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 p CO 2 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 variabilit...
Published in: | Climate of the Past |
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Main Authors: | , , , , , , |
Format: | Text |
Language: | English |
Published: |
2020
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Subjects: | |
Online Access: | https://doi.org/10.5194/cp-16-1-2020 https://cp.copernicus.org/articles/16/1/2020/ |