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WSP06362
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Last modified
1/26/2010 2:22:23 PM
Creation date
10/12/2006 1:34:51 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8210.470
Description
Pacific Southwest Interagency Committee
State
CO
Basin
Colorado Mainstem
Water Division
5
Date
11/1/1971
Author
PSIAC
Title
Pacific Southwest Analytical Summary Report on Water and Land Resources based on Framework Studies of Four Regions - November 1971
Water Supply Pro - Doc Type
Report/Study
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<br />n02611 <br /> <br />2. Possible environmental effects of the massive <br />transfer of. water'frbm the northern part of <br />C'alifornia; <br />3. The effects of continued overdraft of ground- <br />water; <br />4. The deterioration of terminal lakes resulting <br />from increased depletion of tributary stream- <br />flow; and <br />5. The degradation of water quality with more <br />intensive use. <br /> <br />The first of these problems affects all regions; the <br />second affects the California Region. The third <br />affects the Lower Colorado Region primarily, has <br />affected the California Region also, and may continue <br />unless the massive transfer of water is accomplished. <br />The fourth affects the western part of the Great Basin <br />Region; and the fifth affects all regions. <br />Many of the problems of apportionment and <br />utilization of the waters of the Colorado River Basin <br />were settled between 1922 and the present by <br />negotiation, legislation, Federal administrative action, <br />and litigation; but important problems remain. There <br />is a difference of opinion between the Upper and <br />Lower Basin States concerning the items that are to <br />be taken into account in computing the surplus water <br />available for meeting treaty requirements for delivery <br />of 1.5 million acre-feet to the Republic of Mexico. <br />The controversial items are the accounting of con- <br />sumptive uses within the basin, the gains and losses <br />below Lee Ferry - the contribution of tributaries, <br />evaporation from reservoirs - and losses (estimated <br />to be about 300,000 acre-feet per year) incurred in <br />conveying the required quantity from Lee Ferry to <br />Mexico. The commitment for delivery at Lee Ferry is <br />at ieast 7.5 million acre-feet per year averaged over a <br />lO.year period, and, according to some interpreta- <br />tions, it may be as much as 8.25 million acre.feet plus <br />a share of the iosses incurred in delivery of water to <br />Mexico. <br />In the Colorado River Basin Project Act (p.L. <br />90-537), the United States Congress declared that <br />" . . .the satisfaction of the requirements of the <br />Mexican Water Treaty from the Colorado River <br />constitutes a national obligation which shall be the <br />first obligation of any water augmentation project <br />planned pursuant to Section 201 of this Act. . . ". If <br />such augmentation is sufficient to meet the de- <br />ficiencies created by the Mexican Water Treaty, <br />judicial interpretation of the controversial points may <br />never be required. <br />The depletion requirements for water from the <br />Colorado River Basin above Lee Ferry projected to <br />2020 are about 6.5 million acre-feet (4.9 within the <br />basin and 1.6 exported). Most of this would be <br />reflected in depletion of streamflow at Lee Ferry. <br />Consequently, the projected depletions are feasible <br />only when enough water is available to satisfy them, <br /> <br />Water Resources <br /> <br /> <br />without depleting the flow at Lee Ferry more than <br />allowed by the Colorado River Compact. Current <br />usage accounts for much of the nearly complete <br />utilization of the Colorado River, when the mean <br />virgin flow at Lee Ferry is near the level at which it <br />has been for the last 40 years, with the balance of <br />usage caused by. the initial fIlling of Upper Basin <br />reservoirs. Hence, the projected depletion is de- <br />pendent on the long-term mean virgin flow which is <br />greater than the mean since 1930, or on augmenta. <br />tion of the Colorado River flow. <br />The basic apportionments of water from the main <br />stem of the Colorado River below Lee Ferry are 2.8 <br />million acre.feet for consumptive use in Arizona, 4.4 <br />million for California, 0.3 million in Nevada, and 1.5 <br />million for Mexico. Adding losses of 1.6 million <br />(estimated for 2020) from the river and main stem <br />reservoirs makes a total requirement of 10.6 million, <br />of which about 0.8 million acre-feet would be <br />supplied by tributary inflow below Lee Ferry. When <br />Upper Basin depletions reach the projected level (6.5 <br />million), augmentation will be required to meet the <br />foregoing Lower Basin requirements. <br />Although the basic allotments described above <br />combined with upstream depletions exceed the <br />natural yield of the Colorado River Basin, they are <br />not sufficient to meet requirements. California is <br />currently using surplus water in addition to its basic <br />apportionment because Arizona and Nevada do riot <br />have facilities for full utilization of their shares. <br />Nevada has completed the first stage of the Southern <br />Nevada Water Project and is delivering water from <br />Lake Mead to Las Vegas and the surrounding area. <br />With completion of the final stages of the project and <br />the Central Arizona Project facilities, California wlll <br />have to reduce its annual consumptive use of Colorado <br />River water from 4.9 to 4.4 mlllion acre-feet. Arizona <br />has chosen to use part of its share in the Phoenix- <br />Tucson area where the 1965 overdraft of ground- <br />water was about 2.5 million acre.feet. New imports to <br />the area will reduce but not eliminate the overdraft <br />even with no increase in water use. <br />The development of streamflow in the northern <br />part of the California Region to meet requirements <br />involves a large increase in surface storage capacity <br />(from 27 to 106 million acre-feet) and massive <br />transfers of water from north to south. Considerable <br />opposition to such storage and diversion has de. <br />veloped because of possible environmental effects in <br />the northern river basins and in the Sacramento River <br />Delta and San Francisco Bay. <br />Increasing water requirements in the Great Basin <br />Region generally can be met by more intensive use of <br />streamflow, greater use of groundwater, and increased <br />imports from the Colorado River Basin, provided that <br />no attempt is made to maintain Pyramid and Walker <br />Lakes. If Pyramid and Walker Lakes are to be <br /> <br />25 <br />
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