Fast and slow components of interstadial warming in the North Atlantic during the last glacial

Interstadial North Atlantic warming during the last glacial period involved the operation of both fast and slow components of the coupled atmosphere–ocean–sea-ice system, according to analyses from the Portuguese Margin and climate model simulations.

Bibliographic Details
Published in:Communications Earth & Environment
Main Authors: Vasiliki Margari, Luke C. Skinner, Laurie Menviel, Emilie Capron, Rachael H. Rhodes, Maryline J. Mleneck-Vautravers, Mohamed M. Ezat, Belen Martrat, Joan O. Grimalt, David A. Hodell, Polychronis C. Tzedakis
Format: Article in Journal/Newspaper
Language:English
Published: Nature Portfolio 2020
Subjects:
envir
geo
North Atlantic
Sea ice
Online Access:https://doi.org/10.1038/s43247-020-0006-x
https://doaj.org/article/9bf04e66bc204733b65255d4e3dc8bcc
Description
Summary:Interstadial North Atlantic warming during the last glacial period involved the operation of both fast and slow components of the coupled atmosphere–ocean–sea-ice system, according to analyses from the Portuguese Margin and climate model simulations.

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