Articles | Volume 16, issue 1
https://doi.org/10.5194/cp-16-211-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-16-211-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
30 Jan 2020
Research article |
| 30 Jan 2020
| 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
Institute of Global Environmental Change, Xi'an Jiaotong University, Xi'an 710054, China
Institute of Earth Environment, Chinese Academy of Sciences, State Key Laboratory of Loess and Quaternary Geology, Xi'an 710061, China
Hai Cheng
Institute of Global Environmental Change, Xi'an Jiaotong University, Xi'an 710054, China
Department of Earth Sciences, University of Minnesota, Minneapolis,
Minnesota 55455, USA
Yanjun Cai
Institute of Earth Environment, Chinese Academy of Sciences, State Key Laboratory of Loess and Quaternary Geology, Xi'an 710061, China
Institute of Global Environmental Change, Xi'an Jiaotong University, Xi'an 710054, China
Christoph Spötl
Institute of Geology, University of Innsbruck, Innsbruck 6020, Austria
Ashish Sinha
Department of Earth Science, California State University Dominguez
Hills, Carson, California 90747, USA
Gayatri Kathayat
Institute of Global Environmental Change, Xi'an Jiaotong University, Xi'an 710054, China
Hanying Li
Institute of Global Environmental Change, Xi'an Jiaotong University, Xi'an 710054, China
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- Controls on leaf water hydrogen and oxygen isotopes: a local investigation across seasons and altitude J. Liu et al. 10.5194/hess-27-599-2023
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Latest update: 25 Dec 2024
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.
Few studies have paid attention to the important effect of nonsummer monsoon (NSM) precipitation...
