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Last modified
1/26/2010 12:48:38 PM
Creation date
10/11/2006 11:32:16 PM
Metadata
Fields
Template:
Water Supply Protection
File Number
8200.765
Description
White River General
State
CO
Basin
Yampa/White
Water Division
6
Date
10/1/1979
Author
David E Fleming
Title
Environmental Assessment Report - Rangely Project - Taylor Draw Reservoir
Water Supply Pro - Doc Type
Report/Study
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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 />U027il5 <br /> <br />Taylor Draw Reservoir capacity will be 13,800 AF, with <br />the possibility of utilizing the remainder of the storage entitle- <br />ment for later expansion of the project (1). <br /> <br />In the initial years of the project, it is probable that <br />the major use of water will be for irrigation, municipal use, and <br />power generation. As natural resources in the area become more fully <br />developed, the need for industrial water will become increasingly <br />greater. The value of water for this use will far exceed all others. <br /> <br />4. White River Floods <br /> <br />Flood patterns of the White River differ depending upon the <br />location along the river being considered. In the upper reaches of <br />the river peak flows invariably occur as a result of spring snowmelt <br />while peak flows in the lower reaches are more likely to result from <br />heavy rains on lower tributaries. Potentially, the maximum flood at <br />the dam site could occur if snowmelt runoff in the upper basin were <br />combined with heavy rainstorms on the tributaries immediately above <br />the dam site. The pattern' of precipitation is such that heavy rains <br />seldom occur during the period of peak runoff from snowmelt. When <br />they do, they are so widespread in character that their cooling effect <br />reduces the rate of snowmelt to the point where total stream flow may <br />be only slightly affected. In general, streams depending on mountain <br />snowmelt for the major portion of their runoff show an inverse re- <br />lationship between rainfall and runoff during the spring flood <br />season (15). <br /> <br />The Army Corps of Engineers (COE) performed a flood study of <br />the Town of Rangely for flood insurance purposes in 1976. The COE <br />report developed floods for the 10-, 50-, 100- and 500-year storms <br /> <br />II-25 <br />
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