Laserfiche WebLink
<br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />.~ <br /> <br />2478 <br /> <br />Estimates of ETp made with the above equation should be increased 10 <br /> <br />percent for each 1000 meters altitude above sea level in arid and <br /> <br />semi-arid areas. <br /> <br />Crop coefficients must be based upon grass <br /> <br />reference crops. <br /> <br />1.3.4 Radiation Methods <br /> <br />Several solar radiation-based methods have been developed. <br /> <br />The <br /> <br />Jensen-Haise and FAO modified radiation methods, however, are the <br /> <br />most commonly used. <br /> <br />They are popular because they are generally <br /> <br />more reliable than the temperature methods without having the <br /> <br />complexity or data requirements of the combination methods. <br /> <br />Jensen-Haise <br /> <br />M. E. Jensen and H. R. Haise 9/ evaluated 3000 <br />observations of ET as determined by soil sampling <br />procedures over a 35-year period. From these data they <br />developed the following linear equation for potential <br />ET: <br /> <br />ETp = Ct (T-Tx)Rs X 0.000673 lQ/ <br /> <br />( 13) <br /> <br />in which: <br /> <br />ETp is potential evapotranspiration for a well <br />watered crop of alfalfa with 30-50 cm of top <br />growth in in/day, <br /> <br />T is average daily temperature, degrees F, <br /> <br />Tx is the intercept of the temperature axis <br />(Tx = 2.5 -0.14 (e2-el) - elev/550), with <br />elevation in meters, and <br /> <br />Rs is global solar radiation in langleys/day <br />(multiplied by .000673 to obtain in/day). <br /> <br />1-15 <br />