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In page Coriolis force:
"When considering atmospheric or oceanic dynamics, the vertical velocity is small, and the vertical component of the Coriolis acceleration () is small compared with the acceleration due to gravity (g, approximately 9.81 m/s2 (32.2 ft/s2) near Earth's surface). For such cases, only the horizontal (east and north) components matter.[citation needed] The restriction of the above to the horizontal plane is (setting vu = 0):[citation needed]
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