The Coriolis force is an apparent force that results from the rotation of the Earth on its axis. It affects the movement of air masses, ocean currents, and other moving objects over the Earth's surface. Although it is not a real force in the physical sense, it appears because the Earth rotates beneath moving objects. The Coriolis force causes moving bodies to be deflected to the right in the Northern Hemisphere and to the left in the Southern Hemisphere. Its magnitude increases with the speed of the moving object and with latitude, becoming zero at the Equator and maximum at the poles. This force plays a vital role in determining global wind circulation, cyclone rotation, ocean current patterns, and weather systems. It does not alter the speed of moving air but changes its direction, thereby influencing atmospheric circulation. The horizontal pressure distribution on the Earth refers to the variation of atmospheric pressure from one place to another across the Earth's surface. It is controlled by factors such as temperature, altitude, Earth's rotation, the unequal distribution of land and water, and seasonal changes. Differences in atmospheric pressure create pressure gradients, which are responsible for the movement of air from high-pressure areas to low-pressure areas, resulting in the formation of winds. The Earth exhibits a systematic pattern of