Articles | Volume 18, issue 7
https://doi.org/10.5194/cp-18-1675-2022
https://doi.org/10.5194/cp-18-1675-2022
Research article
 | 
20 Jul 2022
Research article |  | 20 Jul 2022

Greenhouse gases modulate the strength of millennial-scale subtropical rainfall, consistent with future predictions

Fei Guo, Steven Clemens, Yuming Liu, Ting Wang, Huimin Fan, Xingxing Liu, and Youbin Sun

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • CC1: 'Comment on cp-2021-188', Long Ma, 13 Mar 2022
  • RC1: 'Comment on cp-2021-188', Anonymous Referee #1, 14 Mar 2022
  • RC2: 'Comment on cp-2021-188', Anonymous Referee #2, 22 Apr 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (12 May 2022) by Amaelle Landais
AR by Fei Guo on behalf of the Authors (23 May 2022)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (04 Jun 2022) by Amaelle Landais
RR by Anonymous Referee #1 (28 Jun 2022)
ED: Publish as is (29 Jun 2022) by Amaelle Landais
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Short summary
Our high-resolution loess Ca/Ti record displays millennial monsoon oscillations that persist over the last 650 kyr. Wavelet results indicate the ice volume and GHG co-modulation at the 100 kyr band and GHG and local insolation forcing at the precession band for the magnitude of millennial monsoon variability of loess Ca/Ti. The inferred mechanism calls on dynamic linkages to variability in AMOC. At the precession band, combined effects of GHG and insolation lead to increased extreme rainfall.