Articles | Volume 12, issue 5
https://doi.org/10.5194/cp-12-1181-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-12-1181-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Palaeogeographic controls on climate and proxy interpretation
School of Geographical Sciences, and Cabot Institute, University of
Bristol, Bristol, BS8 1SS, UK
Alex Farnsworth
School of Geographical Sciences, and Cabot Institute, University of
Bristol, Bristol, BS8 1SS, UK
Claire Loptson
School of Geographical Sciences, and Cabot Institute, University of
Bristol, Bristol, BS8 1SS, UK
Gavin L. Foster
Ocean and Earth Science, University
of Southampton, and National Oceanography Centre, Southampton,
SO14 3ZH, UK
Paul Markwick
Getech Plc, Leeds, LS8 2LJ, UK
Charlotte L. O'Brien
Department
of Earth Sciences, University of Oxford, Oxford, OX1 3AN, UK
Department of Geology and Geophysics, Yale University, New Haven,
CT 06511, USA
Richard D. Pancost
School of Chemistry, and Cabot Institute, University
of Bristol, Bristol, BS8 1TS, UK
Stuart A. Robinson
Department
of Earth Sciences, University of Oxford, Oxford, OX1 3AN, UK
Neil Wrobel
Getech Plc, Leeds, LS8 2LJ, UK
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Short summary
We explore the influence of changing geography from the period ~ 150 million years ago to ~ 35 million years ago, using a set of 19 climate model simulations. We find that without any CO2 change, the global mean temperature is remarkably constant, but that regionally there are significant changes in temperature which we link back to changes in ocean circulation. Finally, we explore the implications of our findings for the interpretation of geological indicators of past temperatures.
We explore the influence of changing geography from the period ~ 150 million years ago to ~ 35...