Articles | Volume 26, issue 14
Research article
28 Jul 2022
Research article |  | 28 Jul 2022

Changes in nonlinearity and stability of streamflow recession characteristics under climate warming in a large glaciated basin of the Tibetan Plateau

Jiarong Wang, Xi Chen, Man Gao, Qi Hu, and Jintao Liu


Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • CC1: 'Comment on hess-2022-25', David Rupp, 15 Feb 2022
    • AC1: 'Reply on CC1', Jiarong Wang, 08 Mar 2022
  • RC1: 'Comment on hess-2022-25', Anonymous Referee #1, 18 Feb 2022
    • AC2: 'Reply on RC1', Jiarong Wang, 08 Mar 2022
  • RC2: 'Comment on hess-2022-25', Anonymous Referee #2, 06 May 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to revisions (further review by editor and referees) (31 May 2022) by Yue-Ping Xu
AR by Jiarong Wang on behalf of the Authors (31 May 2022)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (13 Jun 2022) by Yue-Ping Xu
RR by Anonymous Referee #2 (17 Jun 2022)
RR by Anonymous Referee #1 (22 Jun 2022)
ED: Publish as is (12 Jul 2022) by Yue-Ping Xu
Short summary
The accelerated climate warming in the Tibetan Plateau after 1997 has strong consequences for hydrology, geography, and social wellbeing. In hydrology, the change in streamflow as a result of changes in dynamic water storage originating from glacier melt and permafrost thawing in a warming climate directly affects the available water resources for societies of some of the most populated nations in the world.