What controls precipitation δ18O in the southern Tibetan Plateau at seasonal and intra-seasonal scales? A case study at Lhasa and Nyalam
By: Jing Gao, Valerie Masson-Delmotte, Camille Risi, You He and Tandong Yao
Authors
Jing Gao
Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, CN; State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environment and Engineering Research Institute, Chinese Academy Sciences
You He
Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, CN; State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environment and Engineering Research Institute, Chinese Academy Sciences
Tandong Yao
Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, CN; State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environment and Engineering Research Institute, Chinese Academy Sciences
DOI: https://doi.org/10.3402/tellusb.v65i0.21043 | Journal eISSN: 1600-0889
Language: English
Page range: 21043 - 21043
Submitted on: Apr 4, 2013
Accepted on: Sep 6, 2013
Published on: Jan 1, 2013
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 2013 Jing Gao, Valerie Masson-Delmotte, Camille Risi, You He, Tandong Yao, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.