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David Hutchinson is a Research Fellow at the University of New South Wales, where he specializes in paleoclimate modeling, particularly focusing on past warm climate intervals during the Eocene, Oligocene, and Miocene periods. His research involves investigating the long-term evolution of deep ocean circulation and its implications for climate change. Hutchinson has developed simulations of the Eocene-Oligocene transition using the coupled climate model GFDL CM2.1 and is currently extending research into new intervals of the Oligocene and Miocene. He is undertaking an ARC DECRA fellowship from 2022 to 2025, examining how changes in ocean circulation have impacted the Antarctic ice sheet. Additionally, he has experience as a long-term visitor at the Australian National University, being part of the Climate Fluid Physics group.
University of New South Wales • Sydney, Australia
Conducting research in paleoclimate modeling and coordinating climate change studies.
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