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E. Maier‐Reimer, U. Mikolajewicz, K. Hasselmann (1993)
Mean Circulation of the Hamburg LSG OGCM and Its Sensitivity to the Thermohaline Surface ForcingJournal of Physical Oceanography, 23
J. Marotzke (1997)
Boundary Mixing and the Dynamics of Three-Dimensional Thermohaline CirculationsJournal of Physical Oceanography, 27
K. Bryan, L. Lewis (1979)
A water mass model of the world ocean circulation
J. Boris, D. Book (1973)
Flux-corrected transport. I. SHASTA, a fluid transport algorithm that worksJournal of Computational Physics, 11
A. Weaver, M. Eby (1997)
On the Numerical Implementation of Advection Schemes for Use in Conjunction with Various Mixing Parameterizations in the GFDL Ocean ModelJournal of Physical Oceanography, 27
M. Gregg (1989)
Scaling turbulent dissipation in the thermoclineJournal of Geophysical Research, 94
W. Holland, Julian Chow, F. Bryan (1998)
Application of a Third-Order Upwind Scheme in the NCAR Ocean Model*Journal of Climate, 11
K. Bryan (1997)
A Numerical Method for the Study of the Circulation of the World OceanJournal of Computational Physics, 135
R. Rood (1987)
Numerical advection algorithms and their role in atmospheric transport and chemistry modelsReviews of Geophysics, 25
M. Hecht, W. Holland, P. Rasch (1995)
Upwind‐weighted advection schemes for ocean tracer transport: An evaluation in a passive tracer contextJournal of Geophysical Research, 100
B. Leonard (1990)
A stable and accurate convective modelling procedure based on quadratic upstream interpolationComputer Methods in Applied Mechanics and Engineering, 19
P. Smolarkiewicz (1984)
A Fully Multidimensional Positive Definite Advection Transport Algorithm with Small Implicit DiffusionJournal of Computational Physics, 54
(1987)
Isopycnal diffusion in a z-coordinate ocean model. Ocean Modelling (unpublished manuscripts
H. Tsujino, N. Suginohara (1998)
Thermohaline effects on upper layer circulation of the North PacificJournal of Geophysical Research, 103
P. Gent, J. McWilliams (1990)
Isopycnal mixing in ocean circulation modelsJournal of Physical Oceanography, 20
(1994)
Available from National Aeronautical and Space Administration, Washington, DC 205460001
H. Tsujino, N. Suginohara (1999)
Thermohaline Circulation Enhanced by Wind ForcingJournal of Physical Oceanography, 29
K. Polzin, J. Toole, J. Ledwell, R. Schmitt (1997)
Spatial Variability of Turbulent Mixing in the Abyssal Ocean, 276
W. Schmitz (1995)
On the interbasin‐scale thermohaline circulationReviews of Geophysics, 33
A. Hirst, W. Cai (1994)
Sensitivity of a World Ocean GCM to Changes in Subsurface Mixing ParameterizationJournal of Physical Oceanography, 24
S. Hellerman, M. Rosenstein (1983)
Normal Monthly Wind Stress Over the World Ocean with Error EstimatesJournal of Physical Oceanography, 13
G. Danabasoglu, J. McWilliams, W. Large (1996)
Approach to Equilibrium in Accelerated Global Oceanic Models.Journal of Climate, 9
M. Hecht, F. Bryan, W. Holland (1998)
A consideration of tracer advection schemes in a primitive equation ocean modelJournal of Geophysical Research, 103
B. Leonard, M. Macvean, A. Lock (1994)
The Flux-integral Method for Multidimensional Convection and DiffusionApplied Mathematical Modelling, 19
R. Gerdes, C. Köberle, J. Willebrand (1991)
The influence of numerical advection schemes on the results of ocean general circulation modelsClimate Dynamics, 5
N. Suginohara, S. Aoki (1991)
Buoyancy-driven circulation as horizontal convection on β-planeJournal of Marine Research, 49
K. Bryan (1984)
Accelerating the Convergence to Equilibrium of Ocean-Climate ModelsJournal of Physical Oceanography, 14
H. Hasumi, N. Suginohara (1999)
Atlantic deep circulation controlled by heating in the Southern OceanGeophysical Research Letters, 26
J. Ledwell, A. Watson, C. Law (1993)
Evidence for slow mixing across the pycnocline from an open-ocean tracer-release experimentNature, 364
D. Farrow, D. Stevens (1995)
A New Tracer Advection Scheme for Bryan and Cox Type Ocean General Circulation ModelsJournal of Physical Oceanography, 25
H. Nakano, R. Furue, N. Suginohara (1999)
Effect of seasonal forcing on global circulation in a world ocean general circulation modelClimate Dynamics, 15
Vertical diffusivity at the thermocline depths is now believed to be as small as 1 ×× 10 −−5 m 2 s −−1 . In order to accomplish a reliable simulation of the World Ocean for the vertical diffusivity of 1 ×× 10 −−5 m 2 s −−1 , two advective tracer transport schemes, the Uniformly Third-Order Polynominal Interpolation Algorithm (UTOPIA) of Leonard et al and the Multidimensional Positive Definite Advection Transport Algorithm (MPDATA) of Smolarkiewicz, are incorporated into an ocean general circulation model. Intercomparison is made among simulations using UTOPIA, MPDATA, and the centered differencing scheme. When UTOPIA or MPDATA is adopted, features at the thermocline depths are realistically simulated. Increase in computational cost is moderate. Circulations associated with Antarctic Bottom Water (AABW) in the Atlantic and Circumpolar Deep Water (CDW) in the Pacific are not reproduced at all for such small vertical diffusivity, although the circulation associated with North Atlantic Deep Water (NADW) has reasonable intensity. Another experiment with UTOPIA for the vertical diffusivity of 5 ×× 10 −−5 m 2 s −−1 shows that the circulation associated with NADW is relatively insensitive to vertical diffusivity, compared with the circulation associated with AABW and CDW.
Journal of Physical Oceanography – American Meteorological Society
Published: Aug 6, 1998
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