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<br />Figure <br /> <br />21 <br /> <br />22 <br /> <br />23 <br /> <br />24 <br /> <br />25 <br /> <br />26 <br /> <br />27 <br /> <br />28 <br /> <br />29 <br /> <br />30 <br /> <br />31 <br /> <br />32 <br /> <br />33 <br /> <br />34 <br /> <br />35 <br /> <br />36 <br /> <br />37 <br /> <br />38 <br /> <br />39 <br /> <br />40 <br /> <br />San Juan Sub-Basin, <br /> <br />Upper Colorado Sub- Basin. <br /> <br />North-South and East- West profiles, Upper Colorado and Yampa Drainage <br />Basins. <br /> <br />Distribution of snowfall at Climax, Colorado, as a function of the hourly <br />intensity. Data is fOr' November through May, 1964-67. <br /> <br />Cumulative distribution of snowfall intensity at San Juan Mountain stations, <br />November through April 1948-68. <br /> <br />Cumula.tive distribution of snowfall intensity at lower elevation stations in <br />the San Juan area, November through April 1948-68. <br /> <br />Cumulative contribution of precipitation intensities to total snowfall, <br />November through April 1948-68. <br /> <br />Cumulative contribution of precipitation intensities to total snowfall, <br />November through April 1948-68. <br /> <br />Distribution of snowfall at Climax, Colorado, as a function of the hour of <br />day, November through May, 1964-67. <br /> <br />Six month diurnal frequency pattern of hourly precipitation, November - <br />April for three seasons, at four stations, in or near the Upper Colorado <br />River area above Kremmling. <br /> <br />Diurnal frequency of snowfall at Ouray and Wagonwheel Gap, November- <br />April, 1948-68. <br /> <br />Diurnal frequency of snowfall at Durango, November - April, 1948-68. <br /> <br />Diurnal frequency of snowfall at Silverton, 2NE, Telluride, and Mesa <br />Verde, November - April 1948-68. <br /> <br />Relative per cent of daily snowfall occurring at the respective hours of <br />the day, November - April 1948-68. <br /> <br />Wolf Creek Summit daily distribution of snowfall, November 1958 - April <br />1968 (November - April). <br /> <br />Examples of daily temperature range during continuous cloud cover and <br />snow at Climax 2NW. <br /> <br />Solid Lines: Mean Daily Snowfall at Climax, Colorado, as a function <br />of the cloud top temperature (500 mb). Dashed Line: Adiabatic conden- <br />sate realized from lifting a parcel upward through a saturated 700 - 500 <br />mb layer. <br /> <br />(a) Mean Daily Snowfall at Climax as a function of cloud top temperature <br />(500 mb). (b) Distributions of total snowfall and total occurrences as a <br />function of cloud top temperature (500 mb). <br /> <br />Solid lines: Mean Daily Snowfall at Wolf Creek Pass as a function of <br />cloud top temperature (500 mb). Dashed Lines: Adiabatic condensate <br />realized from lifting a parcel upward through a saturated 700 - 500 mb <br />layer. <br /> <br />(a) Mean Daily Snowfall at Wolf Creek Pass as a function of cloud top <br />temperature (500 mb). (b) Distributions of total snowfall and total <br />occurrences as a function of cloud top temperature (500 mb). <br /> <br />ix <br /> <br />Page Numbers <br /> <br />35 <br /> <br />36 <br /> <br />38 <br /> <br />41 <br /> <br />41 <br /> <br />41 <br /> <br />42 <br /> <br />42 <br /> <br />43 <br /> <br />43 <br /> <br />44 <br />44 <br />44 <br />44 <br />52 <br />52 <br />53 <br /> <br />53 <br /> <br />54 <br /> <br />54 <br />