The hydrological cycle and ocean circulation of the Maritime Continent in the Pliocene: results from PlioMIP2
<p>The Maritime Continent (MC) forms the western boundary of the tropical Pacific Ocean, and relatively small changes in this region can impact the climate locally and remotely. In the mid-Piacenzian warm period of the Pliocene (mPWP; 3.264 to 3.025 Ma) atmospheric CO<span class="inlin...
Main Authors: | , , , , , , , , , , , , , , , , , , , , , , , , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2023-10-01
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Series: | Climate of the Past |
Online Access: | https://cp.copernicus.org/articles/19/2053/2023/cp-19-2053-2023.pdf |