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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 />Chapter 1: South Platte Basin Inventory <br /> <br />March 21,1998 <br />Page 1-7 <br /> <br />Left Hand Creek Near Boulder natural flow + <br />St. Vrain Creek at Lyons natural flow + <br />Big Thompson River at Mouth of Canyon. Near Drake natural flow + <br />Cache La Poudre River at Mouth of Canyon, Near Ft. Collins natural flow + <br />(estimated runoff for remaining mountain drainages) + <br />(estimated runoff for remaining plains drainages). <br /> <br />Natural flow estimates for Boulder Creek at 75th Street, which covered a 1950- <br />1985 period of hydrologic record, were obtained from previous studies by Hydrosphere <br />for the City of Boulder (Hydrosphere. 1993). <br /> <br />Natural flow estimates for Left Hand Creek and St. Vrain Creek. which covered a <br />1970-1980 period of hydrologic record, were obtained from previous studies by Leonard <br />Rice Consulting Water Engineers for the Colorado Water Resources and Power <br />Development Authority (LRCWE, 1984). These estimates were extended to cover the <br />1950-1969 period of record by correlation with natural flows for Boulder Creek at 75'" <br />Street. <br /> <br />Natural flow estimates for the Big Thompson River, which covered a 1950-1994 <br />period of hydrologic record, were obtained from previous studies by the Northern <br />Colorado Water Conservancy District (NCWCD, 1997). <br /> <br />Natural flow estimates for the Cache La Poudre River at mouth of , which <br />covered a 1950-1980 period of hydrologic record, were obtained from previous studies <br />by RCI for the City of Fort Collins (RCI, 1985). <br /> <br />The remaining mountain drainages tributary to Kersey include the Coal Creek, <br />Little Thompson, Buckhorn Creek and Cottonwood Creek drainages. While each of <br />these drainages have been gaged for some period of time, none of the records for <br />these drainages extend for more than 10 years. Natural flow estimates for these <br />remaining mountain drainages were developed by correlation of gaged flows for these <br />drainages with natural flow estimates for the Cache La Poudre at Mouth gage location <br />based upon drainage area and runoff per square mile. The resulting flow component <br />for ungaged mountain tributaries is approximately 31,000 acre-feet per year, or <br />approximately 2% of the estimated natural flow at the Kersey gage. <br /> <br />Natural flow estimates for remaining plains drainages tributary to the Kersey <br />gage were developed by measuring the remaining plains drainage area, applying an <br />average annual unit runoff factor of 1.08 inches per year (USGS 1970), and distributing <br />the estimated annual runoff into monthly fractions based on Longmont precipitation <br />data. The resulting flow component for the remaining plains drainages tributaries to <br />Kersey is approximately 155,000 acre-feet per year, or approximately 11% of the <br />estimated natural flow at the Kersey gage. <br /> <br />Hydrosphere Resource Consuhants, 1002 Walnut Suite 200, Boulder, CO 80302 <br />