Abstract
A simplification and synthesis of late-Würm Northern Hemisphere glaciation is possible by postulating an Arctic Ice Sheet that behaved as a single dynamic system.
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Hughes, T., Denton, G. & Grosswald, M. Was there a late-Würm Arctic Ice Sheet?. Nature 266, 596–602 (1977). https://doi.org/10.1038/266596a0
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DOI: https://doi.org/10.1038/266596a0
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