Institute of International Rivers and Eco-security, Yunnan Key Laboratory of International Rivers and Transboundary Eco-security, State Key Laboratory of Vegetation Structure, Function and Construction (VegLab), Yunnan University, Kunming, 650500, China
Rong Li
Institute of International Rivers and Eco-security, Yunnan Key Laboratory of International Rivers and Transboundary Eco-security, State Key Laboratory of Vegetation Structure, Function and Construction (VegLab), Yunnan University, Kunming, 650500, China
Cheng Wang
Institute of International Rivers and Eco-security, Yunnan Key Laboratory of International Rivers and Transboundary Eco-security, State Key Laboratory of Vegetation Structure, Function and Construction (VegLab), Yunnan University, Kunming, 650500, China
Qiukai Mao
Institute of International Rivers and Eco-security, Yunnan Key Laboratory of International Rivers and Transboundary Eco-security, State Key Laboratory of Vegetation Structure, Function and Construction (VegLab), Yunnan University, Kunming, 650500, China
Institute of International Rivers and Eco-security, Yunnan Key Laboratory of International Rivers and Transboundary Eco-security, State Key Laboratory of Vegetation Structure, Function and Construction (VegLab), Yunnan University, Kunming, 650500, China
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3,506
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4,780
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221
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XML: 140
Total: 4,780
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BibTeX: 133
EndNote: 221
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Total article views: 2,260 (including HTML, PDF, and XML)
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1,348
842
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2,260
178
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PDF: 842
XML: 70
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Supplement: 178
BibTeX: 51
EndNote: 82
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2,158
292
70
2,520
332
82
139
HTML: 2,158
PDF: 292
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Total: 2,520
Supplement: 332
BibTeX: 82
EndNote: 139
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Total article views: 4,780 (including HTML, PDF, and XML)
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Total article views: 2,260 (including HTML, PDF, and XML)
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Total article views: 2,520 (including HTML, PDF, and XML)
Thereof 2,520 with geography defined
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Local and upstream specific humidity is the main factor determining non-monsoon season d-excess variability over southeast Tibetan Plateau (TP) due to the intrusion of cold and dry air from upper levels. During the summer monsoon season, d-excess and δ18O mainly reflect the effect of raindrop evaporation which leads to lower vapor δ18O but higher d-excess values. These findings provide new insights into using water isotopes to track moisture sources and dynamics over the TP.
Local and upstream specific humidity is the main factor determining non-monsoon season d-excess...