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The Coriolis effect describes the pattern of deflection taken by objects not firmly connected to the ground as they travel long distances around Earth. The Coriolis effect is responsible for many large-scale weather patterns. The key to the Coriolis effect lies in Earth’s rotation.
Named after the French mathematician Gaspard Gustave de Coriolis (born in 1792), the Coriolis Effect refers to the curved path that objects moving on Earth’s surface appear to follow because of the spinning of the planet.
The Coriolis effect is a natural event in which objects seem to get deflected while traveling around and above Earth. The planet Earth is constantly rotating, or spinning, from west to east. Every 24 hours, it completes a full rotation. This rotation causes the Coriolis effect.
The Coriolis effect describes how objects that are not connected to the ground seem to get . deflected as they travel long distances around Earth. The Coriolis effect is responsible for many large-scale weather patterns .
The Coriolis effect describes the pattern of deflection taken by objects not firmly connected to the ground as they travel long distances around the Earth.
As these currents flow westward, the Coriolis effect —a force that results from the rotation of the Earth—deflects them. The currents then bend to the right, heading north. At about 30 degrees north latitude, a different set of winds, the westerlies, push the currents back to the east, producing a closed clockwise loop.
The Coriolis effect causes equatorial-bound winds to curve to the right in the northern hemisphere and to the left in the southern hemisphere. This is the reason why hurricanes in the northern hemisphere rotate counterclockwise, but in the southern hemisphere, they rotate clockwise.
noun. movement of air (from a high pressure zone to a low pressure zone) caused by the uneven heating of the Earth by the sun. The Coriolis effect describes the pattern of deflection taken by objects not firmly connected to the ground as they travel long distances around the Earth.
The actual paths of winds—and of ocean currents, which are pushed by wind—are partly a result of the Coriolis effect. The Coriolis effect is named after Gustave Coriolis, the 19th-century French mathematician who first explained it. The key to the Coriolis effect lies in the Earth’s rotation.
Ocean currents are the continuous, predictable, directional movement of seawater driven by gravity, wind (Coriolis Effect), and water density. Ocean water moves in two directions: horizontally and vertically.