The Coriolis force is an apparent force that acts on objects moving in a rotating frame of reference, such as the Earth. It does not represent a true physical force, but rather a consequence of observing motion from a rotating perspective. Mathematically, this force causes moving objects to be deflected relative to the stationary observer, resulting in deflection to the right in the Northern Hemisphere and to the left in the Southern Hemisphere. This force plays a critical role in meteorology and oceanography, significantly influencing the large-scale patterns of global wind currents and ocean gyres, thereby contributing to the rotation and circulation of atmospheric and oceanic systems.