Little Ice Age climate reconstruction from ensemble reanalysis of Alpine glacier fluctuations
Mountain glaciers sample a combination of climate fields – temperature, precipitation and radiation – by accumulation and melting of ice. Flow dynamics acts as a transfer function that maps volume changes to a length response of the glacier terminus. Long histories of terminus positions have been as...
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Format: | Article in Journal/Newspaper |
Language: | English |
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Copernicus
2014
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Online Access: | https://hdl.handle.net/20.500.11850/93545 https://doi.org/10.3929/ethz-b-000093545 |