PP41C:
Lessons for the Future from Cenozoic Warm Climates Posters


Submit an Abstract to this Session


Session ID#: 49490

Session Description:
During the Cenozoic the Earth’s climate has traversed several warm climates, such as those that are known to have existed during the Eocene, Miocene, Pliocene and the interglacial periods of the Quaternary. Each of these periods provides a unique perspective on warming in the Earth system. Studying these warm climate states helps us to both better understand the range of responses of known mechanisms of global and regional warming, and to also uncover mechanisms and interactions that may not be in operation now but may operate in the future warmer state. We invite submissions that employ numerical modelling to enhance our understanding of the future climate by learning from past warm climates. These could include, but not necessarily restricted to, inferences of climate sensitivity and novel feedback mechanisms, data-model comparison, modelling inferences of the impacts of warm climates on fauna, flora and their influence upon human ancestor dispersal.
Primary Convener:  Deepak Chandan, University of Toronto, Physics, Toronto, ON, Canada
Conveners:  Gilles Ramstein, Laboratoire des Sciences du Climat et de l'Environnement, Gif-Sur-Yvette Cedex, Paris, France, Navjit Sagoo, University of Bristol, Bristol, United Kingdom and Alan M Haywood, University of Leeds, Leeds, United Kingdom
Primary Liaison:  Deepak Chandan, University of Toronto, Physics, Toronto, ON, Canada
Chairs:  Deepak Chandan, University of Toronto, Physics, Toronto, ON, Canada, Gilles Ramstein, Laboratoire des Sciences du Climat et de l'Environnement, Gif-Sur-Yvette Cedex, Paris, France and Alan M Haywood, University of Leeds, Leeds, United Kingdom
OSPA Liaison:  Navjit Sagoo, University of Bristol, Bristol, United Kingdom
Index Terms:

1620 Climate dynamics [GLOBAL CHANGE]
1627 Coupled models of the climate system [GLOBAL CHANGE]
3344 Paleoclimatology [ATMOSPHERIC PROCESSES]
9604 Cenozoic [INFORMATION RELATED TO GEOLOGIC TIME]

Abstracts Submitted to this Session:

Simona Bordoni1, Roberta D'Agostino2, Juergen Bader3 and Johann H Jungclaus2, (1)University of Trento, Trento, Italy, (2)Max Planck Institute for Meteorology, Hamburg, Germany, (3)Max Planck Institute for Meteorology, The Land in the Earth System, Hamburg, Germany
Xin Ren, IEE Institute of Earth Environment, Chinese Academy of Sciences, Xi'an, China
Stephen J Hunter1, Alan M Haywood2, Aisling M Dolan1, Julia Claire Tindall2 and Dr. Harry J Dowsett, PhD3, (1)University of Leeds, Leeds, LS2, United Kingdom, (2)University of Leeds, Leeds, United Kingdom, (3)U.S. Geological Survey, Florence Bascom Geoscience Center, Reston, Virginia, United States
Gregory Walters, University of Cambridge, Department of Earth Sciences, Cambridge, United Kingdom, David A Hodell, University of Cambridge, Godwin Laboratory for Palaeoclimate Research, Department of Earth Sciences, Cambridge, United Kingdom and Simon J Kemp, British Geological Survey Keyworth, Environmental Science Centre, Nottinghamshire, United Kingdom
Dr. Harry J Dowsett, PhD1, Marci M Robinson2, Kevin Foley3 and Whittney Spivey3, (1)USGS, Eastern Geology and Paleoclimate Science Center, Reston, United States, (2)USGS, Florence Bascom Geoscience Center, Reston, United States, (3)USGS, Eastern Geology and Paleoclimate Science Center, Reston, VA, United States
Ran Zhang1, Dabang Jiang1, Gilles Ramstein2, Zhongshi Zhang3, Peter C Lippert4 and Entao Yu1, (1)Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China, (2)Laboratoire des Sciences du Climat et de l'Environnement, Gif-Sur-Yvette Cedex, Paris, France, (3)China University of Geosciences Wuhan, Wuhan, China, (4)Univ of Arizona-Geosciences, Tucson, United States