Introduction to geophysical fluid dynamics : physical and numerical aspects

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Southern Ocean eddy phenomenology (2015, background): “The intrinsic meridional propagation of the eddies is equatorward for the long-lived anticyclones and poleward for the cyclones [Cushman-Roisin and Beckers, 2011; CSS11].”
Some Nonlinear, Equatorially Trapped, Nonhydrostatic Internal Geophysical Waves (2014, methodology): “…a broadly used approach for the study of eastward-propagating equatorial Kelvin waves relies on a b-plane approximation of the governing equations in the shallow-water regime of a one-layer reduced gravity model [cf. the discussion in Cushman-Roisin and Beckers (2011) and Fedorov and Brown (2009)].”
Subgrid modelling for two-dimensional turbulence using neural networks (2018, background): “…and geophysical ﬂow problems has revealed that the constant is not single-valued and varies depending on resolution and ﬂow characteristics (Galperin & Orszag 1993; Canuto & Cheng 1997; Vorobev & Zikanov 2008) with higher values speciﬁcally for geophysical ﬂows (Cushman-Roisin & Beckers 2011).”
Local martingale and pathwise solutions for an abstract fluids model (2010, neutral): “See [8], [33] for further physical background.”