Cover Journal of Physical Oceanography
Journal of Physical Oceanography

  • Alvarez, A., J. Tintore, G. Holloway, M. Eby, and J. M. Beckers, 1994: Effect of topographic stress on the circulation in the western Mediterranean. J. Geophys. Res.,99, 16 053–16 064.

  • Andrews, D. G., and M. E. McIntyre, 1978: An exact theory for nonlinear waves on a Lagrangian-mean flow. J. Fluid Mech.,89, 609–646.

  • ——, J. R. Holton, and C. B. Leovy, 1987: Middle Atmosphere Dynamics. Academic Press, 489 pp.

  • Beckmann, A., 1995: Numerical modeling of time-mean flow at isolated seamounts. Topographic Effects in the Ocean. Proceedings ‘Aha Huliko‘a Winter Workshop, P. Muller and D. Henderson, Eds., University of Hawaii, 57–66.

  • ——, and D. B. Haidvogel, 1993: Numerical simulation of flow around a tall isolated seamount. Part I: Problem formulation and model accuracy. J. Phys. Oceanogr.,23, 1736–1753.

  • ——, and ——, 1996: A numerical simulation of flow at Fieberling Guyot. J. Geophys. Res., in press.

  • Bleck, R., C. Rooth, D. Hu, and L. T. Smith, 1992: Salinity-driven thermohaline transients in a wind- and thermohaline-forced isopycnic coordinate model of the North Atlantic. J. Phys. Oceanogr.,22, 1486–1515.

  • Brink, K. H., 1995: Tidal and lower frequency currents above Fieberling Guyot. J. Geophys. Res.,100, 10 817–10 832.

  • Chapman, D. C., and D. B. Haidvogel, 1992: Formation of Taylor caps over a tall isolated seamount in a stratified ocean. Geophys. Astrophys. Fluid Dyn.,64, 31–65.

  • Cherniawsky, J., and G. Holloway, 1991: An upper ocean general circulation model for the North Pacific: Preliminary experiments. Atmos.–Ocean,29, 737–784.

  • ——, and ——, 1993: On western boundary current separation in an upper ocean general circulation model of the North Pacific. J. Geophys. Res.,98, 22 843–22 850.

  • Danabasoglu, G., and J. C. McWilliams, 1995: Sensitivity of the global ocean to parameterizations of mesoscale tracer transports. J. Climate,8, 2967–2987.

  • ——, ——, and P. R. Gent, 1994: The role of mesoscale tracer transports in the global ocean circulation. Science,264, 1123–1126.

  • Danielsen, E. F., and R. S. Hipskind, 1980: An objective method for determining the generalized transport-tensor for two-dimensional Eulerian models. U.S. Govt. Rep. FAA-EE-80-32, 65 pp. [Available from NTIS, Springfield, VA 22161.].

  • Duffy, P. B., P. Eltgroth, A. J. Bourgeois, and K. Caldeira, 1995: Effect of improved subgrid scale transport of tracers on uptake of bomb radiocarbon in the GFDL ocean general circulation model. Geophys. Res. Lett.,22, 1065–1068.

  • Dunkerton, T., 1978: On the mean meridional motions of the stratosphere and mesosphere. J. Atmos. Sci.,35, 2325–2333.

  • Eby, M., and G. Holloway, 1994: Sensitivity of a large-scale ocean model to a parameterization of topographic stress. J. Phys. Oceanogr.,24, 2577–2588.

  • England, M. H., 1993: Representing the global-scale water masses in ocean general circulation models. J. Phys. Oceanogr.,23, 1523–1552.

  • ——, 1995: Usingchlorofluorocarbons to assess ocean climate models. Geophys. Res. Lett.,22, 3051–3054.

  • ——, and G. Holloway, 1996: Simulations of CFC-11 outflow and seawater age in the deep North Atlantic. Applications of Trace Substance Measurements to Oceanographic Problems, P. Schlosser, W. M. Smethie, and J. R. Toggweiler, Eds., Amer. Geophys. Union, in press.

  • Farrow, D. E., and D. P. Stevens, 1995: A new tracer advection scheme for Bryan and Cox type ocean circulation models. J. Phys. Oceanogr.,25, 1731–1741.

  • Fyfe, J., and G. Marinone, 1995: On the role of unresolved eddies in a model of the residual currents in the central Strait of Georgia, B.C. Atmos.–Ocean,33, 613–619.

  • Gent, P. R., and J. C. McWilliams, 1990: Isopycnal mixing in ocean circulation models. J. Phys. Oceanogr.,20, 150–155.

  • ——, J. Willebrand, T. J. McDougall, and J. C. McWilliams, 1995: Parameterizing eddy-induced tracer transports in ocean circulation models. J. Phys. Oceanogr.,25, 463–474.

  • Gerdes, R., C. Koberle, and J. Willebrand, 1991: The influence of numerical advection schemes on the results of ocean general circulation models. Climate Dyn.,5, 211–226.

  • Gill, A. E., 1982: Atmosphere–Ocean Dynamics. Academic Press, 662 pp.

  • Greatbatch, R. J., and K. G. Lamb, 1990: On parameterizing vertical mixing of momentum in non-eddy-resolving ocean model. J. Phys. Oceanogr.,20, 1634–1637.

