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...
Published in: | Quaternary Research |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Cambridge University Press (CUP)
2014
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Subjects: | |
Online Access: | http://dx.doi.org/10.1016/j.yqres.2014.01.006 http://api.elsevier.com/content/article/PII:S003358941400009X?httpAccept=text/xml http://api.elsevier.com/content/article/PII:S003358941400009X?httpAccept=text/plain https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400001186 |