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TC | Articles | Volume 13, issue 6
The Cryosphere, 13, 1743–1752, 2019
https://doi.org/10.5194/tc-13-1743-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
The Cryosphere, 13, 1743–1752, 2019
https://doi.org/10.5194/tc-13-1743-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 28 Jun 2019

Research article | 28 Jun 2019

Apparent discrepancy of Tibetan ice core δ18O records may be attributed to misinterpretation of chronology

Shugui Hou et al.

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Cited articles

An, W., Hou, S., Zhang, W., Wu, S., Xu, H., Pang, H., Wang, Y., and Liu, Y.: Possible recent warming hiatus on the northwestern Tibetan Plateau derived from ice core records, Sci. Rep., 6, 32813, https://doi.org/10.1038/srep32813, 2016. 
Beniston, M., Diaz, H. F., and Bradley, R. S.: Climatic change at high elevation sites: an overview, Clim. Change, 36, 233–251, https://doi.org/10.1023/A:1005380714349, 1997. 
Bolzan, J.: Ice flow at the Dome C ice divide based on a deep temperature profile, J. Geophys. Res., 90, 8111–8124, 1985. 
Cheng, H., Zhang, P., Spötl, C., Edwards, R., Cai, Y., Zhang, D., Sang, W., Tan, M., and An, Z.: The climatic cyclicity in semiarid-arid central Asia over the past 500,000 years, Geophys. Res. Lett. 39, L01705, https://doi.org/10.1029/2011gl050202, 2012. 
Publications Copernicus
Short summary
The apparent discrepancy between the Holocene δ18O records of the Guliya and the Chongce ice cores may be attributed to a possible misinterpretation of the Guliya ice core chronology.
The apparent discrepancy between the Holocene δ18O records of the Guliya and the Chongce ice...
Citation