Articles | Volume 11, issue 8
https://doi.org/10.5194/cp-11-1067-2015
https://doi.org/10.5194/cp-11-1067-2015
Research article
 | 
25 Aug 2015
Research article |  | 25 Aug 2015

Multiscale monsoon variability during the last two climatic cycles revealed by spectral signals in Chinese loess and speleothem records

Y. Li, N. Su, L. Liang, L. Ma, Y. Yan, and Y. Sun

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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Ying Li on behalf of the Authors (21 Apr 2015)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (21 Apr 2015) by Marie-France Loutre
RR by Anonymous Referee #2 (08 May 2015)
RR by Anonymous Referee #1 (08 May 2015)
RR by Anonymous Referee #4 (26 May 2015)
RR by Anonymous Referee #3 (09 Jun 2015)
ED: Reconsider after major revisions (11 Jun 2015) by Marie-France Loutre
AR by Ying Li on behalf of the Authors (22 Jul 2015)  Author's response   Manuscript 
ED: Publish subject to minor revisions (review by Editor) (02 Aug 2015) by Marie-France Loutre
AR by Ying Li on behalf of the Authors (07 Aug 2015)  Author's response   Manuscript 
ED: Publish subject to technical corrections (11 Aug 2015) by Marie-France Loutre
AR by Ying Li on behalf of the Authors (17 Aug 2015)  Manuscript 
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Short summary
Multiscale signals were decomposed from Chinese loess and speleothem records over the last 260 kyr. We found great glacial and orbital impacts on the loess grain size changes and dominant precession forcing in the speleothem δ18O variability. The millennial components are evident in the loess and speleothem proxies with variances of 13 and 17%. Close matches of millennial monsoon events between these two proxies indicate similar driving force linked to high-latitude Northern Hemisphere climate.