1965
DOI: 10.3133/pp441
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Water resources of the Upper Colorado River Basin - Technical report

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Cited by 69 publications
(41 citation statements)
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“…These watersheds are affected by one or more climatically different seasons: frontal rainstorms and snowmelt in the winter and spring, and spotty intensive thunderstorms in the summer. The combination of lithology, catchment area, and rainfall and runoff regimes render these basins highly productive in sediment yield and suspended matter concentration during the summer, while less affected by erosion and transport during the winter (as is clearly demonstrated by the Paria River; data from Iorns, Hembree and Oakland (1965). U.S. Geological Survey Water Supply Paper 1995).…”
Section: The Selected Watersheds-environmental Settingmentioning
confidence: 99%
“…These watersheds are affected by one or more climatically different seasons: frontal rainstorms and snowmelt in the winter and spring, and spotty intensive thunderstorms in the summer. The combination of lithology, catchment area, and rainfall and runoff regimes render these basins highly productive in sediment yield and suspended matter concentration during the summer, while less affected by erosion and transport during the winter (as is clearly demonstrated by the Paria River; data from Iorns, Hembree and Oakland (1965). U.S. Geological Survey Water Supply Paper 1995).…”
Section: The Selected Watersheds-environmental Settingmentioning
confidence: 99%
“…Again, these sediment concentrations are 38 percent greater for the Yampa River and 61 percent greater for the Little Snake River than those estimated by lorns, Hembree, and Oakland (1965). Although the average-annual suspended-sediment concentration in the Little Snake River is an order of magnitude greater than in the Yampa River, the total sediment load from the Yampa River subbasin is about 3 to 4 times greater, due to the relatively lower flow from the Little Snake River subbasin.…”
Section: I«3armentioning
confidence: 63%
“…Based on analysis of these records, the estimated mean annual suspended-sediment load from the basin is about 2.0 million tons (1.8 million t), which is 11 percent higher than that estimated by lorns, Hembree, and Oakland (1965). The difference may be accounted for largely by the inclusion of bedload estimates in Andrews (1978) computations.…”
Section: I«3armentioning
confidence: 84%
“…A comprehensive study of surface-water resources of the Upper Colorado River Basin, which included the Green River Basin in Wyoming, was made by lorns, Hembree, and Oakland (1965). Their report discusses water quantity and quality and determines the effects of water use on streamflow.…”
Section: Summary Of Previous Studiesmentioning
confidence: 99%