National Ice Core Laboratory Science Management Office
Dunde Publications
Tandong, Y., L. Zexia, L.G. Thompson, E. Mosley-Thompson, Y. Wang, L. Tian, N. Wang, and K. Duan. 2006. Delta-O18 records from Tibetan ce cores reveal differences in climatic changes. Annal of Glaciology, 43.
Thompson, L.G., M.E. Davis, E. Mosley-Thompson, P.-N. Lin, K.A. Henderson, and T.A. Mashiotta. 2005. Tropical ice core records: evidence for asynchronous glaciation on Milankovitch timescales. Journal of Quaternary Science, 20(7-8), 723-733.
Thompson, L.G., E. Mosley-Thompson, M. Davis, J. Bolzan, J. Dai, N. Gundestrup, T. Yao, X. Wu and Z. Xie. 1989. Holocene-Late Wisconsin Pleistocene climatic ice core records from Qinghai-Tibetan Plateau. Science, 246(4929), 474-477.
Thompson, L.G., E. Mosley-Thompson and 8 others. 1990. Glacial stage ice-core records from the subtropical Dunde ice cap, China. Annals of Glaciology, 14, 288-297.
Thompson, L.G., E. Mosley-Thompson and five others. 1993. "Recent warming": ice core evidence from tropical ice cores with emphasis upon Central Asia. Global and Planetary Change Section, 7, 145-156.
Feng, Z., L.G. Thompson, E. Mosley-Thompson, J. Dai, M.E. Davis and P.N. Lin. 1993. Temporal and spatial variations of climate in China during the past 10,000 years. The Holocene, 3(2), 174-180.
Lin, P.N., L.G. Thompson, M.E. Davis and E. Mosley-Thompson. 1995. 1000 years of climatic change in China: Ice core 18OO evidence. Annals of Glaciology, 21, 189-195.
** If you know of any additional publications please send them to us at nicl.smo@unh.edu.
National Ice Core Laboratory Science Management Office
National Ice Core Laboratory-Science Management Office (NICL-SMO)
Climate Change Research Center, Institute for the Study of Earth, Oceans, and Space, University of New Hampshire
8 College Road, Durham, New Hampshire 03824, USA Tel: (603) 862-1991, Fax: (603) 862-2124, Email: nicl.smo at unh.edu
This material is based upon work supported by the National Science Foundation under Grant No. ANT-0635515. Any opinions, findings, and conclusions or recommendations expressed in this material are those of the author(s) and do not necessarily reflect the views of the National Science Foundation.
