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Volume 18, issue 12
Hydrol. Earth Syst. Sci., 18, 5361-5376, 2014
https://doi.org/10.5194/hess-18-5361-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
Hydrol. Earth Syst. Sci., 18, 5361-5376, 2014
https://doi.org/10.5194/hess-18-5361-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 20 Dec 2014

Research article | 20 Dec 2014

What causes cooling water temperature gradients in a forested stream reach?

G. Garner et al.
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Andrews, T., Forster, P. M., and Gregory, J. M.: A surface energy perspective on climate change, J. Climate, 22, 2557–2570, 2008.
Bartholow, J. M.: The Stream Segment and Stream network Temperature Models: A Self-Study Course, US Dept. of the Interior, Open-File Report 99-112, US Geological Survey, Fort Collins, CO, USA, 2000.
Beechie, T., Imaki, H., Greene, J., Wade, A., Wu, H., Pess, G., Roni, P., Kimball, J., Stanford, J., Kiffney, P., and Mantua, N.: Restoring salmon habitat for a changing climate, River Res. Appl., 29, 939–960, 2013.
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This study demonstrates the processes by which instantaneous longitudinal water temperature gradients may be generated in a stream reach that transitions from moorland to semi-natural forest in the absence of substantial groundwater inflows. Water did not cool as it flowed downstream. Instead, temperature gradients were generated by a combination of reduced rates of heating in the forested reach and advection of cooler (overnight and early morning) water from the upstream moorland catchment.
This study demonstrates the processes by which instantaneous longitudinal water temperature...
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