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Drought Stressor Monitoring Case Study UPDATE: Winter-Run Chinook Salmon Redd Dewatering Prevention in the Upper Sacramento River

Upper Sacramento River, Shasta County

2016 Update

Species / Location

The Sacramento River is home to four distinct runs (fall, late fall, spring, and winter) of Chinook Salmon (Oncorhynchus tshawytscha) (Figure 1). Winter-run Chinook Salmon (winter-run) are particularly unique compared to other salmon species found on the West Coast in that they spawn during the warm summer months. While spawning during the summer may not seem like an advantageous life history strategy, historically, winter-run spawned in upstream tributaries fed by cold water springs which would stay cool all summer long. Construction of the Shasta and Keswick Dams blocked winter-run from these historic spawning grounds. This left the uppermost reaches of the Sacramento River in Redding as the only locations with suitable spawning habitat and cold water temperatures needed for successful incubation (Figure 2).

Need for Drought Stressor Monitoring

California’s severe drought has further exacerbated the competing demands for limited water resources stored in Shasta Reservoir. The United States Bureau of Reclamation releases higher volumes of water in late spring and early summer due to water delivery needs during that time. This results in uncharacteristically high flows from May to August. Following peak demand, releases are usually reduced starting in September. Winter-run build nests called redds and spawn on underwater gravel bars from April to August. Starting in September, water releases and reductions start to fluctuate and can cause redds to be at risk of being dewatered, or exposed out of the water. Salmon eggs incubate in the gravel for approximately three months, although this timeframe varies based on water temperature, and late spawned eggs will need suitable flow through November for young to successfully emerge out of the redd.

Stressor Monitoring Efforts

Salmon eggs need specific ranges of water velocities, dissolved oxygen levels, and optimal water temperatures for embryo survival. The observed ideal velocity requirements for Chinook Salmon redds are 30-80 cm/sec (1-2.6 ft/sec) while optimal temperatures range from 5- 13°C (41-55°F) (Moyle, 2002). With this in mind, California Department of Fish and Wildlife (CDFW) and Pacific State Marine Fisheries Commission staff surveyed the redds by recording a location for each redd with a Trimble Geo7x handheld GPS unit. In addition, they documented depth, date, time, and if salmon activity was present and took a digital photograph of each redd (Figures 3 and 4). With these data, staff predicted the date when young would emerge and what flow release levels would pose dewatering risks to each redd. All redds were re-measured with every reduction of flow from Keswick Dam.

biologist from the Pacific State Marine Fisheries Commission measuring the water flow at the site of a winter-run redd towards the center of the Upper Sacramento River
Figure 3. Pacific State Marine Fisheries Commission biologist Mike Memeo measures flow over a shallow winter-run redd in the Upper Sacramento River on October 21, 2016. (CDFW photo by S. Alexander)

biologist from the Pacific State Marine Fisheries Commission measuring the water depth at the site of a winter-run redd towards the center of the Upper Sacramento River
Figure 4. Pacific State Marine Fisheries Commission biologist Zach Sigler measures depth of a shallow winter-run redd on August 29, 2016 in the Upper Sacramento River. (CDFW photo by S. Alexander)

Findings

From April 4 through November 5, 2016, a total of 28 redds were identified as being at risk of dewatering and were closely monitored following every Keswick release reduction (Figure 5). Each flow reduction was done in increments of 250 cubic feet per second to prevent any unexpected dewatering. If any redds became too close to being dewatered, future flow reductions would be postponed until eggs had hatched from that redd. Due to CDFW and the Pacific State Marine Fisheries Commission’s close monitoring of these redds and excellent communication with the United States Bureau of Reclamation to ensure that flows were high enough, no winter-run redds became dewatered.

dry, dewatered redds that had previously expired. Due to the monitoring work of CDFW, none of the studied redds died before their eggs had hatched.
Figure 5. Dewatered, expired redds in the Upper Sacramento River. The work of CDFW prevented any of the monitored redds from becoming dewatered prior to young winter-run emerging from the redd. (CDFW photo by S. Alexander)

Future Efforts

CDFW sees the biological need to continue monitoring winter-run redds to ensure the protection of this unique and endangered salmon run. Continued monitoring and collaboration will allow CDFW to effectively manage winter-run populations.

Literature Cited

Moyle, P.B 2002. Salmon and Trout, Salmonidae – Chinook Salmon, (Oncorhynchus tshawytscha) in Inland Fishes of California. Los Angeles, California: University of California press, 251-259.



Fisheries Branch
830 S Street, Sacramento, CA 95811 | (916) 327-8840


large, male winter-run Chinook salmon with hooked upper jaw, open mouth near gravel at bottom of water
Figure 1. Male winter-run Chinook Salmon. (CDFW photo by A. Jensen)

map of the locations of monitored winter-run Chinook Salmon redds and monitoring stations on the Upper Sacramento River; all redds were located downstream of the Keswick Dam - click to enlarge in new window
Figure 2. Map of locations of monitored winter-run redds on the Upper Sacramento River, Shasta County.


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