Articles | Volume 15, issue 4
https://doi.org/10.5194/cp-15-1411-2019
https://doi.org/10.5194/cp-15-1411-2019
Research article
 | 
31 Jul 2019
Research article |  | 31 Jul 2019

Holocene temperature response to external forcing: assessing the linear response and its spatial and temporal dependence

Lingfeng Wan, Zhengyu Liu, Jian Liu, Weiyi Sun, and Bin Liu

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (01 Apr 2019) by Qiuzhen Yin
AR by Lingfeng Wan on behalf of the Authors (02 Apr 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (03 Apr 2019) by Qiuzhen Yin
RR by Anonymous Referee #1 (17 May 2019)
ED: Publish subject to minor revisions (review by editor) (10 Jun 2019) by Qiuzhen Yin
AR by Anna Mirena Feist-Polner on behalf of the Authors (19 Jun 2019)  Author's response
ED: Publish as is (25 Jun 2019) by Qiuzhen Yin
AR by Lingfeng Wan on behalf of the Authors (25 Jun 2019)  Author's response    Manuscript
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Short summary
The linearity of the climate response is strong on orbital and millennial scales throughout the Holocene but poor on the centennial and decadal scale. The regions of strong linear response on the millennial scale are mostly consistent with the orbital scale, notably western Eurasian, North Africa, the subtropical North Pacific, the tropical Atlantic and the Indian Ocean. This finding can improve our understanding of the regional climate response to various climate forcings.