A pretty good sponge: Dealing with open boundaries in limited-area ocean models

Abstract The problem of computing within a limited domain surrounded by open boundaries is discussed within the context of the shallow-water wave equations by comparing three different treatments, all of which surround the domain by absorbing zones intended to prevent reflections of outgoing waves. The first, which has attracted a lot of attention for use in electromagnetic and aeroacoustic applications, is intended to prevent all reflections. However, it has not yet been developed to handle the second important requirement of open boundaries, namely the ability to pass information about external conditions into the domain of interest. The other two treatments, which absorb differences from a specified external solution, allow information to pass through the open boundary in both directions. One, based on the flow relaxation scheme of [Martinsen, E.A., Engedahl, H., 1987. Implementation and testing of a lateral boundary scheme as an open-boundary condition in a barotropic ocean model. Coastal Eng. 11, 603–627] and termed here the “simple sponge,” relaxes all fields toward their external counterparts. The other, a simplification and generalization of the perfectly matched layer, referred to here as the “pretty good sponge,” avoids absorbing the component of momentum parallel to the open boundary. Comparisons for a case that is dominated by outgoing waves shows the pretty good sponge to perform essentially as well as the perfectly matched layer and better than the simple sponge. In comparisons for a geostrophically balanced eddy passing through open boundaries, the pretty good sponge out-performed the simple sponge when the only external information available was about the advecting flow, but when information about the nature of the eddy in the sponge zones was also available, the simple sponge performed better. For the case of an equatorial soliton passing through the boundary and no information provided about its nature outside the open domain, again the pretty good sponge performed better. Proving useful for situations governed by nonlinear equations forced by external conditions and being easy to implement, the pretty good sponge should be considered for use with existing limited-area ocean models.

[1]  E. Turkel,et al.  Absorbing PML boundary layers for wave-like equations , 1998 .

[2]  J. Lavelle Flow, hydrography, turbulent mixing, and dissipation at Fieberling Guyot examined with a primitive equation model , 2006 .

[3]  E. A. Martinsen,et al.  Implementation and testing of a lateral boundary scheme as an open boundary condition in a barotropic ocean model , 1987 .

[4]  Daniel J. Bodony,et al.  Analysis of sponge zones for computational fluid mechanics , 2006, J. Comput. Phys..

[5]  Alexander F. Shchepetkin,et al.  Open boundary conditions for long-term integration of regional oceanic models , 2001 .

[6]  David Gottlieb,et al.  A Mathematical Analysis of the PML Method , 1997 .

[7]  Jean-Pierre Berenger,et al.  A perfectly matched layer for the absorption of electromagnetic waves , 1994 .

[8]  W. Hurlin,et al.  Simulation of the Seasonal Cycle of the Tropical Pacific Ocean , 1987 .

[9]  Ivar Lie,et al.  Well-posed transparent boundary conditions for the shallow water equations , 2001 .

[10]  John P. Boyd,et al.  Equatorial Solitary Waves. Part 3: Westward-Traveling Modons , 1985 .

[11]  K. Döös,et al.  Open boundary conditions for barotropic waves , 2003 .

[12]  Dan Givoli,et al.  High-order nonreflecting boundary conditions for the dispersive shallow water equations , 2003 .

[13]  Patrick Joly,et al.  Stability of perfectly matched layers, group velocities and anisotropic waves , 2003 .

[14]  William H. Raymond,et al.  A radiation boundary condition for multi‐dimensional flows , 1984 .

[15]  Xing Li Absorbing Boundary Conditions for the Numerical Simulation of Acoustic Waves , 2006 .

[16]  A. Mcdonald,et al.  A Step toward Transparent Boundary Conditions for Meteorological Models , 2002 .

[17]  F. Hu A Stable, perfectly matched layer for linearized Euler equations in unslit physical variables , 2001 .

[18]  R. Higdon Radiation boundary conditions for dispersive waves , 1994 .

[19]  I. Orlanski A Simple Boundary Condition for Unbounded Hyperbolic Flows , 1976 .

[20]  E. Blayo,et al.  Revisiting open boundary conditions from the point of view of characteristic variables , 2005 .

[21]  D. Gottlieb,et al.  Regular Article: Well-posed Perfectly Matched Layers for Advective Acoustics , 1999 .

[22]  Beny Neta,et al.  A Perfectly Matched Layer Approach to the Linearized Shallow Water Equations Models , 2004, Monthly Weather Review.

[23]  Fang Q. Hu,et al.  Development of PML absorbing boundary conditions for computational aeroacoustics: A progress review , 2008 .

[24]  Peter G. Petropoulos,et al.  On the Termination of the Perfectly Matched Layer with Local Absorbing Boundary Conditions , 1998 .

[25]  Dan Givoli,et al.  A stratified dispersive wave model withhigh-order nonreflecting boundary conditions , 2004 .

[26]  Eric P. Chassignet,et al.  North Atlantic Simulations with the Hybrid Coordinate Ocean Model (HYCOM): Impact of the Vertical Coordinate Choice, Reference Pressure, and Thermobaricity , 2003 .

[27]  R. Flather A tidal model of the north-west European continental shelf , 1976 .

[28]  S. Tsynkov Numerical solution of problems on unbounded domains. a review , 1998 .

[29]  John P. Boyd,et al.  Equatorial Solitary Waves. Part I: Rossby Solitons , 1980 .

[30]  J. O'Brien,et al.  Open boundary conditions in rotating fluids , 1980 .

[31]  Dale B. Haidvogel,et al.  Numerical Ocean Circulation Modeling , 1999 .

[32]  J. Hesthaven,et al.  The Analysis and Construction of Perfectly Matched Layers for Linearized Euler Equations , 2022 .

[33]  H. Davies,et al.  A lateral boundary formulation for multi-level prediction models. [numerical weather forecasting , 1976 .

[34]  F. Hu On Absorbing Boundary Conditions for Linearized Euler Equations by a Perfectly Matched Layer , 1995 .

[35]  Didier Pinchon,et al.  Conditions limites non réfléchissantes pour un modèle de Saint-Venant bidimensionnel barotrope linéarisé , 1997 .