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Impact of cascade reservoir on continuity of river water temperature: a temperature trend hypothesis in river
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  • You Xu,
  • Zhengjian Yang,
  • Jun Ma,
  • Yong Dan,
  • Defu Liu,
  • Xiaojuan Guo
You Xu
Hubei University of Technology

Corresponding Author:[email protected]

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Zhengjian Yang
Hubei Key Laboratory of Ecological Restoration of River-lakes and Algal Utilization
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Jun Ma
Hubei Key Laboratory of Ecological Restoration of River-lakes and Algal Utilization
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Yong Dan
, China Three Gorges University
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Defu Liu
Hubei University of Technology
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Xiaojuan Guo
China Three Gorges University
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Abstract

Water temperature is an important habitat factor in river ecosystems that exhibits the characteristics of continuous change. Dam construction disrupts the continuity of the water temperature and reset it, thus exerting range reduction and hysteresis effects on the characteristics of water temperature change. The effect of a dam on river continuity is directly related to the dam size. To explain this relationship, two rivers in China were selected: one river without reservoirs and one river with cascade reservoirs. Through the analysis of the longitudinal change of water temperature in free-flowing rivers, we found that water temperature changes continuously and uniformly in the longitudinal direction. Based on this, a temperature trend hypothesis in river was proposed, and the discontinuity of the water temperature in the reservoir section was evaluated. The result is as follows: (1) In mixed reservoirs, river water temperature remained as continuous as free-flowing rivers. However, the river water temperature had a large discontinuity in the stratified reservoir; (2) Water residence time was used as an indicator of the continuity of reservoir water temperature; (3) Selective withdrawal of stratified reservoirs in January could not remove the discontinuity caused by itself, but it worked in June.
15 May 2020Submitted to Hydrological Processes
18 May 2020Submission Checks Completed
18 May 2020Assigned to Editor
18 May 2020Reviewer(s) Assigned
02 Jul 2020Review(s) Completed, Editorial Evaluation Pending
03 Jul 2020Editorial Decision: Revise Major
30 Sep 20201st Revision Received
01 Oct 2020Submission Checks Completed
01 Oct 2020Assigned to Editor
01 Oct 2020Reviewer(s) Assigned
09 Nov 2020Review(s) Completed, Editorial Evaluation Pending
11 Nov 2020Editorial Decision: Revise Minor
21 Nov 20202nd Revision Received
23 Nov 2020Submission Checks Completed
23 Nov 2020Assigned to Editor
23 Nov 2020Reviewer(s) Assigned
23 Nov 2020Review(s) Completed, Editorial Evaluation Pending
23 Nov 2020Editorial Decision: Accept
Jan 2021Published in Hydrological Processes volume 35 issue 1. 10.1002/hyp.13994