Articles | Volume 26, issue 21
Hydrol. Earth Syst. Sci., 26, 5535–5554, 2022
https://doi.org/10.5194/hess-26-5535-2022
Hydrol. Earth Syst. Sci., 26, 5535–5554, 2022
https://doi.org/10.5194/hess-26-5535-2022
Research article
07 Nov 2022
Research article | 07 Nov 2022

A large-sample investigation into uncertain climate change impacts on high flows across Great Britain

Rosanna A. Lane et al.

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on hess-2021-321', Anonymous Referee #1, 22 Jul 2021
    • AC1: 'Reply on RC1', Rosanna Lane, 22 Nov 2021
  • RC2: 'Comment on hess-2021-321', Anonymous Referee #2, 30 Jul 2021
    • AC2: 'Reply on RC2', Rosanna Lane, 22 Nov 2021
  • RC3: 'Comment on hess-2021-321', Anonymous Referee #3, 13 Sep 2021
    • AC3: 'Reply on RC3', Rosanna Lane, 22 Nov 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (further review by editor and referees) (03 Dec 2021) by Nadav Peleg
AR by Rosanna Lane on behalf of the Authors (11 Feb 2022)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (22 Feb 2022) by Nadav Peleg
RR by Anonymous Referee #4 (16 Mar 2022)
RR by Anonymous Referee #3 (28 Mar 2022)
RR by Anonymous Referee #1 (28 Mar 2022)
ED: Publish subject to revisions (further review by editor and referees) (04 May 2022) by Nadav Peleg
AR by Rosanna Lane on behalf of the Authors (08 Sep 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish subject to minor revisions (further review by editor) (15 Sep 2022) by Nadav Peleg
AR by Rosanna Lane on behalf of the Authors (20 Sep 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (22 Sep 2022) by Nadav Peleg
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Short summary
This study modelled the impact of climate change on river high flows across Great Britain (GB). Generally, results indicated an increase in the magnitude and frequency of high flows along the west coast of GB by 2050–2075. In contrast, average flows decreased across GB. All flow projections contained large uncertainties; the climate projections were the largest source of uncertainty overall but hydrological modelling uncertainties were considerable in some regions.