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Steven J. Phipps, Helen V. McGregor, Joëlle Gergis, Ailie J. E. Gallant, Raphael Neukom, Samantha Stevenson, Duncan Ackerley, Josephine R. Brown, Matt J. Fischer, and Tas D. van Ommen

. Proxy data can be used to constrain and evaluate model simulations, while climate models can be used to explore the mechanisms that have driven past climatic changes. For example, Mann et al. (2009) , Graham et al. (2011) , and Goosse et al. (2012) combine proxy data with climate modeling to study the dynamical origins of the MCA. Paleoclimate data–model comparison can be used to assess model performance (e.g., Braconnot et al. 2007a , b ), to constrain projections of future climate change (e

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