  • Haidvogel, D. B., A. Beckmann, D. C. Chapman, and R. Q. Lin, 1993: Numerical simulation of flow around a tall isolated seamount. Part II: Resonant generation of trapped waves. J. Phys. Oceanogr.,23, 2373–2391.

  • Hecht, M. W., W. R. Holland, and P. J. Rasch, 1995: Upwind-weighted advection schemes for ocean tracer transport: An evaluation in a passive tracer context. J. Geophys. Res.,100, 20 763–20 778.

  • Holloway, G., 1992: Representing topographic stress for large-scale ocean models. J. Phys. Oceanogr.,22, 1033–1046.

  • ——, 1996: Neptune effect: Statistical mechanical forcing of ocean circulation. Stochastic Modelling in Physical Oceanography, R. J. Adler, P. Muller, and B. Rozovskii, Eds., Birkhauser, 207–220.

  • ——, and T. Sou, 1996: Measuring skill of a topographic stress parameterization in a large-scale ocean model. J. Phys. Oceanogr.,26, 1088–1092.

  • ——, ——, and M. Eby, 1995: Dynamics of circulation of the Japan Sea. J. Mar. Res.,53, 539–569.

  • Holton, J. R., 1981: An advective model for two-dimensional transport of stratospheric trace species. J. Geophys. Res.,86, 11 989–11 994.

  • Hu, D., 1997: Global-scale water masses, meridional circulation, and heat transport simulated with a global isopycnal ocean model. J. Phys. Oceanogr.,27, 96–120.

  • Kazantsev, E., J. Sommeria, and J. Verron, 1997: Subgrid-scale eddy parameterization by statistical mechanics in a barotropic ocean model. J. Phys. Oceanogr..

  • McCreary, J. P., and P. K. Kundu, 1988: A numerical investigation of the Somali Current during the Southwest Monsoon. J. Mar. Res.,46, 25–58.

  • McDougall, T. J., and P. C. McIntosh, 1996: Thetemporal-residual-mean velocity. Part I: Derivation and the scalar conservation equations. J. Phys. Oceanogr.,26, 2653–2665.

  • New, A. L., R. Bleck, Y. Jia, R. Marsh, M. Huddleston, and S. Gernard, 1995: An isopycnic model study of the North Atlantic. Part I: Model experiment. J. Phys. Oceanogr.,25, 2667–2699.

  • Olbers, D. J., M. Wenzel, and J. Willebrand, 1985: The inference of North Atlantic circulation patterns from climatological hydrographic data. Rev. Geophys.,23, 313–356.

  • Pal, B. K., and G. Holloway, 1996: Dynamics of circulation off the westcoast of Vancouver Island. Contin. Shelf Res.,16, 1591–1607.

  • Redi, M. H., 1982: Oceanic isopycnal mixing by coordinate rotation. J. Phys. Oceanogr.,12, 1154–1158.

  • Robitaille, D. Y., and A. J. Weaver, 1995: Validation of sub-grid-scale mixing schemes using CFCs in a global ocean model. Geophys. Res. Lett.,22, 2917–2920.

  • Salmon, R., G. Holloway, and M. C. Hendershott, 1976: The equilibrium statistical mechanics of simple quasi-geostrophic models. J. Fluid Mech.,75, 691–703.

  • Sou, T., G. Holloway, and M. Eby, 1996: Effects of topographic stress on Caribbean Sea circulation. J. Geophys. Res.,101, 16 449–16 453.

  • Treguier, A. M., I. M. Held, and V. D. Larichev, 1997: On the parameterization of quasigeostrophic eddies in primitive equation ocean models. J. Phys. Oceanogr.,27, 571–584.

  • Tung, K. K., 1982: On the two-dimensional transport of stratospheric trace gases in isentropic coordinates. J. Atmos. Sci.,39, 2330–2355.

All Time Past Year Past 30 Days
Abstract Views 0 0 0
Full Text Views 3 3 3
PDF Downloads 4 4 4
Article Type:
Research Article

Eddy Transport of Thickness and Momentum in Layer and Level Models

Greg Holloway1
View More View Less
  • 1 Institute of Ocean Sciences, Sidney, British Columbia, Canada
Print Publication:
01 Jun 1997
DOI:
https://doi.org/10.1175/1520-0485(1997)027<1153:ETOTAM>2.0.CO;2
Page(s):
1153–1157
Restricted access

Abstract

The relation between thickness diffusion in layer and level models is set out. Parameterizations of thickness diffusion are related to a parameterization of eddy effects on momentum. The author anticipates where these parameterizations for thickness and momenta are likely to fail and how the anticipated failures may be overcome.

Corresponding author address: Dr. Greg Holloway, Institute of Ocean Sciences, University of Victoria, P.O. Box 6000, 9860 West Saanich Road, Sidney, BC V8L 4B2, Canada.

Email: zounds@ios.bc.ca

Abstract

The relation between thickness diffusion in layer and level models is set out. Parameterizations of thickness diffusion are related to a parameterization of eddy effects on momentum. The author anticipates where these parameterizations for thickness and momenta are likely to fail and how the anticipated failures may be overcome.

Corresponding author address: Dr. Greg Holloway, Institute of Ocean Sciences, University of Victoria, P.O. Box 6000, 9860 West Saanich Road, Sidney, BC V8L 4B2, Canada.

Email: zounds@ios.bc.ca

Save