Nearshore temperature findings for the Colorado River in Grand Canyon, Arizona: Possible implications for native fish

Robert P. Ross; William S. Vernieu

doi:10.3133/fs20133104

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Nearshore temperature findings for the Colorado River in Grand Canyon, Arizona: Possible implications for native fish

Robert P. Ross·William S. Vernieu

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Abstract

Since the completion of Glen Canyon Dam, Arizona, in 1963, downstream water temperatures in the main channel of the Colorado River in Glen, Marble, and Grand Canyons are much colder in summer. This has negatively affected humpback chub ( Gila cypha ) and other native fish adapted to seasonally warm water, reducing main-channel spawning activity and impeding the growth and development of larval and juvenile fish. Recently published studies by U.S. Geological Survey scientists found that under certain conditions some isolated nearshore environments in Grand Canyon allow water to become separated from the main-channel current and to warm, providing refuge areas for the development of larval and juvenile fish.

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Source-reported bounding extent: 35.65° to 37.0026° latitude; -114.0491° to -111.3451° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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Robert P. Ross, William S. Vernieu. 2013. Nearshore temperature findings for the Colorado River in Grand Canyon, Arizona: Possible implications for native fish. https://doi.org/10.3133/fs20133104

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