White, Laurent
[UCL]
Beckers, JM.
Deleersnijder, Eric
[UCL]
Legat, Vincent
[UCL]
The main goal of this work is to appraise the finite element method in the way it represents barotropic instabilities. To that end, three different formulations are employed. The free-surface formulation solves the primitive shallow-water equations and is of predominant use for ocean modeling. The vorticity-stream function and velocity-pressure formulations resort to the rigid-lid approximation and are presented because theoretical results are based on the same approximation. The growth rates for all three formulations are compared for hyperbolic tangent and piecewise linear shear flows. Structured and unstructured meshes are utilized. The investigation is also extended to time scales that allow for instability meanders to unfold, permitting the formation of eddies. We find that all three finite element formulations accurately represent barotropic instablities. In particular, convergence of growth rates toward theoretical ones is observed in all cases. It is also shown that the use of unstructured meshes allows for decreasing the computational cost while achieving greater accuracy. Overall, we find that the finite element method for free-surface models is effective at representing barotropic instabilities when it is combined with an appropriate advection scheme and, most importantly, adapted meshes.
- Beckers J-M, Deleersnijder E (1993) Stability of a FBTCS scheme applied to the propagation of shallow-water intertia–gravity waves on various space grids. J Comput Phys 108(1):95–104
- Cockburn B, Karniadakis GE, Shu CW (eds) (2000) Discontinuous Galerkin methods. Theory, computation and applications. In: Lectures notes in computational science and engineering, vol 11. Springer, Berlin Heidelberg New York
- Cushman-Roisin B (1994) Geophysical fluid dynamics. Prentice-Hall, Upper Saddle River, NJ
- Danilov S, Kivman G, Schröter J (2004) A finite-element ocean model: principles and evaluation. Ocean Model 6:125–150
- Dickinson RE, Clare FJ (1973) Numerical study of the unstable modes of a hyperbolic tangent barotropic shear flow. J Atmos Sci 30:1035–1049
- Gresho PM, Chan ST, Lee RL, Upson CD (1984) A modified finite element method for solving the time-dependent, incompressible Navier–Stoked equations. Part 1: theory. Int J Numer Methods Fluids 4:557–598
- Gresho PM, Sani RL (1987) On pressure boundary conditions for the incompressible Navier–Stokes equations. Int J Numer Methods Fluids 7:1111–1145
- Gresho PM, Sani RL (1998) Incompressible flow and the finite element method. Wiley, New York
- Griffies SM, Böning C, Bryan FO, Chassignet EP, Gerdes R, Hasumi H, Hirst A, Treguier A-M, Webb D (2000) Developments in ocean climate modelling. Ocean Model 2:123–192
- Hanert E., Legat V., Deleersnijder E., A comparison of three finite elements to solve the linear shallow water equations, 10.1016/s1463-5003(02)00012-4
- Hanert E, Le Roux DY, Legat V, Deleersnijder E (2004) Advection schemes for unstructured grid ocean modelling. Ocean Model 7:39–58
- Hanert E, Le Roux DY, Legat V, Deleersnijder E (2005) An efficient Eulerian finite element method for the shallow water equations. Ocean Model 10:115–136
- Howard LN (1964) The number of unstable modes in hydrodynamic stability problems. J Mec 3:433–443
- Hart JE (1974) On the mixed stability problem for quasi-geostrophic ocean currents. J Phys Oceanogr 4:349–356
- HUA BACH-LIEN, THOMASSET FRANCOIS, A noise-free finite element scheme for the two-layer shallow water equations, 10.1111/j.1600-0870.1984.tb00235.x
- Killworth PD (1980) Barotropic and baroclinic instability in rotating stratified fluids. Dyn Atmos Ocean 4:143–184
- Killworth PD, Stainforth D, Webb DJ, Paterson SM (1991) The development of a free-surface Bryan–Cox–Semtner ocean model. J Phys Oceanogr 21:1333–1348
- Kuo Hsiao-lan, DYNAMIC INSTABILITY OF TWO-DIMENSIONAL NONDIVERGENT FLOW IN A BAROTROPIC ATMOSPHERE, 10.1175/1520-0469(1949)006<0105:diotdn>2.0.co;2
- Kuo HL (1973) Dynamics of quasigeostrophic flows and instability theory. Adv Appl Mech 13:247–330
- Kuo HL (1978) A two-layer model study of the combined barotropic and baroclinic instability in the tropics. J Atmos Sci 35:1840–1860
- Le Roux DY, Staniforth AN, Lin CA (1998) Finite elements for shallow-water equation ocean models. Mon Weather Rev 126(7):1931–1951
- Michalke A (1964) On the inviscid instability of the hyperbolic tangent velocity profile. J Fluid Mech 19:543–556
- Nechaev D, Schröter J, Yaremchuk M (2003) A diagnostic stabilized finite-element ocean circulation model. Ocean Model 5:37–63
- Pain CC, Piggott MD, Goddard AJH, Fang F, Gorman GJ, Marshall DP, Eaton MD, Power PW, de Oliveira CRE (2004) Three-dimensional unstructured mesh ocean modelling. Ocean Model 10:5–33
- Pedlosky J (1964) The stability of currents in the atmosphere and the ocean: part I. J Atmos Sci 2:201–219
- Pedlosky Joseph, Geophysical Fluid Dynamics, ISBN:9780387907451, 10.1007/978-1-4684-0071-7
- Pietrzak J, Deleersijder E, Schröter J (2005) The second international workshop on unstructured mesh numerical modelling of coastal, shelf and ocean flows, Delft, The Netherlands, September 23–25, 2003. Ocean Model 10:1–3 (Editorial in a special issue)
- Schwanenberg D, Kongeter J (2000) A discontinuous Galerkin method for the shallow water equations with source terms. IEEE Comput Sci Eng 11:419–424
- White L, Legat V, Deleersnijder E, Le Roux D (2006) A one-dimensional benchmark for the propagation of Poincaré waves. Ocean model, in press
Bibliographic reference |
White, Laurent ; Beckers, JM. ; Deleersnijder, Eric ; Legat, Vincent. Comparison of free-surface and rigid-lid finite element models of barotropic instabilities. In: Ocean Dynamics : theoretical, computational oceanography and monitoring, Vol. 56, no. 2, p. 86-103 (2006) |
Permanent URL |
http://hdl.handle.net/2078.1/38467 |