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Climate of the Past An interactive open-access journal of the European Geosciences Union
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Volume 12, issue 11
Clim. Past, 12, 2077–2085, 2016
https://doi.org/10.5194/cp-12-2077-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
Clim. Past, 12, 2077–2085, 2016
https://doi.org/10.5194/cp-12-2077-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 16 Nov 2016

Research article | 16 Nov 2016

Modeling precipitation δ18O variability in East Asia since the Last Glacial Maximum: temperature and amount effects across different timescales

Xinyu Wen et al.

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Cited articles

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Chu, P. C., Li, H.-C., Fan, C., and Chen, Y.-H.: Speleothem evidence for temporal–spatial variation in the East Asian Summer Monsoon since the Medieval Warm Period, J. Quaternary Sci., 27, 901–910, https://doi.org/10.1002/jqs.2579, 2012.
Cuffey, K. M., Clow, G. D., Alley, R. B., Stuiver, M., Waddington, E. D., and Saltus, R. W.: Large Arctic Temperature Change at the Wisconsin-Holocene Glacial Transition, Science, 270, 455–458, 1995.
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Davis, M. E. and Thompson, L. G.: Four Centuries of Climatic Variation Across the Tibetan Plateau from Ice-Core Accumulation and δ18O Records, in: Earth Paleoenvironments: Records Preserved in Mid-and Low-Latitude Glaciers, edited by: Cecil, L. D., Green, J. R., and Thompson, L. G., Springer, 145–161, 2004.
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In this paper, we challenge the usefulness of temperature effect and amount effect, the basic assumptions in past climate reconstruction using a stable water isotope proxy, in East Asia on multiple timescales. By modeling several time slices in the past 22 000 years using an isotope-enabled general circulation model, we suggest great caution when interpreting δ18O records in this area as indicators of surface temperature and/or local monsoonal precipitation, especially on a millennial timescale.
In this paper, we challenge the usefulness of temperature effect and amount effect, the basic...
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