A Unified Formulation of Quasi-Geostrophic and Shallow Water Equations via Projection
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Thiry, Louis
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Sorbonne Univ, ANGE Team, INRIA Paris, Lab Jacques Louis Lions, Paris, FranceSorbonne Univ, ANGE Team, INRIA Paris, Lab Jacques Louis Lions, Paris, France
Thiry, Louis
[1
]
Li, Long
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Univ Rennes 1, ODYSSEY Team, INRIA Rennes, IRMAR, Rennes, FranceSorbonne Univ, ANGE Team, INRIA Paris, Lab Jacques Louis Lions, Paris, France
Li, Long
[2
]
Memin, Etienne
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Univ Rennes 1, ODYSSEY Team, INRIA Rennes, IRMAR, Rennes, FranceSorbonne Univ, ANGE Team, INRIA Paris, Lab Jacques Louis Lions, Paris, France
Memin, Etienne
[2
]
Roullet, Guillaume
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Univ Bretagne Occidentale, Lab Oceanog Phys & Spatiale, Brest, FranceSorbonne Univ, ANGE Team, INRIA Paris, Lab Jacques Louis Lions, Paris, France
Roullet, Guillaume
[3
]
机构:
[1] Sorbonne Univ, ANGE Team, INRIA Paris, Lab Jacques Louis Lions, Paris, France
This paper introduces a unified model for layered rotating shallow-water (RSW) and quasi-geostrophic (QG) equations, based on the intrinsic relationship between these two sets of equations. We propose a novel formulation of the QG equations as a projection of the RSW equations. This formulation uses the same prognostic variables as RSW, namely velocity and layer thickness, thereby restoring the proximity of these two sets of equations. It provides direct access to the ageostrophic velocities embedded within the geostrophic velocities resolved by the QG equations. This approach facilitates the study of differences between QG and RSW using a consistent numerical discretization. We demonstrate the effectiveness of this formulation through examples including vortex shear instability, double-gyre circulation, and a simplified North Atlantic configuration. In this paper, we present a straightforward way to connect two important sets of ocean equations: the layered rotating shallow-water (RSW) equations and the quasi-geostrophic (QG) equations. We consider a unified method to formulate the QG equations as a projection of the RSW equations. This method uses the same variables as the RSW equations, making it easier to understand how these two sets of equations relate to each other. Our approach also provides direct access to important velocity information that is usually hidden in the QG equations. This allows us to study the differences between the QG and RSW equations using the same numerical techniques. We show the benefits of our model with two examples: a vortex shear instability and a double-gyre configuration. This work provides a useful tool for the understanding of ocean dynamics. Developing a unified numerical framework for nested models can greatly simplify oceanographic modeling and enhance accuracy. Introduces QG equations as a projection of rotating shallow-water (RSW) equations using the same prognostic variables Allows consistent nested numerical methods for both QG and RSW equations Successfully tested on vortex shear instability, double-gyre circulation, and a simplified North Atlantic configuration
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[Anonymous], 1992, Journal of Computational Physics, DOI DOI 10.1016/0021-9991(92)90388-F