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Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
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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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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (14 Aug 2014) by Hannah Cloke
AR by Grace Garner on behalf of the Authors (07 Oct 2014)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (07 Oct 2014) by Hannah Cloke
RR by Anonymous Referee #3 (26 Oct 2014)
RR by Anonymous Referee #2 (26 Oct 2014)
ED: Publish subject to minor revisions (Editor review) (28 Oct 2014) by Hannah Cloke
AR by Grace Garner on behalf of the Authors (12 Nov 2014)  Author's response    Manuscript
ED: Publish as is (21 Nov 2014) by Hannah Cloke
Publications Copernicus
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Short summary
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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