <br />The Penman equation is by far the most commonly used of the <br /> <br />combination methods. <br /> <br />.Combination" ~efers to the two components, <br /> <br />net radiation and advective energy. <br /> <br />It has the most extensive data <br /> <br />requirements of all the methods, but is capable of the most accurate <br /> <br />1- 17 <br />