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Stream temperature sensitivity to climate warming in California’s Sierra Nevada: impacts to coldwater habitat

Climatic Change volume 116, pages 149–170 (2013)Cite this article

Abstract

Water temperature influences the distribution, abundance, and health of aquatic organisms in stream ecosystems, so understanding the impacts of climate warming on stream temperature will help guide management and restoration. This study assesses climate warming impacts on stream temperatures in California’s west-slope Sierra Nevada watersheds, and explores stream temperature modeling at the mesoscale. We used natural flow hydrology to isolate climate induced changes from those of water operations and land use changes. A 21 year time series of weekly streamflow estimates from WEAP21, a spatially explicit rainfall-runoff model were passed to RTEMP, an equilibrium temperature model, to estimate stream temperatures. Air temperature was uniformly increased by 2°C, 4°C, and 6°C as a sensitivity analysis to bracket the range of likely outcomes for stream temperatures. Other meteorological conditions, including precipitation, were unchanged from historical values. Raising air temperature affects precipitation partitioning into snowpack, runoff, and snowmelt in WEAP21, which change runoff volume and timing as well as stream temperatures. Overall, stream temperatures increased by an average of 1.6°C for each 2°C rise in air temperature, and increased most during spring and at middle elevations. Viable coldwater habitat shifted to higher elevations and will likely be reduced in California. Thermal heterogeneity existed within and between basins, with the high elevations of the southern Sierra Nevada and the Feather River watershed most resilient to climate warming. The regional equilibrium temperature modeling approach used here is well suited for climate change analysis because it incorporates mechanistic heat exchange, is not overly data or computationally intensive, and can highlight which watersheds are less vulnerable to climate warming. Understanding potential changes to stream temperatures from climate warming will affect how fish and wildlife are managed, and should be incorporated into modeling studies, restoration assessments, and licensing operations of hydropower facilities to best estimate future conditions and achieve desired outcomes.

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Acknowledgements

We would like to thank the South Yuba River Citizen’s League and Sacramento Municipal Utility District for sharing measured water temperature data used for model testing. Thank you also to Leon Basdekas for modeling expertise in the initial stages of the project. Finally, we would like to thank anonymous reviewers for their thoughtful comments and suggestions.

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Authors and Affiliations

  1. Department of Watershed Sciences, Utah State University, 5210 Old Main Hill, Logan, UT, 84322-5210, USA

    Sarah E. Null

  2. Center for Watershed Sciences, University of California, Davis, Davis, CA, 95616, USA

    Joshua H. Viers & Jeffrey F. Mount

  3. Watercourse Engineering, Inc., Davis, CA, 95616, USA

    Michael L. Deas & Stacy K. Tanaka

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  1. Sarah E. Null
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  2. Joshua H. Viers
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  4. Stacy K. Tanaka
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  5. Jeffrey F. Mount
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Correspondence to Sarah E. Null.

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Null, S.E., Viers, J.H., Deas, M.L. et al. Stream temperature sensitivity to climate warming in California’s Sierra Nevada: impacts to coldwater habitat. Climatic Change 116, 149–170 (2013). https://doi.org/10.1007/s10584-012-0459-8

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  • DOI: https://doi.org/10.1007/s10584-012-0459-8

Keywords

  • Climate Warming
  • Chinook Salmon
  • Stream Temperature
  • Watershed Outlet
  • Steelhead Trout