NANADec 12, 2014

A conservation formulation and a numerical algorithm for the double-gyre nonlinear shallow-water model

arXiv:1403.0140
Originality Synthesis-oriented
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For ocean modelers, this provides a more robust numerical method for simulating double-gyre circulation, though it is an incremental improvement over existing finite volume approaches.

The paper reformulates the double-gyre nonlinear shallow-water model into a conservation law and solves it with a second-order fractional-step algorithm that is insensitive to viscosity and achieves high resolution on coarse grids. The method is validated against exact solutions and produces results consistent with literature.

We present a conservation formulation and a numerical algorithm for the reduced-gravity shallow-water equations on a beta plane, subjected to a constant wind forcing that leads to the formation of double-gyre circulation in a closed ocean basin. The novelty of the paper is that we reformulate the governing equations into a nonlinear hyperbolic conservation law plus source terms. A second-order fractional-step algorithm is used to solve the reformulated equations. In the first step of the fractional-step algorithm, we solve the homogeneous hyperbolic shallow-water equations by the wave-propagation finite volume method. The resulting intermediate solution is then used as the initial condition for the initial-boundary value problem in the second step. As a result, the proposed method is not sensitive to the choice of viscosity and gives high-resolution results for coarse grids, as long as the Rossby deformation radius is resolved. We discuss the boundary conditions in each step, when no-slip boundary conditions are imposed to the problem. We validate the algorithm by a periodic flow on an f-plane with exact solutions. The order-of-accuracy for the proposed algorithm is tested numerically. We illustrate a quasi-steady-state solution of the double-gyre model via the height anomaly and the contour of stream function for the formation of double-gyre circulation in a closed basin. Our calculations are highly consistent with the results reported in the literature. Finally, we present an application, in which the double-gyre model is coupled with the advection equation for modeling transport of a pollutant in a closed ocean basin.

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