Twentieth-century glacier change at Svartisen, Norway: the influence of climate, glacier geometry and glacier dynamics
In the 1870s and 1880s, after a long period of cold conditions, most of the glaciers of Svartisen ended near their maximum Neoglacial limit. Subsequent changes, although principally a response to the climatic controls of mass balance, have been influenced by glacier geometry, including area/altitude...
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| Format: | Article in Journal/Newspaper |
| Language: | English |
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1990
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| Online Access: | https://research.manchester.ac.uk/en/publications/bd803303-f13a-4a80-94c9-ee4530023614 |