Corioliseffekti
Corioliseffekti, or the Coriolis effect, is an inertial force that acts on objects in motion relative to a rotating frame of reference. It is most commonly observed in relation to the Earth's rotation. The effect causes a deflection in the path of moving objects, appearing as if a force is pushing them sideways. In the Northern Hemisphere, this deflection is to the right of the object's path, while in the Southern Hemisphere, it is to the left.
The magnitude of the Coriolis effect depends on the speed of the object, the speed of rotation
The effect was first described by Gustave-Gaspard Coriolis in 1835. It is a crucial concept in meteorology,