Quantifying the role of geographic change in Cenozoic ocean heat transport using uncoupled atmosphere and ocean models
Abstract A series of five Cenozoic atmospheric general circulation model (AGCM) experiments has been performed using a new set of paleogeographic reconstructions for 55, 40, 33, 20 and 14 Ma. The five continental reconstructions incorporate the tectonic evolution of early Eocene to middle Miocene continental positions and topography. With all other model boundary conditions and forcings held constant, the series of AGCM experiments captures a