Not exact matches
These simulations were run using the leading - edge, high -
resolution global
ocean circulation model, NEMO.
The higher
resolution model better reflects the
ocean circulation and sea floor bathymetry in smaller, complex areas like the Gulf of Maine and the U.S. Northeast Shelf.
«Northwest Atlantic
Ocean may get warmer, sooner: High resolution global climate model shows much faster warming and changing ocean circulation.&r
Ocean may get warmer, sooner: High
resolution global climate
model shows much faster warming and changing
ocean circulation.&r
ocean circulation.»
Knowledge of dominant scales associated with mesoscale eddies enables a better understanding of the
resolution requirements for the Coupled
Model Intercomparison Project, the framework used for comparison of global coupled
ocean - atmosphere general
circulation models.
The weakening of the Walker
circulation arises in these
models from processes that are fundamentally different from those of El Nià ± o — and is present in both mixed - layer and full -
ocean coupled
models, so is not dependent on the
models» ability to represent Kelvin waves (by the way, most of the IPCC - AR4
models have sufficient oceanic
resolution to represent Kelvin waves and the physics behind them is quite simple — so of all the
model deficiencies to focus on this one seems a little odd).
We have used the Grid ENabled Integrated Earth system
modelling (GENIE) framework to undertake a systematic search for bi-stability of the
ocean thermohaline
circulation (THC) for different surface grids and
resolutions of 3 - D
ocean (GOLDSTEIN) under a 3 - D dynamical atmosphere
model (IGCM).
The Gulf of Mexico
circulation is examined from the results of a high -
resolution (1/12 °) North Atlantic simulation using the Miami Isopycnic Coordinate
Ocean Model.
Although
models of improved
resolution for
ocean circulation are being developed, they do not yet incorporate biogeochemical properties.
However, global
model projections have coarse
resolution, with grid cell sizes of 200 × 200 km or more, reflecting limitations of the
ocean GCM component of global coupled climate and
ocean circulation — biogeochemical
models.
Effects of tropical cyclones on
ocean heat transport in a high
resolution coupled general
circulation model.