A reconciled solution of Meltwater Pulse 1A sources using sea-level fingerprinting
Yucheng Lin, Fiona D. Hibbert, Pippa L. Whitehouse and 4 more
Nature Communications · 2021
doi:10.1038/s41467-021-21990-y (opens in a new tab)
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Abstract
Meltwater Pulse 1A was the most rapid global sea-level rise event during the last deglaciation, but the source of the freshwater causing this rise is debated. Here, the authors use a data-driven inversion approach to show that the North American and Eurasian Ice Sheets were the dominant contributors.
Abstract licence: CC BY-NC-ND
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