OCEAN MODELS
Blanke, B. and Deleduse, P. (1993). Variability of the tropical atlantic ocean simulated
by a general circulation model with two different mixed layer physics. J. Phys.
Ocennogr., 23:1363-1388.
Bleck, R. and Boudra, D. B. (1981). Initial testing of a numerical circulation model
using a hybrid- (quasi-isopycnic) vertical coordinate. J. Phys. Ocennogr., 11355770.
Boer, G. J. and Denis, B. (1997). Numerical convergence of a gcm. Climate dynamics,
13:35!%374.
Bower, A. S., Cann, B. Le, Rhssby, T., Zenk, W., Gould, J., Speer, K., Richardson, P. L., Prater, M. D., and Zhang, H. M. (2002). Directly-measured mid-depth
circulation in the northeastern north atlantic ocean. Natuw, 419 (6907):603-607.
Chanut, J. (2003). Param6trimtion de la restratifidion a p r h convection pmfonde en
mer du Labrador. PhD thesis, universit6 Joseph Fourier, Grenoble, France.
Chanut, J. and Molines, J. M. (2004). Implementation et validation du modhle kpp
dans opa8.1. Rapport technique, LEGI, Grenoble.
Chassignet, E. and Verron, J., editors (1998). Ocenn Modeling and Parameterization,
volume 516 of NATO Science series C. Kluwer Academic Publishers, Cambridge.
Cox, M. D. (1984). A primitive equation, Sdimensional model of the ocean. Technical
Report 1, Geophysical Fluid Dynamics Laboratory, PO Box 308, Princeton, New
Jersey, 08542.
Dengg, J., Boning, C., E r s t , U., Redler, R., and Beckmann, A. (1999). Effects of
improved model representation of overflow water on the subpolar north atlantic.
WOCE Newsletter, 37.
Dengler, M., Schott, F., Eden, C., Brandt, P., Fischer, J., and Zantopp, R. J. (2004).
New mechanisms for deep water transport. Nature. In press.
Dubos, T. and Babiano, A. (2002). Two-dimensional cascades and mixing: a physical
space approach. J. Fluid. Mech., 467:81-100.
Gent, P. R. and McWilliams, J. C. (1990). Isopycnal mixing in ocean circulation model.
J. Phys. Ocennogr., 20:15&155.
Gent, P. R., Willebrand, J., McDougall, T. J., and McWilliams, J. C. (1995). Parameterizing eddy-induced tracer transports in ocean circulation models. J. Phys.
Ocennogr., 25463474.
Gerdes, R. (1993). A primitive equation ocean circulation model using a general vertical coordinate transformation. J. Gwphys. Res., 98:14683-14701.
Gordon, C., Cooper, C., Senior, C. A,, Banks, H., Gregory, J. M., Johns, T. C.,
Mitchell, J. F. B., and Woods, R. A. (2000). The simulation of ast, sea ice extents
and ocean heat transports in a version of the hadley centre coupled model without
flux adjustments. Climate Dynamics, 16:147-168.
Griflies, S. M. (2004). findamentala of ocean climate models. Princeton University
Press, Princeton, U S A .
Griffies, S. M., Boenjng, C., Bryan, F.O., Chaesignet, E. P, Gerdes, R., Hasumi, H.,
Hirst, A,, Tregxier, A. M, and Webb, D. (2000a). Developments in ocean climate
modelling. Ocean Modelling, 2123-192.
Griflies, S. M., Gnanadesikan, A,, Pacanowski, R. C., Larichev, V. D., Dukowicz,
J. K., and Smith, R. D. (1998). Isoneutral diffusion in a z-coordinate ocean model.
J. Phys. Ocennogr., 28:805-830.
Griflies, S. M. and Hallberg, R. W. (2000). Biharmonic friction with a smagorinskylike v k x i t y for use in large scale eddy-permitting ocean models. Monthly Weather
Review, 128:2935-2946.
