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44 3 Basics of Geophysical Fluid Dynamics
Fig. 3.12 Appearance of straight path (white line) of an object (ball) for an observer on a rotating
turntable. The inner end of the white line shows the starting position of the object. The SciLab
script “Straight Path.sce” in the folder “Miscellaneous/Coriolis Force” of the CD-ROM produces
an animation
3.12.2 The Centripetal Force and the Centrifugal Force
Consider an object attached to the end of a rope and spinning around with a rotating
turntable. In the f xed coordinate system, the object’s path is a circle (Fig. 3.13) and
the force that deflect the object from a straight path is called the centripetal force.
This force is directed toward the centre of rotation (parallel to the rope) and, hence,
Fig. 3.13 Left panel In the f xed frame of reference, an object attached to a rope and rotating
at the same rate as the turntable experiences only the centripetal force. Right panel: The object
appears stationary in the rotating frame of reference, which implies a balance between the centripetal force and the centrifugal force. The SciLab script “Centripetal Force.sce” in the folder
“Miscellaneous/Coriolis Force” of the CD-ROM produces an animation