OCEAN MODELS
Merryfield, W. J., Holloway, G., and Gargett, A. E. (1999). A global ocean model
with doublediffusive mixing. J. Phys. Oceanogr., 29:1124-1142.
Pacanowski, R. C. and Philander, S. G. H. (1981). Parameterization of vertical mixing
in numerical models of the tropical ocean. J. Phys. Oceanogr., 11:1442-1451.
Penduff, T., Barnier, B., Verron, J., and Kerbiriou, M. A. (2002). How topographic
smoothing contributes to differentiating the eddy flows simulated by sigma and
z-level models. J. Phys. Oceanogr., 32:122-137.
Phillips, 0. M. (1972). Turbulence in a strongly stratified fluid - is it unstable? Deep
Sea Res., 19:7%81.
Plumb, R. A. and Mahlman, J. D. (1987). The zonally averaged transport characteristics of the gfdl general circulation/transport model. J. Atmos. Sci., 44:298-327.
Price, J. F. and Yang, J. (1998). Marginal sea overflows for climate simulations. In
Ocean Modeling and Parameterization, volume 516 of NATO Science series C,
pages 155-170. Kluwer Academic Publishers.
Rhines, P. B. (1977). The dynamics of unsteady currents, volume 6 of Marine Modelling, The Sea, pages 189-318. Wiley.
Riviere, P., Treguier, A. M., and Klein, P. (2004). Effects of bottom friction on nonlinear equilibration of an oceanic baroclinic jet. J. Phys. Oceanogr., 34:41&432.
Roberts, M. and Marshall, D. (1998). Do we require adiabatic dissipation schemes in
eddy-resolving ocean models? J. Phys. Oceanogr., 28:205&2063.
Ruddick, B. R., McDougall, T. J., and Turner, J. S. (1989). The formation of layers
in a uniformly stirred density gradient. Deep Sea Res., 36:597409.
Schmitt, R. W. (1998). Doublediffusive convection. In Ocean Modeling and Pammeterization, volume 516 of NATO Science series C, pages 215-234. Kluwer Academic
Publishers.
Send, U. and Kase, R. H. (1998). Parameterization of processes in deep convection
regimes. In Ocean Modeling and Parameterization, volume 516 of NATO Science
series C, pages 191-214. Kluwer Academic Publishers.
Shchepetkin, A. F. and McWilliams, J. C. (1998). Quasi-monotone advection schemes
based on explicit locally adaptative dissipation. Monthly Weather Review, 126:15411580.
Siegel, A., Weiss, J. B., Toomre, J., McWilliams, J. C., Berloff, P. S., and Yavneh, I.
(2001). Eddies and vortices in ocean basin dynamics. Geophys. Res. Lets., 28:31833186.
Simmons, H. L., Jayne, S. R., Laurent, L. C. St., and Weaver, A. J. (2004). Tidally
driven mixing in a numerical model of the ocean general circulation. Ocean Modelling, 6:245-263.
Smagorinsky, J. (1963). General circulation experiments with the primitive equations:
I. the basic experiment. Monthly Weather Review, 91:9%164.
Smith, R. D., Maltrud, M. E., Bryan, F. O., and Hecht, M.W. (2000). Simulation of
the north atlantic ocean at 1/10'. J. Phys. Oceanogr., 30:1532-1561.
Smith, R. D. and McWilliams, J. C. (2003). Anisotropic horizontal viscosity for ocean
models. Ocean Modelling, 5:129-156.
Speer, K., Guilyardi, E., and Madec, G. (2000). Southern ocean transformation in a
coupled model with and without eddy mass fluxes. Tellus, 52A:554-565.
Stratford, K. and Haines, K (2000). Frictional sinking of the dense water overflow in
a z-coordinate ogcm of the mediterranean sea. Geophys. Res. Lets., 27:3973-3976.
Toole, J. M. (1998). Turbulent mixing in the ocean. In Ocean Modeling and Pammeterization, volume 516 of NATO Science series C, pages 171-190. Kluwer Academic
Publishers.
