Numerical models of oceans and oceanic processes

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An elastic-viscous-plastic sea ice model formulated on Arakawa B and C grids (2009, methodology): “Such interpolations would be avoided if a C grid were used in the calculation of the sea ice dynamics, which is why we have also formulated a centred difference version of the EVP dynamics (see Kantha and Clayson (2000) for a C grid, centred difference formulation of the VP case).”
A high‐order triangular discontinuous Galerkin oceanic shallow water model (2008, background): “In Stommel ’s theory, the inclusion of the bottom friction raises the order of the governing equation and enables the beta effect to produce a western boundary current [19], which makes Stommel’s solution not quite realistic.”
A review on regional convection‐permitting climate modeling: Demonstrations, prospects, and challenges (2015, background): “In coupled GCM ocean models, deep ocean layers require hundreds of years to adjust while the upper ocean only requires about 50 years [Kantha and Clayson, 2000].”