The current disequilibrium of North Cascade glaciers
Abstract Three lines of evidence indicate that North Cascade (Washington, USA) glaciers are currently in a state of disequilibrium. First, annual balance measured on nine glaciers yields a mean cumulative balance for the 1984–2004 period of −8·58 m water equivalent (w.e.), a net loss of ice thicknes...
Published in: | Hydrological Processes |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Wiley
2006
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Online Access: | http://dx.doi.org/10.1002/hyp.6132 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fhyp.6132 https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.6132 |