These simulations were run using the leading - edge, high -
resolution global ocean circulation model, NEMO.
Not exact matches
«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.
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.