Difference between revisions of "Hydrology"
Cellsworth (Talk | contribs) |
Cellsworth (Talk | contribs) |
||
Line 158: | Line 158: | ||
*[https://www.usbr.gov/uc/rm/amp/amwg/mtgs/12feb22/Attach_09.pdf AIF: Basin Hydrology and Operations PPT] | *[https://www.usbr.gov/uc/rm/amp/amwg/mtgs/12feb22/Attach_09.pdf AIF: Basin Hydrology and Operations PPT] | ||
*[https://www.gcmrc.gov/about/ka/KA%202%20-%2010-19-11/AM%20Talks/Grams%20Flow%20Temp%20Turbidity.pdf Flow Temp Turbidity ] | *[https://www.gcmrc.gov/about/ka/KA%202%20-%2010-19-11/AM%20Talks/Grams%20Flow%20Temp%20Turbidity.pdf Flow Temp Turbidity ] | ||
+ | |||
+ | '''2011''' | ||
+ | *[https://www.usbr.gov/uc/rm/amp/amwg/mtgs/11aug24/Attach_08.pdf AIF: Basin Hydrology and PPT] | ||
'''2003''' | '''2003''' |
Revision as of 14:41, 9 June 2017
|
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 |
---|