Advances in Earth Science ›› 2006, Vol. 21 ›› Issue (12): 1314-1323. doi: 10.11867/j.issn.1001-8166.2006.12.1314

Special Issue: 青藏高原研究——青藏科考虚拟专刊

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Advances in the Study of Stable Oxygen Isotope in Precipitation on the Tibetan Plateau

Yu Wusheng 1,2,Tian Lide 1,2,Ma Yaoming 1,2,Yin Changliang 2
  

  1. 1.Laboratory of Environment and Process on Tibetan Plateau,Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100085,China;2.Key Laboratory of Cryosphere and Environment,Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences,Lanzhou 730000,China
  • Received:2006-10-11 Revised:2006-10-31 Online:2006-12-15 Published:2006-12-15

Yu Wusheng,Tian Lide,Ma Yaoming,Yin Changliang. Advances in the Study of Stable Oxygen Isotope in Precipitation on the Tibetan Plateau[J]. Advances in Earth Science, 2006, 21(12): 1314-1323.

Stable oxygen isotope(δ18O)in ice core records is good proxy for temperature record and is representative of climatic change. The study of the δ18O variation in precipitation can throw light on the climatic significance of δ18O records in ice core. This paper reviews the advances in the study of stable oxygen isotope in precipitation in the monsoon region,the non-monsoon region,and the transition region between the monsoon region and the non-monsoon region on the Tibetan Plateau,respectively. Moreover,an outlook on future research over the Tibetan Plateau is presented in this paper.

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