Late Glacial mountain glacier culmination in Arctic Norway prior to the Younger Dryas
Climate changes during the Late Glacial period (LG; 15-11 ka) as recorded in Greenland and Antarctic ice cores show a bipolar pattern. Between 14.5 ka and 13 ka ago, the northern latitudes experienced the Bølling/Allerød (BA) warm period, while southern records feature the Antarctic Cold Reversal (A...
Published in: | Quaternary Science Reviews |
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Main Authors: | , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Elsevier
2020
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Subjects: | |
Online Access: | https://hdl.handle.net/11250/2754479 https://doi.org/10.1016/j.quascirev.2020.106461 |