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Climate of the Past An interactive open-access journal of the European Geosciences Union
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Volume 12, issue 8
Clim. Past, 12, 1635–1644, 2016
https://doi.org/10.5194/cp-12-1635-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
Clim. Past, 12, 1635–1644, 2016
https://doi.org/10.5194/cp-12-1635-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 11 Aug 2016

Research article | 11 Aug 2016

Reconstructing geographical boundary conditions for palaeoclimate modelling during the Cenozoic

Michiel Baatsen et al.
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Amante, C. and Eakins, B. W.: ETOPO1 1 Arc-Minute Global Relief Model: Procedures, Data Sources and Analysis, NOAA Technical Memorandum NESDIS NGDC-24, National Geophysical Data Center, NOAA, https://doi.org/10.7289/V5C8276M, 2016.
Barron, E. J. and Washington, W. M.: The role of geographic variables in explaining paleoclimates: Results from Cretaceous climate model sensitivity studies, J. Geophys. Res., 89, 1267–1279, https://doi.org/10.1029/JD089iD01p01267, 1984.
Bijl, P. K., Schouten, S., Sluijs, A., Reichart, G.-J., Zachos, J. C., and Brinkhuis, H.: Early Palaeogene temperature evolution of the southwest Pacific Ocean, Nature, 461, 776–779, https://doi.org/10.1038/nature08399, 2009.
Bijl, P. K., Bendle, J. A. P., Bohaty, S. M., Pross, J., Schouten, S., Tauxe, L., Stickley, C. E., McKay, R. M., Röhl, U., Olney, M., Sluijs, A., Escutia, C., and Brinkhuis, H.: Eocene cooling linked to early flow across the Tasmanian Gateway, P. Natl. Acad. Sci. USA, 110, 9645–9650, https://doi.org/10.1073/pnas.1220872110, 2013.
Bosboom, R., Dupont-Nivet, G., Grothe, A., Brinkhuis, H., Villa, G., Mandic, O., Stoica, M., Huang, W., Yang, W., Guo, Z., and Krijgsman, W.: Linking Tarim Basin sea retreat (west China) and Asian aridification in the late Eocene, Basin Res., 26, 621–640, https://doi.org/10.1111/bre.12054, 2014a.
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One of the major difficulties in modelling palaeoclimate is constricting the boundary conditions, causing significant discrepancies between different studies. Here, a new method is presented to automate much of the process of generating the necessary geographical reconstructions. The latter can be made using various rotational frameworks and topography/bathymetry input, allowing for easy inter-comparisons and the incorporation of the latest insights from geoscientific research.
One of the major difficulties in modelling palaeoclimate is constricting the boundary...
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