Response to Increasing Southern Hemisphere Winds in CCSM4

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Using a resolution function to regulate parameterizations of oceanic mesoscale eddy effects (2013, background): “Some improvements in large-scale measures of eddy effects, such as the Southern Ocean overturning response to wind-stress changes, can be obtained by adopting parameterizations whose intensity and structure are free to vary greatly with the model’s simulated state (Gent and Danabasoglu, 2011).”
Observations, inferences, and mechanisms of the Atlantic Meridional Overturning Circulation: A review (2016, background): “…and Radko, 2003; Abernathey et al., 2011], and hence, the response of the AMOC to Southern Ocean winds is relatively modest [Hallberg and Gnanadesikan, 2006; Farneti et al., 2010; Farneti and Delworth, 2010; Farneti and Gent, 2011; Gent and Danabasoglu, 2011; Bryan et al., 2013; Gent, 2015].”
Antarctic climate response to stratospheric ozone depletion in a fine resolution ocean climate model (2012, methodology): “5) at two resolutions, with set-ups that are identical to those in Gent et al. [2010], Kirtman et al. [2012], and Bryan and Gent [2012].”