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Migration highway - PowerPoint PPT Presentation

Processes at the shelf edge.

Processes at the shelf edge. At the shelf edge: The current speed can vary with depth, but the direction of the current is always along the isobaths. This assumes a linear, steady, frictionless flow; i.e. a geostrophic flow cannot move across the shelf slope or shelf edge.

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Migration highway - PowerPoint PPT Presentation

Processes at the shelf edge.