Equilibrium line altitudes of alpine glaciers in Alaska suggest Last Glacial Maximum summer temperature was 2–5 °C lower than during the pre-industrial

The lack of continental ice sheets in Alaska during the Last Glacial Maximum (LGM; 26–19 ka) has long been attributed to extensive aridity in the western Arctic. More recently, climate model outputs, a few isolated paleoclimate studies, and global paleoclimate synthesis products show mild summer tem...

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Bibliographic Details
Published in:Climate of the Past
Main Authors: Walcott, Caleb K., Briner, Jason P., Tulenko, Joseph P., Evans, Stuart M.
Format: Text
Language:English
Published: 2024
Subjects:
Online Access:https://doi.org/10.5194/cp-20-91-2024
https://cp.copernicus.org/articles/20/91/2024/