Application of a distributed degree-day model of glaciers in the upper reaches of the Beida River Basin-Reference-Cited by-同舟云学术

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Application of a distributed degree-day model of glaciers in the upper reaches of the Beida River Basin

Published:2016-03 Issue:6 Volume:75 Page:
ISSN:1866-6280
Container-title:Environmental Earth Sciences
language:en
Short-container-title:Environ Earth Sci

Author:

Wang Sheng,Wang Jinfeng,Pu Jianchen

Funder

the National Natural Science Foundation of China

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/s12665-015-4973-7.pdf

Reference66 articles.

1. Arnold NS, Willis IC, Sharp MJ et al (1996) A distributed surface energy-balance model for a small valley glacier. I. Development and testing for Haut Glacier d’Arolla, Valais, Switzerland. J Glaciol 42:77–89

2. Barnett TP, Adam JC, Lettenmaier DP (2005) Potential impacts of a warming climate on water availability in snow-dominated regions. Nature 438:303–309. doi: 10.1038/nature04141

3. Bassford RP, Siegert MJ, Dowdeswell JA (2006) Quantifying the mass balance of ice caps on Severnaya Zemlya, Russian High Arctic III: sensitivity of ice caps in Severnaya Zemlya to future climate change. Arct Antarct Alp Res 38:21–33. doi:10.1657/1523-0430(2006)038[0021:QTMBOI]2.0.CO;2

4. Braithwaite RJ (1984) Can the mass balance of a glacier be estimated from its equilibrium line altitude? J Glaciol 30:364–368

5. Braithwaite RJ, Olesen OB (1993) Seasonal variation of ice ablation at the margin of the Greenland ice sheet and its sensitivity to climate change, Qamanârssûp, West Greenland. J Glaciol 39:267–274

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