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Original Articles

A numerical model comparison of baroclinic instability in the presence of topography

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Pages 42-65 | Received 02 Mar 1998, Accepted 04 Jun 1999, Published online: 15 Dec 2016

References

  • Arakawa, A. and Lamb, V. R. 1977. Computational design of the basic dynamical processes of the UCLA general circulation model. In: Methods in computational physics 17, Academic Press, pp. 174–264.
  • Asselin, R. 1972. Frequency filter for time integrations. Mon. Wea. Re v. 100, 487–490.
  • Bleck, R. and Boudra, D. B. 1981. Initial testing of a numerical ocean circulation model using a hybrid (quasi-isopycnic) vertical coordinate. J. Phys. Oceanogr. 11, 755–770.
  • Bleck, R. and Boudra, D. B. 1986. Wind-driven spin-up in eddy-resolving ocean models formulated in iso-pycnic and isobaric coordinates. J. Geophys. Res. 91, 7611–7621.
  • Bleck, R. and Smith, L. 1990. A wind-driven isopycnic coordinate model of the north and equatorial Atlantic Ocean. Part I: Model development and supporting experiments. J. Geophys. Res. 95, 3272–3285.
  • Bryan, K. 1969. A numerical method for the study of the circulation of the world ocean. J. Comp. Phys. 4, 347–376.
  • Chao, S. 1990. Instabilities of fronts over a continental margin. J. Geophys. Res. 95, 3199–3211.
  • Chassignet, E. P. 1992. Rings in numerical models of ocean general circulation-a statistical study. J. Geo-phys. Res. 97, 9479–9492.
  • Cox, M. D. 1984. A primitive equation, 3-dimensional model of the ocean. GFDL Ocean Group Tech. Report, No. 1, 250 pp.
  • Cox, M. D. and Bryan, K. 1984. A numerical model of the ventilated thermocline. J. Phys. Oceanogr. 14, 674–687.
  • Derome, J. and Dolph, C. L. 1970. Three-dimensional non-geostrophic disturbances in a baroclinic zonal flow. Geophys. Fluid Dyn. 1, 91–122.
  • Drijfhout, S. S. 1992. Ring genesis and the related heat transport. Part II: A model comparison. J. Phys. Oceanogr. 22, 268–285.
  • Fofonoff, N. P. 1962. Physical properties of sea water. The Sea, Vol. 1. New York, Interscience, 864 pp.
  • Griffiths, C. 1992. Modelling the Iceland Faerce front. PhD thesis, Univ. of Exeter, Exeter, England. 191 pp.
  • Hecht, M. W., Holland, W. R. and Rasch, P. J. 1995. Upwind-weighted advection schemes for ocean tracer transport-an evaluation in a passive tracer context. J. Geophys. Res. 100, 20,763-20,778.
  • Hecht, M. W., Bryan, F. O. and Holland, W. R. 1998. A consideration of tracer advection schemes in a primi-tive equation ocean model. J. Geophys. Res. 103, 3301–3321.
  • Hoskins, B. and Bretherton, F. P. 1972. Atmospheric frontogenesis models: mathematical formulation and solution. J. Atmos. Sc i. 29, 11–37.
  • Huppert, H. E. and Bryan, K. 1976. Topographically generated eddies. Deep Sea Res. 23, 655–679.
  • Ikeda, M. 1981. Meanders and detached eddies of a strong eastward-flowing jet using a two-layer quasi-geostrophic model. J. Phys. Oceanogr. 11, 526–540.
  • Ikeda, M. and Wood, R. A. 1993. Mesoscale stability of an ocean current in the Bryan-Cox model. J. Geophys. Res. 98, 12,527-12,536.
  • Killworth, P. D. 1987. Topographic instabilities in level model OGCMs. Ocean Modelling 75.
  • Killworth, P. D., Stainforth, D., Webb, D. J. and Paterson, S. M. 1991. The development of a free-surface Bryan-Cox-Semtner ocean model. J. Phys. Oceanogr. 21, 1333–1348.
  • Lazier, J. R. N. and Wright, D. G. 1993. Annual velocity variations in the Labrador Sea. J. Phys. Oceanogr. 23, 659–678.
  • LeBlond, P.H. 1982. Satellite observations of Labrador Current undulations. Atmosphere-Ocean 20, 129–142.
  • Lorenz, E. 1967. The nature and theory of the general circulation of the atmosphere. World Meteorol. Organ-ization, Geneva.
  • Matsuno, T. 1966. Numerical integrations of the primi-tive equations by a simulated backward difference method. J. Meteor. Soc. Japan 44, 76–84.
  • Maskell, S. J., Heathershaw, A. D. and Stretch, C. E. 1992. Topographic and eddy effects in a primitive equation model of the Iceland-Faeroes front. J. Marine Systems 3, 343–380.
  • New, A. L., Bleck, R., Jia, Y., Marsh, R., Huddleston, M. and Barnard, S. 1995. An isopycnic model study of the north Atlantic. Part I: Model experiment. J. Phys. Oceanogr. 25, 2667–2699.
  • Oberhuber, J. 1993. Simulation of the Atlantic circulation with a coupled sea ice-mixed layer-isopycnal general circulation model. Part I: Model description. J. Phys. Oceanogr. 23, 808–829.
  • Orlanski, I. and Cox, M. D. 1973. Baroclinic instability in ocean currents. Geophys. Fluid Dyn. 3, 297–332.
  • Pedlosky, J. 1979. Geophysical fluid dynamics. Springer Verlag, 624 pp.
  • Roberts, M. J., Marsh, R., New, A. L. and Wood, R. A. 1996. An intercomparison of a Bryan-Cox-type ocean model and an isopycnic ocean model. Part I: The subpolar gyre and high-latitude processes. J. Phys. Oceanogr. 26, 1495–1527.
  • Rood, R. B. 1987. Numerical advection algorithms and their role in atmospheric transport and chemistry models. Reviews of Geophys. 25, 71–100.
  • Smith, L. T. 1992. Numerical simulations of stratified rotating flow over finite amplitude topography. J. Phys. Oceanogr. 22, 686–696.
  • Wajsowicz, R. C. 1986. Free planetary waves in finite-difference numerical models. J. Phys. Oceanogr. 16, 773–789.
  • Wang, W. 1997. The gulf stream near 73°W: views from observations and a primitive equation model. Deep Sea Research, Part I. Oceanographic Research Papers, 44, 1147-1166.
  • Wilkin, J. L., Mansbridge, J. V. and Godfrey, J. S. 1995. Pacific ocean heat transport at 24°N in a high-reso-lution global model. J. Phys. Oceanogr. 25, 2204–2214.
  • Wood, R. A. and Ikeda, M. 1994. Comparison of meso-scale meanders and eddies simulated by quasigeostrophic and primitive equation models: a case study. J. Geophys. Res. 99, 22,645-22, 663.
  • Zalesak, S. T. 1979. Fully multidimensional fluxscale corrected transport algorithms for fluids. J. Comp. Phys. 31, 335-362.