Difference between revisions of "Hydrology"
Cellsworth (Talk | contribs) |
Cellsworth (Talk | contribs) |
||
Line 114: | Line 114: | ||
'''2018''' | '''2018''' | ||
+ | *[https://www.usbr.gov/uc/rm/amp/twg/mtgs/18jun25/Attach_02.pdf Basin Hydrology, Water Years 2018-2019 Operationts PPT] | ||
*[https://www.usbr.gov/uc/rm/amp/amwg/mtgs/18may22/Attach_02.pdf Basin Hydrology, Reservoir Operations 2018 and 2019 Hydrograph PPT] | *[https://www.usbr.gov/uc/rm/amp/amwg/mtgs/18may22/Attach_02.pdf Basin Hydrology, Reservoir Operations 2018 and 2019 Hydrograph PPT] | ||
*[https://www.usbr.gov/uc/rm/amp/twg/mtgs/18apr23/Attach_13.pdf The 21st Century Colorado River Hot Drought and Implications for the Future PPT] | *[https://www.usbr.gov/uc/rm/amp/twg/mtgs/18apr23/Attach_13.pdf The 21st Century Colorado River Hot Drought and Implications for the Future PPT] |
Revision as of 15:34, 8 November 2018
|
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 |
---|