The Effect of Orbital Forcing on the Mean Climate and Variability of the Tropical Pacific

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Deconstructing the Last Glacial termination: the role of millennial and orbital-scale forcings (2011, background): “All rights reserved. doi:10.1016/j.quascirev.2011.02.005 Lunt et al., 2006; Marsh et al., 2006; Timmermann et al., 2007, 2009a; Timm and Timmermann, 2007; Liu et al., 2009; Timmermann and Menviel, 2009).”
Early Pliocene increase in thermohaline overturning: A precondition for the development of the modern equatorial Pacific cold tongue (2010, result): “This SST response to CAS closure is very similar to the SST response of the HadCM3 model to an intensification of the AMOC [Timmermann et al., 2007b] (Figure 10b) and to the ECBILT‐CLIO SST response to CAS closing (see auxiliary material).”
The influence of a weakening of the atlantic meridional overturning circulation on ENSO (2006, background): “The results may have important implications for the interpretation of global multidecadal variability and paleo-proxy data.”