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<br />~ <br /> <br />-.... <br /> <br />= <br /> <br />Cloud water mixing ratio of liquid or solid at point I <br />Additional condensation (or evaporation) caused by vertical <br />displacement between points I and I+l. <br />Precipitation efficiency <br />Density of water <br />Acceleration due to gravity <br /> <br />Qx = <br />ACI,I+1= <br /> <br />E <br />Pit <br />g <br /> <br />= <br /> <br />= <br /> <br />Figure 1 is a representation of the two-dimensional flow across a <br />barrier, employed by the model, as given by Rhea (1977). The symbols <br />used are defined in equation (1). <br /> <br />Vo,qo,Oo <br /> <br />} V..q ..0. <br />API <br /> <br />2:. <br /> <br />l V2,Q2,02 <br />{ l1P2 <br /> <br />2:2 <br /> <br /> <br />2:0 <br /> <br />Xo X. X2 <br />Figure 1. Symbolic two-dimensional flow across a barrier (Rhea, 1977). <br /> <br /> <br />l1Po <br /> <br />Model Domain <br /> <br />The model domain grid employed for the Gunnison watershed modeling <br />and in the Salt-Verde study (Medina, 1991) had a point spacing of 10 km <br />in a SOO-km wide (east-west) by 470-km long (north-south) rectangle, or <br />S-km spaciI?-g and S-km greater dimensions. The Gunnison study area, <br />given in figure 2, is located on the windward slope of the continental <br /> <br />26 31 36 41 46 51 56 61 66 71 76 81 86 91 96 <br />iOl 101 <br />96 96 <br />91 91 <br />86 86 <br />81 81 <br />76 76 Figure 2. Model <br />71 71 topography for the <br />66 66 Gunnison River <br />61 61 watershed (contours <br /> in feet since the <br />56 56 model is mixed <br />51 51 mode) . <br />46 46 <br />41 41 <br />36 36 <br />31 31 <br />26 26 <br />21 21 <br />16 16 <br />11 11 <br />6 <br /> 61 <br /> <br />