File:Geostrophic current.pdf
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Geostrophic_current.pdf (0 × 0 pixels, file size: 27 KB, MIME type: application/pdf)
Summary
Schematic of geostrophic flow. The pressure gradient force (PGF) acts from high to low pressure. The Coriolis force is directed in the direction opposite to the PGF. The resulting Geostrophic flow is a balance between the PGF and the Coriolis force.
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Date/Time | Dimensions | User | Comment | |
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current | 09:24, 9 January 2017 | 0 × 0 (27 KB) | 127.0.0.1 (talk) | Schematic of geostrophic flow. The pressure gradient force (PGF) acts from high to low pressure. The Coriolis force is directed in the direction opposite to the PGF. The resulting Geostrophic flow is a balance between the PGF and the Coriolis force. |
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