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Simulation of Density-Driven Frictional Downslope Flow in Z-Coordinate Ocean Models
Z-Coordinate Ocean Models Simulation Density-Driven Frictional Downslope Flow
2008/10/23
An important component of the ocean’s thermohaline circulation is the sinking of dense water from continental shelves to abyssal depths. Such downslope flow is thought to be a consequence of bottom st...
Inclusion of Thermobaricity in Isopycnic-Coordinate Ocean Models
Inclusion of Thermobaricity Isopycnic-Coordinate Ocean Models
2008/7/22
Buoyancy anomalies caused by thermobaricity, that is, the modulation of seawater compressibility by potential temperature anomalies, underlie a long-standing argument against the use of potential-dens...