Authors: Sathyanadh, Anusha, Monteil, Guillaume, Scholze, Marko, Klosterhalfen, Anne, Laudon, Hjalmar, Wu, Zhendong, Gerbig, Christoph, Peters, Wouter, Bastrikov, Vladislav, Nilsson, Mats, B, Peichl, Matthias, Oldeman, Arthur, M, Baatsen, Michiel, L J, von Der Heydt, Anna, S, Dijkstra, Henk, A, Tindall, Julia, C, Abe-Ouchi, Ayako, Booth, Alice, R, Brady, Esther, Chan, Wing-Le, Chandan, Deepak, Chandler, Mark, Contoux, Camille, Feng, Ran, Guo, Chuncheng, Haywood, Alan, Hunter, Stephen, J, Kamae, Youichi, Li, Qiang, Xiangyu, Lohmann, Gerrit, Lunt, Daniel, Nisancioglu, Kerim, H, Otto-Bliesner, Bette, L, Peltier, W, Richard, Pontes, Gabriel, Ramstein, Gilles, Sohl, Linda, E, Stepanek, Christian, Tan, Ning, Zhang, Qiong, Zhongshi, Wainer, Ilana, Williams, Charles, J R
Venue: N/A
Type: Publication
Abstract: The mid-Pliocene warm period (3.264–3.025 Ma) is the most recent geological period during which atmospheric CO2 levels were similar to recent historical values (∼400 ppm). Several proxy reconstructions for the mid-Pliocene show highly reduced zonal sea surface temperature (SST) gradients in the tropical Pacific Ocean, indicating an El Niño-like mean state. However, past modelling studies do not show these highly reduced gradients. Efforts to understand mid-Pliocene climate dynamics have led to the Pliocene Model Intercomparison Project (Pl...
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DOI:
10.5194/cp-17-2427-2021
(Found 2 versions)
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