The Temporal-Residual-Mean Velocity. Part II: Isopycnal Interpretation and the Tracer and Momentum Equations

By Trevor J. McDougall, P. McIntosh. 2001

177 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/2cf3d3cc81326a67632ec429a53d8f8bf1c3a470

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Citations in the corpus

The GFDL Global Ocean and Sea Ice Model OM4.0: Model Description and Simulation Features (2019, background): “…subgrid advective terms solely as lateral transports, thus interpreting them as layer bolus transport as appropriate for vertical Lagrangian models rather than a three‐dimensional eddy‐induced advection as appropriate for vertical Eulerian models (see McDougall & McIntosh, 2001 for details).”
Parameterization of Eddy Fluxes near Oceanic Boundaries (2008, background): “However, near horizontal and vertical boundaries eddies can develop diabatic behavior, and some ad hoc form of adjustment has to be made to avoid false eddy transports through the solid boundaries (Danabasoglu and McWilliams 1995; Large et al. 1997; McDougall and McIntosh 2001; Killworth 2001).”
A boundary-value problem for the parameterized mesoscale eddy transport (2010, methodology): “TRM hu 0q0i j@z ~qj þ 1 2 hðq0Þ2i@zhui j@z ~qj2 ; ð40Þ where ~q is the modified mean potential density (see for details, McDougall and McIntosh, 2001).”
The Role of Eddies in Determining the Structure and Response of the Wind-Driven Southern Hemisphere Overturning: Results from the Modeling Eddies in the Southern Ocean (MESO) Project (2006, background): “Theoretical formalisms such as the temporal residual mean (McDougall and McIntosh 2001) or the transformed Eulerian mean (TEM; Andrews and McIntyre 1976; Ferrari and Plumb 2003) cast the eddy transport into a form that isolates the eddy terms in the momentum, tracer transport, or continuity equation”
Fundamentals of Ocean Climate Models (2004, background): “When a fluid parcel nears a boundary, if the vertical displacement ξ ∼ λ1 |S| is greater than the distance to the boundary, the density surface associated with that eddy is truncated or clipped by the boundary (for discussions, see Treguier et al., 1997; Held and Schneider, 1999; McDougall and McInt”
Can Large Eddy Simulation Techniques Improve Mesoscale Rich Ocean Models (2013, methodology): “Roberts and Marshall [1998] suggest that the Gent and McWilliams [1990] parameterization (hereafter gM) may be used as a subgrid-scale mechanism for the dissipation of enstrophy in eddying models.”
North Atlantic Simulations with the Hybrid Coordinate Ocean Model (HYCOM): Impact of the Vertical Coordinate Choice, Reference Pressure, and Thermobaricity (2003, methodology): “5 turbulence closure model (Mellor and Yamada 1982), or a Goddard Institute for Space Studies (GISS) level-2.”