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A Two-Level Wind and Buoyancy Driven Thermocline Model
Two-Level Wind Buoyancy Driven Thermocline Model
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2009/1/16
A simple two-level model is designed to simulate the “thermocline equations,” applicable for large-scale steady oceanic flow. The model serves two functions. First, it replaces problems with the inter...
Matching a Ventilated Thermocline Model with Inertial Western Boundary Currents
Ventilated Thermocline Model Inertial Western Boundary Currents western boundary region
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2008/12/30
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 Continuously Stratified Thermocline Model Incorporating a Mixed Layer of Variable Thickness and Density
continuously stratified thermocline model variable depth
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2008/12/24
A continuously stratified, steady thermocline model is formulated in which a mixed layer of variable depth and density overlies a stratified thermocline. Rather than prescribe the distribution of dens...
Stationary Shock Fronts in a Continuously Stratified Thermocline Model
Stationary Shock Fronts Thermocline Model
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2008/12/12
Fronts are ubiquitous in the ocean. Recent work by Dewar has considered the formation of oceanic fronts in a simple layered model.
In this contribution, the position and structure of similar fronts...