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Last modified
8/16/2009 2:44:06 PM
Creation date
2/20/2007 11:04:47 AM
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Board Meetings
Board Meeting Date
11/13/2006
Description
En-Bloc Non Reimbursable Investments USGS Snowmelt Timing Study
Board Meetings - Doc Type
Memo
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<br />ST A TE OF COLORADO <br /> <br />Colorado Water Conservation Board <br /> <br />. Department of Natural Resources <br />I~B Sherman Street, ROO1l1 721 <br />Denver, Cnlor<ldo 110203 <br />Phone: (~03) H6n-~+l1 <br />FAX: (~03) Hb6-!-!7-! <br />\\' \\'\,' .L'\\'C b. ~ta tl\.('l).lIS <br /> <br /> <br />MEMORANDUM <br /> <br />Bill Owens <br />Governor <br /> <br />TO: -- -- -----C6rorado Water Conservafion Board- ~----- - <br />FROM :-- - - Michelle Garrison, Wat~r Supply Protection Program <br /> <br />Russell George <br />Executive-Director <br /> <br />Rod Kuharich <br />CWCS Director <br /> <br />DATE: <br />RE: <br /> <br />November 13. 2006 <br />Agenda Item 11f: En-Bloc Non-Reimbursable Investments <br />USGS Snowmelt Ti!l1i!,g ~~udy <br /> <br />Dan McAuliffe <br />Deputy Director <br /> <br />Introduction <br /> <br />Recent studies of streamflow timing in the Western United States indicate that over the past 50 years, snowmelt <br />runoff in much of the West is occurring earlier than in the past. The analysis noted that changes were most <br />pronounced in the Sierra Nevada, Cascades, and northern Rocky Mountains, and only minor changes in streamflow <br />timing were identitied in Colorado. The study raised important issues about the potential effects of climate change <br />. on water supplies in the west, but the results for Colorado were somewhat puzzling given local perceptions that <br />recently, melt has been occLlrring earlier in Colorado as well. <br /> <br />Because of the puzzling results for Colorado, the USGS Colorado Water Science Center conducted preliminary <br />analyses on a dozen SNOTEL and streamflow sites in selected river basins in Colorado. Results indicate that <br />snowmelt and runoff are occun'ing earlier at almost all of the sites that were tested, in some cases by as much as 2 <br />weeks. There appear to be important regional variations in the snowmelt- and runoff-timing trends, with relatively <br />strong trends in the Animas and Arkansas river basins and weaker trends in the South Platte river basin. Changes in <br />snowmelt timing at the pilot study sites were strongly correlated with increasing springtime air temperatures. These <br />preliminary results suggest a more detailed analysis is warranted, which could provide new information having <br />important implications for water resource management and availability in Colorado. <br /> <br />Discussion <br /> <br />The USGS Colorado Water Science Center proposes a detailed analysis of snowpack melt timing, streamtlow <br />runoff timing, and trends in monthly air temperature and precipitation in high-elevation areas in Colorado. The <br />objective is to document recent trends in snowmelt and runoff timing, and to quantify how those parameters are <br />affected by changing climate. Snowmelt timing will be analyzed for selected SNOTEL sites and streamtlow timing <br />will be analyzed for selected headwater streams with minimal or no diversions. All of the major river basins in the <br />westem part of the state, including those in the Front Range, will be covered. Climate data will be obtained from <br />meteorologic stations co-located with the SNOTEL sites, and trend analyses of monthly air temperature and <br />precipitation will be conducted. Results will be used to estimate potential changes in runoff amount and timing <br />under a variety of climate change scenarios to understand possible implications to water resources in Colorado <br />including changes in water use, reservoir operations, timing and magnitude of snowmelt flooding, drought <br />response, and availability of flow at certain times to meet in stream flow rights. <br />. <br /> <br />Flood rrotection . Water Supply rlanning and Finance. Sh'eam and Lake Protection <br />Water Supply Protection. Conservation and Drought Planning <br />
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