Tropical climate instability: The last glacial cycle from a Qinghai- Tibetan ice core

Science

Volumn 276, Issue 5320, 1997, Pages 1821-1825

  Thompson, L G ^a   Yao, T ^b   Davis, M E ^a   Henderson, K A ^a   Mosley Thompson, E ^a   Lin, P N ^a   Beer, J ^c   Synal, H A ^d   Cole Dai, J ^a   Bolzan, J F ^a  

^a OHIO STATE UNIVERSITY   (United States)

^b Lanzhou Inst Glaciol G   (China)

^c SWISS FEDERAL INSTITUTE OF AQUATIC SCIENCE AND TECHNOLOGY   (Switzerland)

^d PAUL SCHERRER INSTITUTE   (Switzerland)

Author keywords

[No Author keywords available]

Indexed keywords

ICE;

GLACIAL CYCLE; ICE CORE RECORD; LAST GLACIAL; PALAEOCLIMATE; TROPICAL CLIMATE;

ARTICLE; CHINA; COLD CLIMATE; ENVIRONMENTAL FACTOR; PRIORITY JOURNAL; TROPIC CLIMATE;

CHINA, QINGHAI PROVINCE; CHINA, TIBETAN PLATEAU;

EID: 0030847781     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.276.5320.1821     Document Type: Article

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65. We thank the many scientists, engineers, technicians and graduate students from the Byrd Polar Research Center and the Lanzhou Institute of Glaciology and Geocryology (China). Special thanks are extended to B. Koci, lead ice core driller; and to V. Mikhalenko, B. Barber, and W. Tamayo Alegre for field assistance. This work was supported by NSF's Office of Climate Dynamics and the Division of Polar Programs (grants ATM-8519794, ATM-89116635, and DPP-9014931), the National Geographic Society (grants 3323-86, 4309-90, and 4522-91), Ohio State University, and the State Committee of Science and Technology and the National Natural Science Foundation of China. This is contribution 1051 of the Byrd Polar Research Center.