Modeling a modern-like pCO2 warm period (Marine Isotope Stage KM5c) with two versions of an Institut Pierre Simon Laplace atmosphere–ocean coupled general circulation model

The mid-Piacenzian warm period (3.264 to 3.025 Ma) is the most recent geological period with present-like atmospheric pCO2 and is thus expected to have exhibited a warm climate similar to or warmer than the present day. On the basis of understanding that has been gathered on the climate variability...

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Bibliographic Details
Published in:Climate of the Past
Main Authors: Tan, Ning, Contoux, Camille, Ramstein, Gilles, Sun, Yong, Dumas, Christophe, Sepulchre, Pierre, Guo, Zhengtang
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2020
Subjects:
article
Verlagsveröffentlichung
Greenland
Laplace
Ice Sheet
Sea ice
Online Access:https://doi.org/10.5194/cp-16-1-2020
https://noa.gwlb.de/receive/cop_mods_00049984
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00049601/cp-16-1-2020.pdf
https://cp.copernicus.org/articles/16/1/2020/cp-16-1-2020.pdf

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