Large-scale mass transports, water mass formation, and diffusivities estimated from World Ocean Circulation Experiment (WOCE) hydrographic data

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Eddy stirring in the Southern Ocean (2011, methodology): “[2009], Smith 714 and Marshall [2009] and Abernathy et al. [2009] based on 715 numerical simulations of varying complexity.”
The GFDL CM3 Coupled Climate Model: Characteristics of the Ocean and Sea Ice Simulations (2011, methodology): “16 discussed in section 3c), which is somewhat stronger than estimates from observations (Ganachaud 2003; Lumpkin and Speer 2003; Talley 2003, 2008), which in turn leads to a lower simulated Atlantic DSL in both models.”
The Impact of Abyssal Mixing Parameterizations in an Ocean General Circulation Model (2009, background): “However, there is no observational evidence to suggest that the mixing in the ocean is horizontally uniform, and indeed there is signiﬁcant evidence that it is heterogeneous with spatial variations of several orders of magnitude in its intensity (Polzin et al. 1997; Ganachaud 2003).”
Global Ocean Meridional Overturning (2007, methodology): “The net overturning across 32°S, at 20.9 6.7 Sv, is close to previous estimates at this latitude (21 6 Sv: Ganachaud 2003b; 22 Sv: Talley et al. 2003).”