The vector formula for the magnitude and direction of the Coriolis acceleration is derived through vector analysis and is
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:The Coriolis acceleration ( and hence the Coriolis force ) only exists when using polar co-ordinates.
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The pressure gradient force is represented by blue arrows, the Coriolis acceleration ( always perpendicular to the velocity ) by red arrows
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The Coriolis acceleration is perpendicular to the longitudinal flight path and will be of the same magnitude for northbound and southbound flights.
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In the micromechanical type, the Coriolis acceleration is measured by a micro-mechanical capacitive acceleration sensor placed on an oscillating element.
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The pressure-gradient force is represented by blue arrows, the Coriolis acceleration ( always perpendicular to the velocity ) by red arrows
7.
The asymmetry between the prograde and retrograde satellites can be explained very intuitively by the Coriolis acceleration in the frame rotating with the planet.
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When considering atmospheric or oceanic dynamics, the vertical velocity is small, and the vertical component of the Coriolis acceleration is small compared to gravity.
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At the synoptic scale, the Coriolis acceleration acting on moving air masses ( outside of the tropics ), plays a dominant role in predictions.
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For the acceleration, is the centripetal acceleration and } } the Coriolis acceleration, in addition to the radial acceleration } } and angular acceleration.
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