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Chapter 11: Rotational Dynamics and Static Equilibrium Applications |
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The Coriolis
Effect, named after a 19th century French mathematician, describes the observed motions of objects
whose positions are recorded in a rotating coordinate system. These effects include curved
trajectories and action-reaction force pairs that show up in such accelerated systems. Consider the situation schematically illustrated in the diagram on the left. Imagine two people sitting on a rotating platform. The people are represented by the red and the green dots. We are looking down at the platform which is rotating clockwise beneath us. Relative to a X-Y coordinate system on the ground, the red dot has a tangential velocity in the positive y-direction, the blue dot has a tangential velocity in the positive x-direction.
Suppose that at the instant depicted in the diagram the person in red is instructed to throw a ball in such as a way that the person in blue could catch it a quarter of a period later, i.e. when his location would be where the white dot is now. In the ground-based frame of reference the ball has a y-velocity as indicated by the black arrow in the vector diagram. The blue person has to throw the ball in the direction indicated by the blue vector. As a result the ball will start with an initial velocity represented by the red vector in the velocity vector diagram. The magnitude of the resultant velocity has to equal the distance between the blue dot and the white dot, divided by the quarter period of rotation of the platform.
What would the path of the ball look like, as recorded in a coordinate system attached to the platform?
The two pictures below are taken from a video recording of an event similar to the ball throw described above. The first image is the instant the boy in yellow throws the ball across the merry-go-round. The second image is the later instant when the boy in red catches the ball (at his new location.)
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| throw | Catch |
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| Path in Ground System | Path in Rotating System |
Maps attached to the spinning earth are rotating frames of reference. If you impart a
northward initial velocity to a missile launched at the equator, the missile will not move along the
meridian. The meridian on the map is rotating with the spinning earth. Referenced to this the earth-based
the missile will follow a curved path. This is a real effect that has to be dealt with if the missile
is to reach the target successfully. The earthly weather is carried by the winds. These are driven by
temperature and pressure differences in the atmosphere. The air is pushed from regions of high
pressure to regions of low pressure. As the air masses move from one latitude to another, the Coriolis
effect causes their paths to curve. Thus instead of moving directly into the low pressure regions,
wind masses will circle them, forming vortices called cyclones in the northern hemisphere and typhoons
in the southern hemisphere (as depicted in the image from NASA.)
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