451
McGillicuddy , D. J. J., A. R. Robinson, D. A. Siegel. H. W. Jannash, R.
Johnson, T. D. Dickey, J. McNeil, A. F. Michael, and A. H. Knap, 1998:
Influence of mesoscale eddies on new production in the Sargasso Sea,
Nature, 392, 263-265.
McManus, J.P. and D. Prandle, 1994: Comparisons between observations and
model simulations of dissolved trace metal concentrations in the southem
North Sea. Marine Pollution Bulletin. 28(7),451-455.
McManus, J.P. and D. Prandle, 1996: Development of a model to reproduce
observed suspended sediment in the southem North Sea using principle component analyses with multiple linear regression. Continental Shelf Research
17(7),761-778.
McPhaden M.J. 1993 : TOGA-TAO and the 1991-1993 El Nifio/Southem Oscillation event. Oceanography, VoI. 6, No. 2: 36-44
McPhaden, M.J., 1995: The tropical atmosphere ocean array is completed. Bulletin American Meteorological Society, 75,5,739-741.
MedGOOS, 1999: Workshop: 'Benefits of the implementation of the Global
Ocean Observing System in the Mediterranean region'. 1-3 November 1999,
Rabat, Morocco. Abstracts. 54 pp.
Mellor, G.L., S.Hakkinen, T.Ezer and R.Patchen, 2001: A generalization of a
sigma coordinate ocean model and an intercomparison of model vertical
grids. This volume.
Mellor, G.L. and S. X. H. Wang, 1996: Pressure compensation and the bottom
boundary layer. Journal of Physical Oceanography, 26, 2214-2222.
Mellor, G. L. and A. F. Blumberg, 1985: Modeling Vertical and horizontal diffusivities with the sigma coordinate system. Mon Wea. Rev. 113, 1379-1383.
Mellor, G. L. and T. Yamada, 1982: Development of a turbulent closure model
for geophysical fluid problems. Rev. Geophys., 20, 851-875.
Mellor, G. L., 1991: An equation of state for numerical models of ocean and
estuaries. J. Atmos. Ocean Technol., 8, 609-61l.
Mellor, G. L., 1996: User's guide for a three-dimensional, primitive equation,
numerical ocean model. Report, Prog. in Atmos. and Ocean. Sci, Princeton
University, Princeton NJ 08540, 35 pp.
Mellor, G. L., L.-Y. Oey and T. Ezer, 1998: Sigma coordinate pressure gradient
errors and the seamount problem. J. Atmos. Oceanic. Technol., 15, 11221131.
Mellor, G. L., T. Ezer and L. Y. Oey, 1994: The pressure gradient conundrum of
sigma coordinate ocean models. J. Atmos. Oceanic. Technol., Il, 1126-1134.
Mellor, G.L. and T. Yamada, 1974: A hierarchy of turbulence closure models
for planetary boundary layers. J. Atmos. Sci., 1791-1806.
Mellor, G.L., and T. Ezer, 1991: A GulfStream model and an altimetry assimilation scheme. J. Geophys. Res., 96(C5), 8779-8795.
Mesinger, F., 1984: A blocking technique for representation of muontains in
atmospheric models. Rev. Meteor. Aeronautica, 44, 195-202.
McGillicuddy , D. J. J., A. R. Robinson, D. A. Siegel. H. W. Jannash, R.
Johnson, T. D. Dickey, J. McNeil, A. F. Michael, and A. H. Knap, 1998:
Influence of mesoscale eddies on new production in the Sargasso Sea,
Nature, 392, 263-265.
McManus, J.P. and D. Prandle, 1994: Comparisons between observations and
model simulations of dissolved trace metal concentrations in the southem
North Sea. Marine Pollution Bulletin. 28(7),451-455.
McManus, J.P. and D. Prandle, 1996: Development of a model to reproduce
observed suspended sediment in the southem North Sea using principle component analyses with multiple linear regression. Continental Shelf Research
17(7),761-778.
McPhaden M.J. 1993 : TOGA-TAO and the 1991-1993 El Nifio/Southem Oscillation event. Oceanography, VoI. 6, No. 2: 36-44
McPhaden, M.J., 1995: The tropical atmosphere ocean array is completed. Bulletin American Meteorological Society, 75,5,739-741.
MedGOOS, 1999: Workshop: 'Benefits of the implementation of the Global
Ocean Observing System in the Mediterranean region'. 1-3 November 1999,
Rabat, Morocco. Abstracts. 54 pp.
Mellor, G.L., S.Hakkinen, T.Ezer and R.Patchen, 2001: A generalization of a
sigma coordinate ocean model and an intercomparison of model vertical
grids. This volume.
Mellor, G.L. and S. X. H. Wang, 1996: Pressure compensation and the bottom
boundary layer. Journal of Physical Oceanography, 26, 2214-2222.
Mellor, G. L. and A. F. Blumberg, 1985: Modeling Vertical and horizontal diffusivities with the sigma coordinate system. Mon Wea. Rev. 113, 1379-1383.
Mellor, G. L. and T. Yamada, 1982: Development of a turbulent closure model
for geophysical fluid problems. Rev. Geophys., 20, 851-875.
Mellor, G. L., 1991: An equation of state for numerical models of ocean and
estuaries. J. Atmos. Ocean Technol., 8, 609-61l.
Mellor, G. L., 1996: User's guide for a three-dimensional, primitive equation,
numerical ocean model. Report, Prog. in Atmos. and Ocean. Sci, Princeton
University, Princeton NJ 08540, 35 pp.
Mellor, G. L., L.-Y. Oey and T. Ezer, 1998: Sigma coordinate pressure gradient
errors and the seamount problem. J. Atmos. Oceanic. Technol., 15, 11221131.
Mellor, G. L., T. Ezer and L. Y. Oey, 1994: The pressure gradient conundrum of
sigma coordinate ocean models. J. Atmos. Oceanic. Technol., Il, 1126-1134.
Mellor, G.L. and T. Yamada, 1974: A hierarchy of turbulence closure models
for planetary boundary layers. J. Atmos. Sci., 1791-1806.
Mellor, G.L., and T. Ezer, 1991: A GulfStream model and an altimetry assimilation scheme. J. Geophys. Res., 96(C5), 8779-8795.
Mesinger, F., 1984: A blocking technique for representation of muontains in
atmospheric models. Rev. Meteor. Aeronautica, 44, 195-202.