Abstract: The circulation of the equatorial Pacific is simulated with an implementation of the Miami Isopycnic-Coordinate Ocean Model in a Pacific basin extending from 40°N to 40°S. At a horizontal resolution of 1.25° the annual ...

Abstract: A global isopycnal coordinate GCM is used to investigate the processes that drive the meridional circulation, transformation, and interocean exchange of water masses in the Southern Ocean. The noneddy-resolving model (mesh ...