Implications of legacy watershed disturbances for channel structure and salmon habitat availability under different low-flow levels: an analysis of 45 years of discharge–habitat relationships at Carnation Creek, British Columbia

Author:

Reid David A.1,Pike Robin2,Bird Stephen3,Tschaplinski Peter4,Wilford David5

Affiliation:

1. Department of Geography, The University of British Columbia. 1984 West Mall Rd., Vancouver, BC V6T 1Z2, Canada.

2. British Columbia Ministry of Environment and Climate Change Strategy, Watershed Protection and Sustainability, P.O. Box 9362, Stn. Prov. Govt., Victoria, BC V8W 9M2, Canada.

3. Fluvial Systems Research Inc., 501-15216 North Bluff Rd., White Rock, BC V4B 0A7, Canada.

4. British Columbia Ministry of Environment and Climate Change Strategy, Conservation Science Section, P.O. Box 9338, Stn. Prov. Govt. Victoria, BC V8W 9M1, Canada.

5. British Columbia Ministry of Forests, Lands, Natural Resource Operations and Rural Development, 3333 Tatlow Rd., Smithers, BC V0J 2N5, Canada.

Abstract

In streams where water availability is limited, conservative flow ranges are often adopted by water managers to ensure that streamflow is available to meet the ecological requirements of aquatic organisms. However, a variety of natural and anthropogenic disturbances can influence stream channel morphology and in-stream wood characteristics through time, potentially altering the availability of habitat at a given flow level. Using a 2D hydrodynamic modelling approach incorporating 45 years of detailed channel morphology data from Carnation Creek, British Columbia, this paper examines relationships between legacy (forestry-driven) watershed disturbance, changes to channel morphology, and habitat availability for juvenile coho salmon (Oncorhynchus kisutch) under nine flow levels. Results indicate that substantial variability in the abundance of salmonid habitat is present through time, even when modelled flow levels are held constant. Additionally, trade-offs were observed between availability of habitat types as discharge increased. Finally, modelling results indicate that habitat availability is reduced following historical harvesting. These findings suggest that legacy watershed disturbances affecting stream channel form and function are worth considering when allocating streamflow.

Publisher

Canadian Science Publishing

Subject

Aquatic Science,Ecology, Evolution, Behavior and Systematics

Reference49 articles.

1. LARGE WOODY DEBRIS JAMS, CHANNEL HYDRAULICS AND HABITAT FORMATION IN LARGE RIVERS

2. Annear, T., Chisholm, I., Beecher, H., Locke, A., Aarrestad, P., Coomer, C. et al. 2004. Instream flows for riverine resource stewardship. [Revised ed.] Instream Flow Council, Cheyenne, Wyo.

3. Bates, D., Maechler, M., Bolker, B., Walker, S., Christensen, R. Singmann., H. et al. 2019. Package “lme4”: linear mixed-effects models using ‘Eigen’ and S4. R package, version 1.1-21.

4. Evaluation of Depth and Velocity Preferences of Juvenile Coho Salmon in Washington Streams

5. The Network Dynamics Hypothesis: How Channel Networks Structure Riverine Habitats

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