Shelf-Break Fronts are a process by which stratification of the water column occurs. This stratification normally results in thermoclines, since they occur where a sudden change in water depth causes a constriction of the current flow. They can be expressed as a ratio of their potential energy due to maintaining mixed (non-stratified) conditions, to the dissipated energy produced by the current being forced across the sudden change in depth. This can be expressed as:
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