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Report on Review of 308 Report Platte River, Colo., Wyo., and Nebr., House Document No. 197 73D Congress 2nd Session on Flood Control for Bear Creek Colorado
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Report on Review of 308 Report Platte River, Colo., Wyo., and Nebr., House Document No. 197 73D Congress 2nd Session on Flood Control for Bear Creek Colorado
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Report on Review of 308 Report Platte River, Colo., Wyo., and Nebr., House Document No. 197 73D Congress 2nd Session on Flood Control for Bear Creek Colorado
State
CO
Basin
South Platte
Water Division
1
Date
3/1/1941
Author
Besson, F. S.
Title
Report on Review of 308 Report Platte River, Colo., Wyo., and Nebr., House Document No. 197 73D Congress 2nd Session on Flood Control for Bear Creek Colorado
Water Supply Pro - Doc Type
Report/Study
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II. STOR16 AND FLOOD CHARACTERISTICS <br />A. GENERAL CONSIDERATIONS <br />32. General. The flow of Bear Creek is extremely erratic. The <br />normal or base flow is derived largely from snow -melt in the high eleva- <br />tion headwater area; and it reaches its peak during May and June. During <br />the months of June, July, and August the portion of the basin between <br />Morrison and Evergreen is subject to cloudburst storms which result in <br />flash floods on the main stem and tributaries in this area. It is note- <br />worthy that there is no evidence of past floods on the main stem at ele <br />vations of over 8,000 feet, <br />33. The extremely rugged topography and the high intensity of rain- <br />fall, cause rapid concentration of run -off with very high peak rates of <br />flow. Intense rainfall from past storms in this basin has been limited <br />to small areas, seldom exceeding 20 or 25 square miles, and as the volume <br />of flood run -off is comparatively small, flood peaks are quickly moder- <br />ated downstream by the action of channel and overbank storage. <br />34. Storm rainfall in the basin is largely orographic in character. <br />The principal source of precipitable moisture is Tropical i/laritime air <br />masses which originate over the Gulf of Mexico and break out northward <br />over the Great Plains. When these warm, moisture -laden air masses are <br />deflected upward by the abrupt uplift of the foothills of the Front Range, <br />cooling and rapid condensation of moisture result. The degree of mois <br />ture saturation and instability of the air mass and its rate of ascent <br />or overturning determine the intensity of the rainfall. <br />35. Cloudburst storms of eastern Colorado,- Previous studies of <br />cloudbursts in Colorado show that most storms of this type have occurred <br />within 50 miles of the eastern slope of the Rocky Mountains and at eleva- <br />tions of from 6,000 to 7,000 feet. These storms are characterized by <br />intense rainfall for a short period and are usually confined to a rela- <br />- 11 - <br />
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