Dynamical response of the southwestern Laurentide Ice Sheet to rapid Bølling–Allerød warming

Dynamical response of the southwestern Laurentide Ice Sheet to rapid Bølling–Allerød warming

<p>The shift in climate that occurred between the Last Glacial Maximum (LGM) and the Early Holocene (ca. 18–12 kyr BP) displayed rates of temperature increase similar to present-day warming trends. The most rapid recorded changes in temperature occurred during the abrupt climate oscillations k...

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Bibliographic Details
Main Authors: S. L. Norris, M. Margold, D. J. A. Evans, N. Atkinson, D. G. Froese
Format: Article
Language:English
Published: Copernicus Publications 2024-04-01
Series:The Cryosphere
Online Access:https://tc.copernicus.org/articles/18/1533/2024/tc-18-1533-2024.pdf

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