Articles | Volume 20, issue 9
https://doi.org/10.5194/cp-20-2017-2024
https://doi.org/10.5194/cp-20-2017-2024
Research article
 | 
16 Sep 2024
Research article |  | 16 Sep 2024

Contrasting responses of summer precipitation to orbital forcing in Japan and China over the past 450 kyr

Taiga Matsushita, Mariko Harada, Hiroaki Ueda, Takeshi Nakagawa, Yoshimi Kubota, Yoshiaki Suzuki, and Youichi Kamae

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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 egusphere-2024-307', Anonymous Referee #1, 07 Mar 2024
    • AC2: 'Reply on RC1', Mariko Harada, 02 May 2024
  • RC2: 'Comment on egusphere-2024-307', Anonymous Referee #2, 10 Mar 2024
    • AC1: 'Reply on RC2', Mariko Harada, 02 May 2024

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Reconsider after major revisions (13 May 2024) by Qiuzhen Yin
AR by Mariko Harada on behalf of the Authors (23 Jun 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to minor revisions (review by editor) (03 Jul 2024) by Qiuzhen Yin
AR by Mariko Harada on behalf of the Authors (11 Jul 2024)  Author's response   Author's tracked changes   Manuscript 
EF by Sarah Buchmann (16 Jul 2024)  Supplement 
ED: Publish as is (23 Jul 2024) by Qiuzhen Yin
AR by Mariko Harada on behalf of the Authors (23 Jul 2024)
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Short summary
We present a climate simulation using version 2.3 of the Meteorological Research Institute's Coupled General Circulation Model (MRI-CGCM2.3) to examine the impact of insolation changes on East Asian summer monsoon variability over the past 450 kyr. We show that changes in summer insolation over East Asia led to distinct climatic responses in China and Japan, driven by altered atmospheric circulation due to the intensification of the North Pacific subtropical high and the North Pacific High.