Uncertainties originating from GCM downscaling and bias correction with application to the MIS-11c Greenland Ice Sheet

<p>The Marine Isotope Stage 11c (MIS-11c) interglacial is an enigmatic period characterized by a long duration of relatively weak insolation forcing, but it is thought to have been coincident with a large global sea-level rise of 6–13 m. The configuration of the Greenland Ice Sheet during the...

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Bibliographic Details
Main Authors: B. R. Crow, L. Tarasov, M. Schulz, M. Prange
Format: Article
Language:English
Published: Copernicus Publications 2024-02-01
Series:Climate of the Past
Online Access:https://cp.copernicus.org/articles/20/281/2024/cp-20-281-2024.pdf