Integration of Tibetan Plateau ice-core temperature records and the influence of atmospheric circulation on isotopic signals in the past century

Abstract Temperature signals in ice-core δ 18 O on the Tibetan Plateau (TP), particularly in the central and southern parts, continue to be debated because of the large scale of atmospheric circulation. This study presents ten ice-core δ 18 O records at an annual resolution, with four (Malan, Muztag...

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Bibliographic Details
Published in:Quaternary Research
Main Authors: Yang, Xiaoxin, Yao, Tandong, Joswiak, Daniel, Yao, Ping
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2014
Subjects:
Online Access:http://dx.doi.org/10.1016/j.yqres.2014.01.006
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