Fundamentals of Ocean Climate Models

By S. Griffies. 2004

380 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/dbbd847651254044c93e719fe6700ab4afbfd798

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In Global and Planetary Change

In Oceanography

Citations in the corpus

The GFDL Global Ocean and Sea Ice Model OM4.0: Model Description and Simulation Features (2019, methodology): “…∂t r ∇r ¼ bx ∂∂x r þ by ∂ ∂y r : (A20) The transport of seawater crossing surfaces of constant r is measured by the dia‐surface velocity component (see section 6.7 of Griffies, 2004) ∂z ∂r Dr Dt ¼ zr _r ; (A21) with zr the specific thickness that is assumed one‐signed throughout the ocean, and…”
A boundary-value problem for the parameterized mesoscale eddy transport (2010, methodology): “However, even if the diffusivity has become a nonlocal function of the vertical density structure, the streamfunction WGM has generally remained a local function of the neutral slope at each point in the ocean in most current parameterizations.”
Parameterization of Eddy Fluxes near Oceanic Boundaries (2008, methodology): “This simulation confirms that the diabatic component of the mesoscale eddy fluxes is not confined to the mixed layer, contrary to what is assumed in Treguier et al. (1997) and Griffies (2004).”
Resolution convergence and sensitivity studies with North Atlantic circulation models. Part I: The western boundary current system (2007, methodology): “…the preservation of grid-Reynolds and grid-Peclet numbers with 14 variable resolution, as mentioned in the Model Configuration section, and which we have long used as a rule-of-thumb (the basis for this scaling can be found in the Appendix of Bryan et al. 1975, and in Chapter 18 of Griffies 2004) .”