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="inline-formula"><su...

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Hlavní autoři:	X. Ren, D. J. Lunt, E. Hendy, A. von der Heydt, A. Abe-Ouchi, B. Otto-Bliesner, C. J. R. Williams, C. Stepanek, C. Guo, D. Chandan, G. Lohmann, J. C. Tindall, L. E. Sohl, M. A. Chandler, M. Kageyama, M. L. J. Baatsen, N. Tan, Q. Zhang, R. Feng, S. Hunter, W.-L. Chan, W. R. Peltier, X. Li, Y. Kamae, Z. Zhang, A. M. Haywood
Médium:	Artigo
Jazyk:	Inglês
Vydáno:	Copernicus Publications 2023-10-01
Edice:	Climate of the Past
On-line přístup:	https://cp.copernicus.org/articles/19/2053/2023/cp-19-2053-2023.pdf
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