Merryfield, W. J., Holloway, G., and Gargett, A. E. (1999). A global ocean model
with doublediffusive mixing. J. Phys. Oceanogr., 29:1124-1142.
Pacanowski, R. C. and Philander, S. G. H. (1981). Parameterization of vertical mixing
in numerical models of the tropical ocean. J. Phys. Oceanogr., 11:1442-1451.
Penduff, T., Barnier, B., Verron, J., and Kerbiriou, M. A. (2002). How topographic
smoothing contributes to differentiating the eddy flows simulated by sigma and
z-level models. J. Phys. Oceanogr., 32:122-137.
Phillips, 0. M. (1972). Turbulence in a strongly stratified fluid - is it unstable? Deep
Sea Res., 19:7%81.
Plumb, R. A. and Mahlman, J. D. (1987). The zonally averaged transport characteristics of the gfdl general circulation/transport model. J. Atmos. Sci., 44:298-327.
Price, J. F. and Yang, J. (1998). Marginal sea overflows for climate simulations. In
Ocean Modeling and Parameterization, volume 516 of NATO Science series C,
pages 155-170. Kluwer Academic Publishers.
Rhines, P. B. (1977). The dynamics of unsteady currents, volume 6 of Marine Modelling, The Sea, pages 189-318. Wiley.
Riviere, P., Treguier, A. M., and Klein, P. (2004). Effects of bottom friction on nonlinear equilibration of an oceanic baroclinic jet. J. Phys. Oceanogr., 34:41&432.
Roberts, M. and Marshall, D. (1998). Do we require adiabatic dissipation schemes in
eddy-resolving ocean models? J. Phys. Oceanogr., 28:205&2063.
Ruddick, B. R., McDougall, T. J., and Turner, J. S. (1989). The formation of layers
in a uniformly stirred density gradient. Deep Sea Res., 36:597409.
Schmitt, R. W. (1998). Doublediffusive convection. In Ocean Modeling and Pammeterization, volume 516 of NATO Science series C, pages 215-234. Kluwer Academic
Publishers.
Send, U. and Kase, R. H. (1998). Parameterization of processes in deep convection
regimes. In Ocean Modeling and Parameterization, volume 516 of NATO Science
series C, pages 191-214. Kluwer Academic Publishers.
Shchepetkin, A. F. and McWilliams, J. C. (1998). Quasi-monotone advection schemes
based on explicit locally adaptative dissipation. Monthly Weather Review, 126:15411580.
Siegel, A., Weiss, J. B., Toomre, J., McWilliams, J. C., Berloff, P. S., and Yavneh, I.
(2001). Eddies and vortices in ocean basin dynamics. Geophys. Res. Lets., 28:31833186.
Simmons, H. L., Jayne, S. R., Laurent, L. C. St., and Weaver, A. J. (2004). Tidally
driven mixing in a numerical model of the ocean general circulation. Ocean Modelling, 6:245-263.
Smagorinsky, J. (1963). General circulation experiments with the primitive equations:
I. the basic experiment. Monthly Weather Review, 91:9%164.
Smith, R. D., Maltrud, M. E., Bryan, F. O., and Hecht, M.W. (2000). Simulation of
the north atlantic ocean at 1/10'. J. Phys. Oceanogr., 30:1532-1561.
Smith, R. D. and McWilliams, J. C. (2003). Anisotropic horizontal viscosity for ocean
models. Ocean Modelling, 5:129-156.
Speer, K., Guilyardi, E., and Madec, G. (2000). Southern ocean transformation in a
coupled model with and without eddy mass fluxes. Tellus, 52A:554-565.
Stratford, K. and Haines, K (2000). Frictional sinking of the dense water overflow in
a z-coordinate ogcm of the mediterranean sea. Geophys. Res. Lets., 27:3973-3976.
Toole, J. M. (1998). Turbulent mixing in the ocean. In Ocean Modeling and Pammeterization, volume 516 of NATO Science series C, pages 171-190. Kluwer Academic
Publishers.