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ARTICLE

Evaluating Head-of-Reservoir Water Temperature for Juvenile Chinook Salmon and Steelhead at Shasta Lake with Modeled Temperature Curtains

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Pages 1161-1175 | Received 28 Jan 2017, Accepted 26 Jun 2017, Published online: 06 Sep 2017
 

Abstract

Loss of historical spawning and rearing habitat in the rivers and tributaries of California’s Central Valley is one of the factors that led to the listing of Chinook Salmon Oncorhynchus tshawytscha and steelhead O. mykiss under the Endangered Species Act. To recover these salmonid populations, an interagency committee is developing a plan to reintroduce fish to tributaries upstream of Shasta Dam and provide juvenile fish passage downstream past the dam. One downstream fish passage alternative involves the collection and transport of juvenile fish from head-of-reservoir locations. A hydrodynamic and water quality model (CE-QUAL-W2) of Shasta Lake and its main tributaries was used to assess where and when water temperatures were favorable for juvenile salmonid collection on the McCloud River arm of the lake under different hydrologic scenarios. The application of anchored and floating temperature curtains (i.e., flexible fabric flow barriers) was examined to assess whether they could be used to improve temperature conditions for juvenile fish by reducing temperatures to within an optimal range. Model results indicated that head-of-reservoir conditions without a temperature curtain were suitable for spring-run Chinook Salmon, fall-run Chinook Salmon, and steelhead but not for winter-run and late-fall-run Chinook Salmon. However, permanent or temporary use of temperature curtains, especially a long floating curtain, may improve conditions for juvenile winter-run and late-fall-run Chinook Salmon by reducing or eliminating lethal water temperatures.

Received January 28, 2017; accepted June 26, 2017 Published online September 8, 2017

ACKNOWLEDGMENTS

Funding support was provided by USBR. We are grateful to Joe Sapin, Merlynn Bender, and Chris Berger for their support with W2; Tracy Vermeyen and Paul Fujitani for providing data from USBR; and Jason Caldwell for providing the meteorological data. We also thank Lisa Atwell and Alexes Garrett for their assistance with the graphics; and John Volk, Rowan Gaffney, Eileen Umana, and Weston Fettgather for creating and setting up the profile views of temperature conditions on the McCloud River arm. We appreciate the helpful suggestions provided by two reviewers.

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