Articles | Volume 14, issue 6
https://doi.org/10.5194/cp-14-789-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-14-789-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Climate sensitivity and meridional overturning circulation in the late Eocene using GFDL CM2.1
David K. Hutchinson
CORRESPONDING AUTHOR
Department of Geological Sciences, Stockholm University, 10691
Stockholm, Sweden
Agatha M. de Boer
Department of Geological Sciences, Stockholm University, 10691
Stockholm, Sweden
Helen K. Coxall
Department of Geological Sciences, Stockholm University, 10691
Stockholm, Sweden
Rodrigo Caballero
Department of Meteorology, Stockholm University, 10691 Stockholm,
Sweden
Johan Nilsson
Department of Meteorology, Stockholm University, 10691 Stockholm,
Sweden
Michiel Baatsen
IMAU, Utrecht University, Princetonplein 5, 3584CC Utrecht, the
Netherlands
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Discussed (final revised paper)
Latest update: 20 Nov 2024
Short summary
The Eocene--Oligocene transition was a major cooling event 34 million years ago. Climate model studies of this transition have used low ocean resolution or topography that roughly approximates the time period. We present a new climate model simulation of the late Eocene, with higher ocean resolution and topography which is accurately designed for this time period. These features improve the ocean circulation and gateways which are thought to be important for this climate transition.
The Eocene--Oligocene transition was a major cooling event 34 million years ago. Climate model...