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Last modified
1/26/2010 4:18:40 PM
Creation date
10/21/2007 11:04:46 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
6/2/1998
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 - 06-02-98
Water Supply Pro - Doc Type
Report/Study
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<br />002398 <br /> <br />spring flood below the lake's surface, but as fall progresses, this mass becomes colder and <br /> <br />eventually sinks. The late summer salinity plume is convectively mixed with the colder bottom <br /> <br />hugging flow; which we have dubbed the fall SWARM bottom flow because of it's high Salinity <br /> <br />and relative WARMth (compared to other bottom layers). Oxygen levels are typically low due to <br /> <br />high oxygen demand from the inflow. This cell of water is the greatest contributor of salinity to the <br /> <br />hypolimnion on an annual basis. As the SWARM plug flows downlake, it incorporates-- through <br /> <br />diffusion, dispersion and entrainment --the previous winter's underflows that have remained <br /> <br />relatively stagnant since the spring flood first appeared. When this saline mass of water reaches the <br /> <br />dam (between February and March), it contributes to the state of meromixis if of sufficient salinity <br /> <br />to resist subsequent mixing. <br /> <br />Deep Winter FRESCO: During the deepest cold of winter, convective mixing is most extensive. <br /> <br />In the inflow area, the winter river inflow is at its coldest, most oxygen saturated, and saline. This <br /> <br />cold saline winter inflow is mixed (convective mixing and entrainment) with the last of the spring <br /> <br />flood near the inflow. A relatively FRESh plug of the lake's COldest most oxygenated water results. <br /> <br />The FRESCO bottom flow follows the SWARM plug down the bottom of the lake, typically set in <br /> <br />motion in January and February. <br /> <br />The FRESCO's downlake momentum will eventually reach the SWARM which has made contact <br /> <br />with the dam. The momentum of the FRESCO rocks the hypolimnion like a lever, moving the <br /> <br />uplake chemocline downward as the chemocline at the dam moves upward. It is at this time that the <br /> <br />highest conductivity, lowest temperature and lowest dissolved oxygen levels are discharged from <br /> <br />the penstocks, as seen in Lees Ferry water quality (Figs. 12-15). At this point uplake, the fresh cold <br /> <br />bottom plug typically has three options. I) Hvpolimnetic Overflow: If the FRESCO flow is not <br /> <br />sufficiently cold or the chemical gradient between it and the meromictic salty warm bottom plug is <br /> <br />too great, its momentum will carry it over the hypolimnion where it is entrained by the penstock <br />06/02/98 DRAFT Pe, .1 of 62 <br />
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