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<br />e <br /> <br />e <br /> <br />e <br /> <br />.0 <br /> <br /> <br />80 <br /> <br />~ <br />z <br />... <br />~ 70 <br />... <br />.. <br />o <br />o <br />... <br />~ 60 <br />< <br /> <br />"""V/Olio <br />s€>Osor, <br /> <br />-- --- <br /> <br />. <br /> <br />~ <br />~ <br />o <br />z to <br />< <br />... <br />~ <br /> <br />~~/,. I <br />.s'~<;I..s- <br /> <br />--- <br /> <br />4 <br /> <br />30 <br />o <br /> <br />2 <br /> <br />4 6 8 10 12 14 <br />AGE at:" SNOW SURfACE. DAYS <br />Figure 6. Variation in snow surface albedQ with time. <br /> <br />.. <br /> <br />EM 11I~I406 <br />5 JIUl 60 <br /> <br />--f- <br /> <br />-- <br /> <br />.. <br /> <br />20 <br /> <br />excess of 80% cover), the wind variable may be negleeted, and convection-condensation melt may <br />be computed as a function of air and dewpoint temperatures alone. <br />The convection-condensation melt equation is based on measurements of air and dewpoint <br />temperatures at the 10-foot level, and wind speeds at the 50-foot level. For forested areas, <br />wind values to be applied are those which are representative of the open portions of the basin. <br />The reductions of wind speed in the forested portions are accounted for in the selection of the <br />basin convection-condensation melt coefficient, k. Also, as explained in paragraph 3-08, when <br />measurements of air temperature and wind are at significantly different levels than those speci- <br />fied above, it is necessary to adjust them to the standard levels, The form of the genera\ <br />eonvection-condensation melt equation is that of equation 14 (par. 2-10), with the additional <br />effect of the convection-condensation melt coeffieient, k. <br /> <br />4~08. GENERALIZED BASIN SNOWMELT EQUATIONS. The following equations for rain- <br />free periods have been developed on the basis of the above-stated assumptions and requirements, <br />for varying conditions of forest environment, Exeept that they compensate for loss by forest <br />transpiration (by assuming it to be equal to shortwave radiation melt, which is not computed for <br />forested areas), the melt coefficients represent the actual melt of the snowpack, expressed as daily <br />ablation in inches of water equivalent over the snow-covered area, The coefficients also express <br />melt for a ripe snowpack (isothermal at 320 F, and with 3% free water content), <br /> <br />Heavily forested area: <br /> <br />M =0.074(0.53T;+0.47T;) <br /> <br />Forested area: <br /> <br />M ~k(O.0084v) (0.22T' .+O.78T' ,) +0.029T'. <br /> <br />Partly forested area: <br /> <br />M =k' (1- F) (0,00401,) (I-a) +k(0.0084v) (O,22T; +O,78T;) + F(0.029T;) <br />OlJen area: <br /> <br />M =k' (0,00508/,) (I-a) + (1- N) (O,0212T;-0.84) + N(O,029T;) <br />+k(O,0084v) (O.22T;+O,78T~) <br />15 <br /> <br />(22) <br /> <br />(23) <br /> <br />(24) <br /> <br />(25) <br />