Blanke, B. and Deleduse, P. (1993). Variability of the tropical atlantic ocean simulated
by a general circulation model with two different mixed layer physics. J. Phys.
Ocennogr., 23:1363-1388.
Bleck, R. and Boudra, D. B. (1981). Initial testing of a numerical circulation model
using a hybrid- (quasi-isopycnic) vertical coordinate. J. Phys. Ocennogr., 11355770.
Boer, G. J. and Denis, B. (1997). Numerical convergence of a gcm. Climate dynamics,
13:35!%374.
Bower, A. S., Cann, B. Le, Rhssby, T., Zenk, W., Gould, J., Speer, K., Richardson, P. L., Prater, M. D., and Zhang, H. M. (2002). Directly-measured mid-depth
circulation in the northeastern north atlantic ocean. Natuw, 419 (6907):603-607.
Chanut, J. (2003). Param6trimtion de la restratifidion a p r h convection pmfonde en
mer du Labrador. PhD thesis, universit6 Joseph Fourier, Grenoble, France.
Chanut, J. and Molines, J. M. (2004). Implementation et validation du modhle kpp
dans opa8.1. Rapport technique, LEGI, Grenoble.
Chassignet, E. and Verron, J., editors (1998). Ocenn Modeling and Parameterization,
volume 516 of NATO Science series C. Kluwer Academic Publishers, Cambridge.
Cox, M. D. (1984). A primitive equation, Sdimensional model of the ocean. Technical
Report 1, Geophysical Fluid Dynamics Laboratory, PO Box 308, Princeton, New
Jersey, 08542.
Dengg, J., Boning, C., E r s t , U., Redler, R., and Beckmann, A. (1999). Effects of
improved model representation of overflow water on the subpolar north atlantic.
WOCE Newsletter, 37.
Dengler, M., Schott, F., Eden, C., Brandt, P., Fischer, J., and Zantopp, R. J. (2004).
New mechanisms for deep water transport. Nature. In press.
Dubos, T. and Babiano, A. (2002). Two-dimensional cascades and mixing: a physical
space approach. J. Fluid. Mech., 467:81-100.
Gent, P. R. and McWilliams, J. C. (1990). Isopycnal mixing in ocean circulation model.
J. Phys. Ocennogr., 20:15&155.
Gent, P. R., Willebrand, J., McDougall, T. J., and McWilliams, J. C. (1995). Parameterizing eddy-induced tracer transports in ocean circulation models. J. Phys.
Ocennogr., 25463474.
Gerdes, R. (1993). A primitive equation ocean circulation model using a general vertical coordinate transformation. J. Gwphys. Res., 98:14683-14701.
Gordon, C., Cooper, C., Senior, C. A,, Banks, H., Gregory, J. M., Johns, T. C.,
Mitchell, J. F. B., and Woods, R. A. (2000). The simulation of ast, sea ice extents
and ocean heat transports in a version of the hadley centre coupled model without
flux adjustments. Climate Dynamics, 16:147-168.
Griflies, S. M. (2004). findamentala of ocean climate models. Princeton University
Press, Princeton, U S A .
Griffies, S. M., Boenjng, C., Bryan, F.O., Chaesignet, E. P, Gerdes, R., Hasumi, H.,
Hirst, A,, Tregxier, A. M, and Webb, D. (2000a). Developments in ocean climate
modelling. Ocean Modelling, 2123-192.
Griflies, S. M., Gnanadesikan, A,, Pacanowski, R. C., Larichev, V. D., Dukowicz,
J. K., and Smith, R. D. (1998). Isoneutral diffusion in a z-coordinate ocean model.
J. Phys. Ocennogr., 28:805-830.
Griflies, S. M. and Hallberg, R. W. (2000). Biharmonic friction with a smagorinskylike v k x i t y for use in large scale eddy-permitting ocean models. Monthly Weather
Review, 128:2935-2946.