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A simple theoretical model for the oceanic thermocline and the associated field of current is presented. The model consists of a finite but arbitarily large number of inviscid, homogeneous fluid layer...
A model of cross-gyre geostrophic flow is presented. It is a two-layer model of the (Northern Hemisphere) subtropical thermocline above a resting lower ocean. The northern boundary of the gyre is take...
A steady state numerical solution is found for an idealized, rectangular ocean basin driven by wind and surface buoyancy flux. A three-dimensional primitive equation model is used. In agreement ...
A three-dimensional, primitive equation numerical model is used to study the effects of mesoscale eddies within the subtropical thermocline. Solutions are obtained for an ocean bounded by idealized to...
An analytical study of the combined wind-driven and buoyancy-driven thermocline problem is presented. The analysis is an extension of the ventilated thermocline model of Luyten et al. An exact solu...
Three exact, closed-form analytical solutions for the subtropical gyre are presented for the ideal fluid thermocline equations. Specifically, the flow is exactly geostrophic, hydrostatic, and mass and...
A primitive equation, eddy-resolving numerical model is used to study the inherent time scales of variability in the subtropical ocean, assuming temporally constant surface forcing. Three primary scal...
Air–Sea interaction influences the ventilated thermocline by forcing the mixed layer to deepen and cool poleward. When there is flow from the mixed layer into the interior, the mixed-layer depth and d...
A two-layered ventilated thermocline model is matched with inertial western boundary currents in the southern part of the western boundary region. For general cases the western boundary currents break...
A model of the ventilated thermocline consisting of three adiabatic layers surmounted by a mixed layer of finite thickness is presented. The mixed-layer depth density increase continuously northward, ...
The time dependence of the ventilated thermocline is examined via analytical and numerical means. The original Henderschott model is modified such that the outcrops all occur on the same geopotential ...
The mixed layer thickness generally increases in the northward direction, but its change seems to occur rather sharply in a narrow transition zone, referred to as a mixed layer front here. The author ...
Climate variability of a layered model of the ventilated thermocline is studied. Assuming the Ekman pumping is unchanged, cooling (heating) causes a southward (northward) shift of the outcrop line and...
Climate variability induced by surface cooling in a four-moving-layer model of the ventilated thermocline is studied. The perturbations propagate within the characteristic cones defined by streamlines...
A two-moving-layer model is used to examine the structure of the equatorial thermocline and its connection with the extratropical thermocline. It is found that cooling (warming) in extratropics genera...

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