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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Bibliographic Details
Main Author: Lüthi, Martin P.
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus 2014
Subjects:
Ela
Online Access:https://hdl.handle.net/20.500.11850/93545
https://doi.org/10.3929/ethz-b-000093545