Reconstructing surface temperature changes over the past 600 years using climate model simulations with data assimilation

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Assimilation of Time-Averaged Pseudoproxies for Climate Reconstruction (2014, methodology): “For a typical multiproxy network, Mann et al. (2007) estimate a mean autocorrelation of 0.”
A Pseudoproxy Evaluation of Bayesian Hierarchical Modeling and Canonical Correlation Analysis for Climate Field Reconstructions over Europe (2013, background): “For instance, paleoclimatic data assimilation schemes recently have been proposed and explored (Widmann et al. 2010; Goosse et al. 2010; Luterbacher et al. 2010a).”
Deconstructing the Last Glacial termination: the role of millennial and orbital-scale forcings (2011, background): “LOCH is a 3-dimensional global model of the oceanic carbon cycle (Mouchet and Francois, 1996; Menviel et al., 2008b; Goosse et al., 2010a).”