Algorithms for Density, Potential Temperature, Conservative Temperature, and the Freezing Temperature of Seawater

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A Technical Guide to MOM4 (2004, background): “(1991), discretization of gravity waves on a B-grid can admit a stationary grid scale checkerboard pattern (see also Messinger (1973) and Janjić (1974) for atmospheric discussions).”
A Gibbs function for seawater thermodynamics for -6 to 80 °C and salinity up to 120gkg-1 (2008, background): “Inclusion of specific entropy would, for example, allow for an effective and accurate computation of potential temperature and potential density (Bradshaw, 1978; Feistel, 1993), especially in numerical ocean models (McDougall et al., 2003; Jackett et al., 2006).”
The Parallelized Large-Eddy Simulation Model (PALM) version 4.0 for atmospheric and oceanic flows: model formulation, recent developments, and future perspectives (2015, methodology): “The algorithm is based on polynomials depending on Sa, θ , and p (see Jackett et al., 2006, Table A2).”