Articles | Volume 14, issue 5
https://doi.org/10.5194/cp-14-653-2018
https://doi.org/10.5194/cp-14-653-2018
Research article
 | 
24 May 2018
Research article |  | 24 May 2018

Decreasing Indian summer monsoon on the northern Indian sub-continent during the last 180 years: evidence from five tree-ring cellulose oxygen isotope chronologies

Chenxi Xu, Masaki Sano, Ashok Priyadarshan Dimri, Rengaswamy Ramesh, Takeshi Nakatsuka, Feng Shi, and Zhengtang Guo

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (18 Jul 2017) by Michael Evans
AR by Masaki Sano on behalf of the Authors (02 Sep 2017)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (13 Oct 2017) by Michael Evans
RR by Anonymous Referee #1 (18 Oct 2017)
RR by Anonymous Referee #3 (06 Nov 2017)
RR by Richard Fiorella (08 Nov 2017)
RR by Anonymous Referee #2 (09 Nov 2017)
ED: Reconsider after major revisions (04 Dec 2017) by Michael Evans
AR by Masaki Sano on behalf of the Authors (26 Jan 2018)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (29 Jan 2018) by Michael Evans
RR by Anonymous Referee #2 (23 Feb 2018)
ED: Publish subject to minor revisions (review by editor) (05 Apr 2018) by Michael Evans
AR by Masaki Sano on behalf of the Authors (12 Apr 2018)  Author's response    Manuscript
ED: Publish subject to technical corrections (23 Apr 2018) by Michael Evans
AR by Masaki Sano on behalf of the Authors (24 Apr 2018)  Author's response    Manuscript
Download
Short summary
We have constructed a regional tree ring cellulose oxygen isotope record using a total of five chronologies obtained from the Himalaya. Centennial changes in the regional tree ring record indicate a trend of weakened Indian summer monsoon (ISM) intensity since 1820. Decreasing ISM activity is also observed in various high-resolution ISM records from southwest China and Southeast Asia, and may be the result of reduced land–ocean thermal contrasts since 1820.