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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Cited articles

Baker, A. J., Sodemann, H., Baldini, J. U., Breitenbach, S. F., Johnson, K. R., Hunen, J., and Zhang, P.: Seasonality of westerly moisture transport in the East Asian summer monsoon and its implications for interpreting precipitation δ18O, J. Geophys. Res.-Atmos., 120, 5850–5862, 2015. 
Cai, Y., Fung, I. Y., Edwards, R. L., An, Z., Cheng, H., Lee, J.-E., Tan, L., Shen, C.-C., Wang, X., and Day, J. A.: Variability of stalagmite-inferred Indian monsoon precipitation over the past 252,000 y, P. Natl. Acad. Sci. USA, 112, 2954–2959, 2015. 
Cai, Z., Tian, L., and Bowen, G. J.: ENSO variability reflected in precipitation oxygen isotopes across the Asian Summer Monsoon region, Earth Planet. Sc. Lett., 475, 25–33, 2017. 
Cai, Z., Tian, L., and Bowen, G. J.: Spatial-seasonal patterns reveal large-scale atmospheric controls on Asian Monsoon precipitation water isotope ratios, Earth Planet. Sc. Lett., 503, 158–169, 2018. 
Caley, T., Roche, D. M., and Renssen, H.: Orbital Asian summer monsoon dynamics revealed using an isotope-enabled global climate model, Nat. Commun., 5, 5371, https://doi.org/10.1038/ncomms6371, 2014. 
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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.