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 Publications 2014
Subjects:
Ela
Online Access:https://www.zora.uzh.ch/id/eprint/101706/
https://www.zora.uzh.ch/id/eprint/101706/1/2014%20L%C3%BCthiM_tc-8-639-2014%20.pdf
https://doi.org/10.5167/uzh-101706
https://doi.org/10.5194/tc-8-639-2014