• The hydrological cycle and ocean circulation of the Maritime Continent in the Pliocene: results from PlioMIP2 

      Ren, Xin; Lunt, Daniel J.; Hendy, Erica; Von Der Heydt, Anna; Abe-Ouchi, Ayako; Otto-Bliesner, Bette; Williams, Charles J. R.; Stepanek, Christian; Guo, Chuncheng; Chandan, Deepak; Lohmann, Gerrit; Tindall, Julia C.; Sohl, Linda E.; Chandler, Mark A.; Kageyama, Masa; Baatsen, Michiel L. J.; Tan, Ning; Zhang, Qiong; Feng, Ran; Hunter, Stephen; Chan, Wing-Le; Peltier, W. Richard; Li, Xiangyu; Kamae, Youichi; Zhang, Zhongshi; Haywood, Alan M. (Journal article; Peer reviewed, 2023)
      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 ...