Articles | Volume 12, issue 4
Earth Syst. Dynam., 12, 1061–1098, 2021
https://doi.org/10.5194/esd-12-1061-2021
Earth Syst. Dynam., 12, 1061–1098, 2021
https://doi.org/10.5194/esd-12-1061-2021

Research article 02 Nov 2021

Research article | 02 Nov 2021

Climate change in the High Mountain Asia in CMIP6

Mickaël Lalande 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 esd-2021-43', Anonymous Referee #1, 20 Jul 2021
    • AC1: 'Reply on RC1', Mickaël Lalande, 13 Aug 2021
  • RC2: 'Comment on esd-2021-43', Anonymous Referee #2, 25 Jul 2021
    • AC2: 'Reply on RC2', Mickaël Lalande, 13 Aug 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish as is (23 Aug 2021) by Govindasamy Bala
AR by Mickaël Lalande on behalf of the Authors (14 Sep 2021)  Author's response    Manuscript

Post-review adjustments

AA: Author's adjustment | EA: Editor approval
AA by Mickaël Lalande on behalf of the Authors (21 Oct 2021)   Author's adjustment   Manuscript
EA: Adjustments approved (24 Oct 2021) by Govindasamy Bala
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Short summary
Climate change over High Mountain Asia is investigated with CMIP6 climate models. A general cold bias is found in this area, often related to a snow cover overestimation in the models. Ensemble experiments generally encompass the past observed trends, suggesting that even biased models can reproduce the trends. Depending on the future scenario, a warming from 1.9 to 6.5 °C, associated with a snow cover decrease and precipitation increase, is expected at the end of the 21st century.
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