boa_co said:
O.K. It's a bit more clear now. But where does the Coriolis Effect come from then?
It's practical to first discuss two effects separately, and later combine them again.
- There is the case of tangential velocity (with respect to the rotating system), but no radial velocity. Then you get the effect that is the subject of the
https://www.physicsforums.com/showthread.php?t=393932" that DH pointed out in an earlier message.
- There is the case of radial velocity, but no tangential velocity (initially).
In the case where the centripetal force is
precisely enough to sustain the circumnavigating motion there is no radial velocity. To have some inward/outward radial velocity there needs to be a either a surplus of centripetal force, or not enough of it.
The left hand side of the animation shows an object moving along an ellipse-shaped trajectory. A centripetal force sustains that trajectory, the animation depicts the case where the strength of the centripetal force is proportional to the distance to the central point.
Interestingly, the ellipse-shaped trajectory can be thought of as decomposed in a circle and an epi-circle.
The right hand side of the animation shows what the motion looks like as seen from a point of view that is rotating with constant angular velocity. As you can see the animation combines the cases of motion in radial direction and motion in tangential direction.
When a mass has a velocity with respect to the rotating system there is a tendency to deflect. This tendency to deflect is equally strong in all directions.