Articles | Volume 17, issue 6
Clim. Past, 17, 2481–2513, 2021
https://doi.org/10.5194/cp-17-2481-2021
Clim. Past, 17, 2481–2513, 2021
https://doi.org/10.5194/cp-17-2481-2021

Research article 02 Dec 2021

Research article | 02 Dec 2021

Holocene vegetation transitions and their climatic drivers in MPI-ESM1.2

Anne Dallmeyer 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 cp-2021-51', Qiong Zhang, 08 Jun 2021
    • AC1: 'Reply on RC1', Anne Dallmeyer, 06 Sep 2021
  • RC2: 'Comment on cp-2021-51', Anonymous Referee #2, 24 Jul 2021
    • AC2: 'Reply on RC2', Anne Dallmeyer, 06 Sep 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (10 Sep 2021) by Steven Phipps
AR by Anne Dallmeyer on behalf of the Authors (22 Sep 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (23 Sep 2021) by Steven Phipps
RR by Anonymous Referee #3 (11 Oct 2021)
ED: Publish as is (22 Oct 2021) by Steven Phipps
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Short summary
Using the comprehensive Earth system model, MPI-ESM1.2, we explore the global Holocene vegetation changes and interpret them in terms of the Holocene climate change. The model results reveal that most of the Holocene vegetation transitions seen outside the high northern latitudes can be attributed to modifications in the intensity of the global summer monsoons.