4.7 Article

Can air temperature be used to project influences of climate change on stream temperature?

Journal

ENVIRONMENTAL RESEARCH LETTERS
Volume 9, Issue 8, Pages -

Publisher

IOP PUBLISHING LTD
DOI: 10.1088/1748-9326/9/8/084015

Keywords

air temperature; stream temperature; climate projection; climate change; temperature biases; Mohseni model; salmon

Funding

  1. National Science Foundation's Long-Term Ecological Research Program [DEB 08-23380]
  2. US Forest Service Pacific Northwest Research Station
  3. Oregon State University [10-JV-11261991055]
  4. US Geological Survey
  5. Division Of Environmental Biology
  6. Direct For Biological Sciences [0823380] Funding Source: National Science Foundation

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Worldwide, lack of data on stream temperature has motivated the use of regression-based statistical models to predict stream temperatures based on more widely available data on air temperatures. Such models have been widely applied to project responses of stream temperatures under climate change, but the performance of these models has not been fully evaluated. To address this knowledge gap, we examined the performance of two widely used linear and nonlinear regression models that predict stream temperatures based on air temperatures. We evaluated model performance and temporal stability of model parameters in a suite of regulated and unregulated streams with 11-44 years of stream temperature data. Although such models may have validity when predicting stream temperatures within the span of time that corresponds to the data used to develop them, model predictions did not transfer well to other time periods. Validation of model predictions of most recent stream temperatures, based on air temperature-stream temperature relationships from previous time periods often showed poor performance when compared with observed stream temperatures. Overall, model predictions were less robust in regulated streams and they frequently failed in detecting the coldest and warmest temperatures within all sites. In many cases, the magnitude of errors in these predictions falls within a range that equals or exceeds the magnitude of future projections of climate-related changes in stream temperatures reported for the region we studied (between 0.5 and 3.0 degrees C by 2080). The limited ability of regression-based statistical models to accurately project stream temperatures over time likely stems from the fact that underlying processes at play, namely the heat budgets of air and water, are distinctive in each medium and vary among localities and through time.

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