Author
Listed:
- Ulrich Salzmann
(Faculty of Engineering and Environment, Northumbria University)
- Aisling M. Dolan
(School of Earth and Environment, University of Leeds)
- Alan M. Haywood
(School of Earth and Environment, University of Leeds)
- Wing-Le Chan
(Atmosphere and Ocean Research Institute, University of Tokyo)
- Jochen Voss
(School of Mathematics, University of Leeds)
- Daniel J. Hill
(British Geological Survey, Keyworth)
- Ayako Abe-Ouchi
(Atmosphere and Ocean Research Institute, University of Tokyo
Japan Agency for Marine-Earth Science and Technology)
- Bette Otto-Bliesner
(National Center for Atmospheric Research)
- Frances J. Bragg
(School of Geographical Sciences, University of Bristol)
- Mark A. Chandler
(Columbia University—NASA/GISS)
- Camille Contoux
(LSCE/IPSL, CNRS-CEA-UVSQ
Sisyphe, CNRS/UPMC Univ Paris 06)
- Harry J. Dowsett
(Eastern Geology and Paleoclimate Science Center, US Geological Survey)
- Anne Jost
(Sisyphe, CNRS/UPMC Univ Paris 06)
- Youichi Kamae
(Graduate School of Life and Environmental Sciences, University of Tsukuba)
- Gerrit Lohmann
(Alfred Wegener Institute for Polar and Marine Research)
- Daniel J. Lunt
(School of Geographical Sciences, University of Bristol)
- Steven J. Pickering
(School of Earth and Environment, University of Leeds)
- Matthew J. Pound
(Faculty of Engineering and Environment, Northumbria University)
- Gilles Ramstein
(LSCE/IPSL, CNRS-CEA-UVSQ)
- Nan A. Rosenbloom
(National Center for Atmospheric Research)
- Linda Sohl
(Columbia University—NASA/GISS)
- Christian Stepanek
(Alfred Wegener Institute for Polar and Marine Research)
- Hiroaki Ueda
(Graduate School of Life and Environmental Sciences, University of Tsukuba)
- Zhongshi Zhang
(Institute of Atmospheric Physics, Chinese Academy of Sciences
Bjerknes Centre for Climate Research)
Abstract
A global data set of proxy-based temperature estimates and biome reconstructions is used to assess the ability of eight climate models to simulate the warm environments of the Pliocene. Model results show a substantial cold bias in the Northern Hemisphere. Sensitivity tests identify temporal variability, the temperature difference over the proxy time range, as an important factor in model–data discrepancies, indicating that future comparisons should focus on time slices with the same orbital forcing
Suggested Citation
Ulrich Salzmann & Aisling M. Dolan & Alan M. Haywood & Wing-Le Chan & Jochen Voss & Daniel J. Hill & Ayako Abe-Ouchi & Bette Otto-Bliesner & Frances J. Bragg & Mark A. Chandler & Camille Contoux & Har, 2013.
"Challenges in quantifying Pliocene terrestrial warming revealed by data–model discord,"
Nature Climate Change, Nature, vol. 3(11), pages 969-974, November.
Handle:
RePEc:nat:natcli:v:3:y:2013:i:11:d:10.1038_nclimate2008
DOI: 10.1038/nclimate2008
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