Articles | Volume 17, issue 4
Clim. Past, 17, 1735–1749, 2021
https://doi.org/10.5194/cp-17-1735-2021
Clim. Past, 17, 1735–1749, 2021
https://doi.org/10.5194/cp-17-1735-2021

Research article 24 Aug 2021

Research article | 24 Aug 2021

Signals of Holocene climate transition amplified by anthropogenic land-use changes in the westerly–Indian monsoon realm

Nicole Burdanowitz et al.

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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 (17 Mar 2021) by Luc Beaufort
AR by Nicole Burdanowitz on behalf of the Authors (15 Apr 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (15 Apr 2021) by Luc Beaufort
RR by Anonymous Referee #1 (17 May 2021)
RR by Anonymous Referee #2 (21 May 2021)
ED: Publish subject to minor revisions (review by editor) (15 Jun 2021) by Luc Beaufort
AR by Nicole Burdanowitz on behalf of the Authors (09 Jul 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish subject to technical corrections (29 Jul 2021) by Luc Beaufort
AR by Nicole Burdanowitz on behalf of the Authors (03 Aug 2021)  Author's response    Manuscript
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Short summary
To study the interaction of the westerlies and Indian summer monsoon (ISM) during the Holocene, we used paleoenvironmental reconstructions using a sediment core from the northeast Arabian Sea. We found a climatic transition period between 4.6 and 3 ka BP during which the ISM shifted southwards and the influence of Westerlies became prominent. Our data indicate a stronger influence of agriculture activities and enhanced soil erosion, adding to Bond event impact after this transition period.