Difference between revisions of "Hydrology"
Cellsworth (Talk | contribs) |
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− | |1980|| | + | |1980||13.68||xx || |
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− | |1978|| | + | |1978||11.07||xx || |
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− | |1977|| | + | |1977||3.55||xx || |
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− | |1971|| | + | |1971||11.82||xx || |
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− | |1969|| | + | |1969||11.53||xx || |
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− | |1968|| | + | |1968||10.32||xx || |
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− | | | + | |1964||7.49||xx || |
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Revision as of 13:05, 25 November 2020
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Upper Colorado River Basin HydrologyThe Upper Colorado River Basin regularly experiences significant year to year hydrologic variability. During the 17-year period 2000 to 2015, however, the unregulated inflow to Lake Powell, which is a good measure of hydrologic conditions in the Colorado River Basin, was above average in only 3 out of the past 17 years. The period 2000-2016 is the lowest 17-year period since the closure of Glen Canyon Dam in 1963, with an average unregulated inflow of 8.57 maf, or 79% of the 30-year average (1981-2010). (For comparison, the 1981-2010 total water year average is 10.83 maf.) The unregulated inflow during the 2000-2016 period has ranged from a low of 2.64 maf (24% of average) in water year 2002 to a high of 15.97 maf (147% of average) in water year 2011. [1] |
Current Status |
Current Operations | Inflow Forecasts and Model Projections |
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