Hummock corridors in the south‐central sector of the Fennoscandian ice sheet, morphometry and pattern
Abstract Subglacial conditions strongly influence the flow of ice‐sheets, in part due to the availability of melt water. Contemporary ice sheets are retreating and are affected by increased melting as climate warms. The south Swedish uplands (SSU) were deglaciated during the relatively warm Bølling‐...
Published in: | Earth Surface Processes and Landforms |
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Main Authors: | , |
Other Authors: | |
Format: | Article in Journal/Newspaper |
Language: | English |
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Wiley
2017
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Online Access: | http://dx.doi.org/10.1002/esp.4294 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fesp.4294 https://onlinelibrary.wiley.com/doi/pdf/10.1002/esp.4294 https://onlinelibrary.wiley.com/doi/full-xml/10.1002/esp.4294 |