δ 18O record and temperature change over the past 100 years in ice cores on the Tibetan Plateau

Author:

Yao Tandong,Guo Xuejun,Thompson Lonnie,Duan Keqin,Wang Ninglian,Pu Jianchen,Xu Baiqing,Yang Xiaoxin,Sun Weizhen

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Reference23 articles.

1. Wang, S. H. W., Gong, D. Y., Chinese temperature in several special periods during Holocene, Natural Science Progress (in Chinese), 2000, 10(4): 325–332.

2. Yang, B., Braeuning, A., Johnson, K. et al., General characteristics of temperature variation in China during the last two millennia, J. Geophys. Res., 2002, 29(9): 381–384.

3. Shi, Y. F., Yao, T. D., Yang, B., Climate change of the past 2000a in 10a time scale from Guliya Ice core and its comparison with historical record in East China, Science in China, Series D (in Chinese), 1999, 42(suppl.): 91–100.

4. Wang, SH.W., Ye, J.L., Gong, D.Y et al., Establishment of Chinese temperature series in the past centuries, Newsletter of Applied Meteorology (in Chinese), 1998, 9(4): 391–401.

5. Wang, N. L., Thompson, L. G., Davis, M. E. et al., Influence of variations in NAO and SO on air temperature over the northern Tibetan Plateau as recorded by δ 18O in the Malan ice core, Geophysical Research Letters, 2003, 30(22): 2167–2172.

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