What controls precipitation δ18O in the southern Tibetan Plateau at seasonal and intra-seasonal scales? A case study at Lhasa and Nyalam-Reference-Cited by-同舟云学术

What controls precipitation δ18O in the southern Tibetan Plateau at seasonal and intra-seasonal scales? A case study at Lhasa and Nyalam

Published:2013-10-31 Issue:1 Volume:65 Page:21043
ISSN:1600-0889
Container-title:Tellus B: Chemical and Physical Meteorology
language:en
Short-container-title:Tellus B: Chemical and Physical Meteorology

Author:

Gao Jing¹²,Masson-Delmotte Valerie³,Risi Camille⁴,He You¹²,Yao Tandong¹²

Affiliation:

1. Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China

2. State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environment and Engineering Research Institute, Chinese Academy Sciences, Beijing, China

3. LSCE, UMR 8212 CEA/CNRS/UVSQ – IPSL, Gif-sur-Yvette, France

4. LMD/IPSL, CNRS, UPMC, Paris, France

Publisher

Informa UK Limited

Subject

Atmospheric Science

Link

https://www.tandfonline.com/doi/pdf/10.3402/tellusb.v65i0.21043

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3. Climatic and atmospheric circulation pattern variability from ice-core isotope/geochemistry records (Altai, Tien Shan and Tibet)