ACKNOWLEDGEMENTS

The authors would like to thank the United States Geological Survey for providing the PRISM2 digital data set. We would also like to thank Dr. Mark Chandler of the Goddard Institute of Space Science (GISS/NASA) for his advice and experience concerning aspects of middle Pliocene palaeoclimate modelling. This research was carried out in receipt of a Reading University Endowment Trust Fund award, which is gratefully acknowledged.

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