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WSPC12524 (2)
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Last modified
1/26/2010 4:18:40 PM
Creation date
10/21/2007 10:54:04 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8220.101.10
Description
Colorado River Water Projects - Glen Canyon Dam-Lake Powell - Adaptive Management
State
CO
Basin
Colorado Mainstem
Date
3/6/1998
Author
DOI-GCMRC
Title
Assessment of Impacts of Glen Canyon Dam Operations on Water Quality Resources in Lake Powell and the Colorado River in Grand Canyon - Grand Canyon Monitoring and Research Center - Draft - 03-06-98
Water Supply Pro - Doc Type
Report/Study
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<br />- -;;----.-!::.. <br /> <br />002312 <br /> <br />Lake Powell to the 1094 m (3,590 ft) elevation to avoid impinging on Rainbow Bridge National <br /> <br /> <br />Monument. During this period there was maximal powerplant production at Glen Canyon Dam. <br /> <br /> <br />For a third time, after initial filling of Lake Powell was achieved in 1980, releases again exceeded <br /> <br /> <br />. '- _.10.2 km~ (8.23 mat). For the period of 1983 to 1987 annual releases_werewel1.abovethis level- <br /> <br /> <br />corresponding with wet conditions in the Upper Colorado River Basin. From 1995 to 1997, <br /> <br /> <br />annual releases again exceeded the minimum requirements. Each of these periods was followed <br /> <br /> <br />by a reduction in the salinity of the hypolimnion. <br /> <br />c.c: Monthly Release Volumes <br />Monthly release volumes are determined as part of the development of the Annual Operating <br /> <br /> <br />Plan and are based on anticipated power demands, forecasted inflows, and other factors such as <br /> <br /> <br />storage equalization between Lake Powell and Lake Mead. Typically, high releases occur in the <br /> <br /> <br />month of January and again in August, in response to increased power demands during these <br /> <br /> <br />months. Of significance is that high release volumes do not always concur with peaks in reservoir <br /> <br /> <br />inflow. An important effect of this timing is that high releases in January occur during the <br /> <br /> <br />upwelling of saline hypolimnetic water normally seen shortly after the first of the year. This <br /> <br /> <br />upwelling and its subsidence appear to be a function of the winter density currents impinging on <br /> <br /> <br />this body of water. The significance of the high January release volume is that more saline water <br /> <br />is removed from the reservoir during this upwelling than if releases were lower. Therefore, the <br /> <br />timing of these high releases facilitates the replacement of the hypolimnion near the dam. <br /> <br />d. Daily Release Volumes <br />Under existing operating criteria dictated by the recent Glen Canyon Dam ElS and Record of <br /> <br />Decision releases cannot exceed 25,000 cfs except under emergency conditions or when required <br /> <br />for flood control. Furthermore, during high release months, daily fluctuations cannot exceed 8000 <br /> <br />03/06/98 <br /> <br />DRAFF <br /> <br />Page36 of 62 <br />
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