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Coriolis force |
Also found in: Encyclopedia, Wikipedia, Hutchinson | 0.04 sec. |
Coriolis force [ˌkɒrɪˈəʊlɪs] n (Astronomy) a fictitious force used to explain a deflection in the path of a body moving in latitude relative to the earth when observed from the earth. The deflection (Coriolis effect) is due to the earth's rotation and is to the east when the motion is towards a pole [named after Gaspard G. Coriolis (1792-1843), French civil engineer]
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Notice, especially from (2), that the geostrophic wind is the result of a balance between two forces, pressure gradient force (PGF) and Coriolis force (CF). For example, the role of wind-driven changes includes a review of how local wind-driven currents along a coast can, via the action of the Coriolis force, change coastal sea level, but does not describe how some wind-driven effects can propagate along continental boundaries as coastally trapped waves. The coriolis force generates a torque measuring proportional to the mass flow, which is transmitted to a strain gage load cell. |
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