Two tales of initializing decadal climate predictions experiments with the ECHAM5/MPI-OM model

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How does internal variability influence the ability of CMIP5 models to reproduce the recent trend in Southern Ocean sea ice extent (2012, background): “Matei et al. (2012a) have pointed out a significant correlation between hindcast and observations for the Atlantic Meridional Overturning Circulation (AMOC) strength at 26.5◦ N690 up to 4 yr ahead.”
Decadal climate prediction: an update from the trenches (2014, methodology): “…skill of temperature in the North Atlantic (e.g., Smith et al. 2010; van Oldenborgh et al. 2012; Pohlmann et al. 2009; Keenlyside et al. 2008; Matei et al. 2012c; Doblas-Reyes et al. 2013; Yang et al. 2013; A. Rosati et al. 2014, unpublished manuscript; R. Msadek et al. 2014, unpublished…”
A Review of the Role of the Atlantic Meridional Overturning Circulation in Atlantic Multidecadal Variability and Associated Climate Impacts (2019, methodology): “…initialized decadal prediction experiments in reproducing the observed subpolar AMV signal at decadal lead times (e.g., Hermanson et al., 2014; Matei et al., 2012; Msadek et al., 2014; Robson, Sutton, & Smith, 2012, 2014; Yang et al., 2013; Yeager et al., 2012, 2015, 2018; Yeager & Robson,…”