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| Titel |
Mid-Pliocene East Asian monsoon climate simulated in the PlioMIP |
| VerfasserIn |
R. Zhang, Q. Yan, Z. S. Zhang, D. Jiang, B. L. Otto-Bliesner, A. M. Haywood, D. J. Hill, A. M. Dolan, C. Stepanek, G. Lohmann, C. Contoux, F. Bragg, W.-L. Chan, M. A. Chandler, A. Jost, Y. Kamae, A. Abe-Ouchi, G. Ramstein, N. A. Rosenbloom, L. Sohl, H. Ueda |
| Medientyp |
Artikel
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| Sprache |
Englisch
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| ISSN |
1814-9324
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| Digitales Dokument |
URL |
| Erschienen |
In: Climate of the Past ; 9, no. 5 ; Nr. 9, no. 5 (2013-09-03), S.2085-2099 |
| Datensatznummer |
250085219
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| Publikation (Nr.) |
 copernicus.org/cp-9-2085-2013.pdf |
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| Zusammenfassung |
| Based on simulations with 15 climate models in the Pliocene Model
Intercomparison Project (PlioMIP), the regional climate of East Asia
(focusing on China) during the mid-Pliocene is investigated in this study.
Compared to the pre-industrial, the multi-model ensemble mean (MMM) of all
models shows the East Asian summer winds (EASWs) largely strengthen in
monsoon China, and the East Asian winter winds (EAWWs) strengthen in south
monsoon China but slightly weaken in north monsoon China in the mid-Pliocene.
The MMM of all models also illustrates a warmer and wetter mid-Pliocene
climate in China. The simulated weakened mid-Pliocene EAWWs in north monsoon
China and intensified EASWs in monsoon China agree well with geological
reconstructions. However, there is a large model–model discrepancy in
simulating mid-Pliocene EAWW, which should be further addressed in the
future work of PlioMIP. |
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