The Coriolis Effect is a phenomenon that occurs due to the rotation of the Earth. As the Earth spins on its axis from west to east, moving objects, such as air or water currents, are deflected to the right in the Northern Hemisphere and to the left in the Southern Hemisphere. This deflection is caused by the difference in rotational speed at different latitudes. The Coriolis Effect has a significant impact on weather patterns and ocean currents. In the Northern Hemisphere, winds in high pressure systems spiral clockwise and winds in low pressure systems spiral counterclockwise. In the Southern Hemisphere, the opposite is true. Additionally, ocean currents are also influenced by the Coriolis Effect. In the Northern Hemisphere, currents tend to flow to the right of their intended direction, while in the Southern Hemisphere, they flow to the left. This can lead to the formation of gyres, or large circulating ocean currents. Overall, the Coriolis Effect is an important concept in understanding global weather patterns and ocean circulation. It helps explain why certain phenomena occur the way they do and how they impact the Earth's climate and environment.