A Quaternary history of ice sheet dynamics in the Transantarctic Mountains.
The Antarctic Ice Sheets responded significantly to climatic conditions during the Last Glacial Maximum (LGM) and the subsequent warming that followed. Therefore, an understanding of how Antarctica reacted to past climates is necessary to predict the response of its ice sheets to current and future...
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Format: | Article in Journal/Newspaper |
Language: | English |
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University of Canterbury. Department of Geological Sciences / Gateway Antarctica
2013
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Online Access: | https://dx.doi.org/10.26021/5789 https://ir.canterbury.ac.nz/handle/10092/8726 |