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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 />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />003022 <br /> <br />UPPER YAMPA SUBBASIN <br /> <br />Location and Description <br /> <br /> <br />The Upper Yampa Subbasin includes the watershed <br /> <br /> <br />area of the Yampa River upstream from the U. S. Geological <br /> <br /> <br />Survey Maybell gaging station. The Yampa River heads on the <br /> <br /> <br />Continental Divide and runs in a general westerly direction <br /> <br /> <br />to its junction with the Green River in northwest Colorado. <br /> <br /> <br />The subbasin includes a major part of Routt and Moffat Coun- <br /> <br /> <br />ties and small portions of Rio Blanco and Garfield Counties. <br /> <br /> <br />The watershed is all above an elevation of 5,900 feet <br /> <br /> <br />and extends to mountain peaks over 12,400 feet along the Con- <br /> <br /> <br />tinental Divide. Over 80 percent of the watershed area is <br /> <br /> <br />above an elevation of 7,000 feet. Records show that sections <br /> <br /> <br />of the upper watershed receive over 50 inches a year of pre- <br /> <br /> <br />cipitation. <br /> <br />Watershed Runoff <br />The average annual historic runoff for the Yampa <br />River at the U. S. Geological Survey Maybell gaging station <br />for the 18-year study period of 1943-1960 amounted to <br />1,061,900 acre feet. This runoff, which originated on only <br />52 percent of the watershed area, is 82 percent of the water- <br />shed runoff for the entire basin in Colorado. About 72 per- <br />cent of the runoff originated from the melting of accumulated <br />winter snow and occurs during the three snowmelt months of May, <br />June and July. The following table gives the annual runoff <br /> <br />7 <br />