Chapter 4 Ekman layer transports, Ekman pumping, and the Sverdrup balance Geostrophic flow, or the flow produced by a balance between the pressure gradient force and the Coriolis force, is frictionless flow. But momentum

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Date: 2006-08-17 03:26:18		Chapter 4 Ekman layer transports, Ekman pumping, and the Sverdrup balance Geostrophic flow, or the flow produced by a balance between the pressure gradient force and the Coriolis force, is frictionless flow. But momentum Add to Reading List Source URL: gaea.es.flinders.edu.au Download Document from Source Website File Size: 1,64 MB Share Document on Facebook