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Last modified
7/28/2009 2:35:36 PM
Creation date
3/11/2008 2:43:11 PM
Metadata
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Template:
Weather Modification
Project Name
Uintah Ecology Project
Title
Potential Ecological Impacts of Snowpack Augmentation in the Uintah Mountains, Utah
Date
4/20/1981
State
UT
Weather Modification - Doc Type
Report
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<br />INTRODUCTION <br /> <br />The Uinta Mountains are a major watershed giving rise to four of <br /> <br />Utah's major rivers: the Bear, Duchesne, Provo, and the Weber. About <br /> <br />1.8 Km3 (1.6 x 106 acre feet) of surface runoff water originate annually <br />on the range (Wasatch National Forest 1976 and Jeppson et al. 1968). <br />About 68% of that water feeds into the Green River, a major tributary of <br />the Colorado (Jeppson et al. 1968). The Uintas are thus a ,major source <br />..~~ <br />of water for the Upper Colorado Drainage Basin as well as for the Great <br />Basin portion of Utah. <br />In 1978, the Soil Conservation Service (SCS) maintained 48 precipi- <br />tation storage gages in the Uinta Mountains (Whaley and Lytton 1979a). <br />Forty-four of those gages provide total annual precipitation data for <br />the period 1973-78. Twenty-seven of the 44 stations were read on April <br />1, July 1 and October 1 during the period 1973-78. This combination of <br />stations forms the basis for the following discussion of annual preci- <br />pitation and the seasonal components thereof in the Uinta Moutains. <br />In addition to the foregoing precipitation gages, the SCS also <br />maintains 47 snow courses in the Uintas in cooperation with the U.S. <br />Forest Service and the Utah Division of Water Resources (Whaley and <br />Lytton 1979b). Thirty-seven of those courses were read annually on <br />April 1 for the period 1973-79. We here summarize characteristics of <br />the April 1 snowpack of the Uintas for the 1973-79 period based upon <br />those 37 courses. <br /> <br />18 <br /> <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 />
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