Graduation Date

Summer 2025

Document Type

Thesis

Program

Master of Science degree with a major in Natural Resources, option Fisheries

Committee Chair Name

Darren Ward

Committee Chair Affiliation

Cal Poly Humboldt Faculty or Staff

Second Committee Member Name

Daniel Barton

Second Committee Member Affiliation

Cal Poly Humboldt Faculty or Staff

Third Committee Member Name

Alison O'Dowd

Third Committee Member Affiliation

Cal Poly Humboldt Faculty or Staff

Keywords

Survival, Radio telemetry, Movement, Dams, Salmon, Klamath River

Subject Categories

Fisheries

Abstract

The removal of four impassable hydroelectric dams on the Klamath River provides salmonids with the opportunity to recolonize their historic range in the upper Klamath River watershed. However, successful reestablishment of salmon populations requires juvenile salmon born in Oregon's upper tributaries to safely migrate downstream through the river's upper reaches. This stretch of the Klamath River, immediately downstream of Upper Klamath Lake, presents multiple migration challenges, including two flow-control dams not scheduled for removal (Link River Dam and Keno Dam), significant water diversions, and water quality issues. To evaluate these challenges, I conducted experimental releases of radio-tagged juvenile Chinook salmon over two years pre-dam removal (2022-2023). I monitored migration survival from the outlet of Upper Klamath Lake at Link River Dam downstream through Keno Dam to JC Boyle Reservoir. In both years, tagged juvenile Chinook successfully navigated downstream past both dams. Survival rates were lowest immediately downstream of Link River Dam. Although environmental factors, such as water flow and temperature, did not significantly influence survival rates, larger fish had higher survival. Additionally, water flow, temperature, and fish size significantly affected movement rate. Given that many fish survived migration through my entire study reach, these results highlight the opportunity to reestablish Chinook salmon in the Upper Klamath basin.

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