Ocean Turbulence. Part II: Vertical Diffusivities of Momentum, Heat, Salt, Mass, and Passive Scalars

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Second-order turbulence closure models for geophysical boundary layers. A review of recent work (2005, methodology): “Statistical modelling of free convection is an area of active research (see Canuto et al., 2001a; Mironov, 2001), and model improvements for such flows may be expected in the near future.”
Evaluation of vertical coordinate and vertical mixing algorithms in the HYbrid-Coordinate Ocean Model (HYCOM) (2004, methodology): “The Goddard Institute for Space Studies (GISS; Canuto et al., 2001, 2002 ) model is a level 2”
Observational and numerical modeling methods for quantifying coastal ocean turbulence and mixing (2008, background): “For the pressure–strain correlators a plethora of closures may be found in the literature (see e.g. Mellor and Yamada, 1974; Launder et al., 1975; Kantha and Clayson, 1994; Canuto et al., 2001, 2002; Cheng et al., 2002; Umlauf and Burchard, 2005).”
The Flexible Global Ocean‐Atmosphere‐Land System Model Grid‐Point Version 3 (FGOALS‐g3): Description and Evaluation (2020, methodology): “The chlorophyll‐a‐dependent solar penetration of the Ohlmann (2003) scheme (Lin et al., 2007) and vertical mixing of Canuto et al. (2001, 2002) are used in LICOM3.”