Evolutions of water stable isotopes and the contributions of cryosphere to the alpine river on the Tibetan Plateau-Reference-Cited by-同舟云学术

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Evolutions of water stable isotopes and the contributions of cryosphere to the alpine river on the Tibetan Plateau

Published:2015-12-21 Issue:1 Volume:75 Page:
ISSN:1866-6280
Container-title:Environmental Earth Sciences
language:en
Short-container-title:Environ Earth Sci

Author:

Yang Yuzhong,Wu Qingbai,Jin Huijun

Funder

Chinese Academy of Sciences Key Research Program

Research Fund of State Key Laboratory of Frozen Soils Engineering

Publisher

Springer Science and Business Media LLC

Subject

Earth-Surface Processes,Geology,Pollution,Soil Science,Water Science and Technology,Environmental Chemistry,Global and Planetary Change

Link

http://link.springer.com/content/pdf/10.1007/s12665-015-4894-5.pdf

Reference62 articles.

1. Buttle J (1994) Isotope hydrograph separations and rapid delivery of pre-event water from drainage basins. Prog Phys Geogr 18(1):16–41

2. Cable J, Ogle K, Williams D (2011) Contribution of glacier meltwater to streamflow in the Wind River Range, Wyoming, inferred via a Bayesian mixing model applied to isotopic measurements. Hydrol Process 25:2228–2236

3. Cheng GD, Jin HJ (2013) Permafrost and groundwater on the Qinghai-Tibet Plateau and in northeast China. Hydrogeol J 21(1):5–23

4. Craig H (1961) Isotopic variations in meteoric waters. Science 133(3465):1702–1703

5. Cui BL, Li XY (2015) Characteristics of stable isotopes and hydrochemistry of river water in the Qinghai Lake Basin, northeast Qinghai-Tibet Plateau, China. Environ Earth Sci 73(8):4251–4263

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