Dynamics of the cold surface layer of polythermal Storglaciären, Sweden
Polythermal glaciers, i.e. glaciers with a combination of ice at and below the freezing point, are widespread in arctic and subarctic environments. The polythermal structure has major implications for glacier hydrology, ice flow and glacial erosion. However, the interplay of factors governing its sp...
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Format: | Doctoral Thesis |
Language: | English |
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Stockholms universitet, Institutionen för naturgeografi och kvartärgeologi
2004
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Online Access: | http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-161 http://nbn-resolving.de/urn:isbn:91-7265-907-6 |