Articles | Volume 16, issue 1
https://doi.org/10.5194/cp-16-211-2020
https://doi.org/10.5194/cp-16-211-2020
Research article
 | 
30 Jan 2020
Research article |  | 30 Jan 2020

Effect of precipitation seasonality on annual oxygen isotopic composition in the area of spring persistent rain in southeastern China and its paleoclimatic implication

Haiwei Zhang, Hai Cheng, Yanjun Cai, Christoph Spötl, Ashish Sinha, Gayatri Kathayat, and Hanying Li

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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 (06 Mar 2019) by Helen McGregor
AR by Haiwei Zhang on behalf of the Authors (14 Jun 2019)
ED: Referee Nomination & Report Request started (03 Jul 2019) by Helen McGregor
RR by Anonymous Referee #3 (12 Aug 2019)
RR by Norbert Frank (27 Sep 2019)
ED: Publish subject to minor revisions (review by editor) (13 Oct 2019) by Helen McGregor
AR by Haiwei Zhang on behalf of the Authors (26 Oct 2019)  Author's response   Manuscript 
ED: Publish as is (06 Jan 2020) by Helen McGregor
AR by Haiwei Zhang on behalf of the Authors (07 Jan 2020)  Manuscript 
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Short summary
Few studies have paid attention to the important effect of nonsummer monsoon (NSM) precipitation on the speleothem δ18O in SE China. We find the summer monsoon precipitation is equivalent to NSM precipitation amount in the area of spring persistent rain in SE China, and we discuss the relationships between seasonal precipitation amount, moisture source, δ18O, and ENSO. Characterizing the spatial differences in seasonal precipitation is key to interpreting the speleothem δ18O record.