Tributaries affect the thermal response of lakes to climate change

Råman Vinnå, Love; Wüest, Alfred; Zappa, Massimiliano; Fink, Gabriel; Bouffard, Damien

doi:https://doi.org/10.5194/hess-22-31-2018

Articles | Volume 22, issue 1

https://doi.org/10.5194/hess-22-31-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/hess-22-31-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 22, issue 1

Research article

|

04 Jan 2018

Research article |

| 04 Jan 2018

Tributaries affect the thermal response of lakes to climate change

Love Råman Vinnå, Alfred Wüest, Massimiliano Zappa, Gabriel Fink, and Damien Bouffard

Download

Final revised paper (published on 04 Jan 2018)
Preprint (discussion started on 03 Jul 2017)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

- Printer-friendly version

- Supplement

RC1: 'Reviewer comments', Anonymous Referee #1, 20 Jul 2017
- AC1: 'Answers to reviewer 1', Carl Love Mikael Råman Vinnå, 18 Aug 2017
RC2: 'Review of HESS 2017-337', Anonymous Referee #2, 30 Jul 2017
- AC2: 'Answers to reviewer 2.', Carl Love Mikael Råman Vinnå, 18 Aug 2017

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

ED: Reconsider after major revisions (further review by Editor and Referees) (09 Sep 2017) by Anas Ghadouani

AR by Love Råman Vinnå on behalf of the Authors (17 Oct 2017) Author's response Manuscript

ED: Referee Nomination & Report Request started (17 Oct 2017) by Anas Ghadouani

RR by Anonymous Referee #1 (31 Oct 2017)

ED: Publish as is (08 Nov 2017) by Anas Ghadouani

AR by Love Råman Vinnå on behalf of the Authors (13 Nov 2017)

Short summary

Responses of inland waters to climate change vary on global and regional scales. Shifts in river discharge regimes act as positive and negative feedbacks in influencing water temperature. The extent of this effect on warming is controlled by the change in river discharge and lake hydraulic residence time. A shift of deep penetrating river intrusions from summer towards winter can potentially counteract the otherwise negative climate effects on deep-water oxygen content.