Abstract:[1] The disruption of an arrested bottom Ekman layer on a lake boundary slope is initiated when buoyancy enters the balance between the Coriolis force and the pressure gradient. This process is shown to behave in a lake in a qualitatively similar manner to the ocean. A greater bottom slope and stronger stratification are found to dramatically shorten the shutdown timescale of the Ekman flux compared to typical values on the continental shelf and slope. Convergence of the flow at the density front, where the th… Show more
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