Coriolis Effect - Research Article from World of Earth Science

This encyclopedia article consists of approximately 2 pages of information about Coriolis Effect.

Coriolis Effect - Research Article from World of Earth Science

This encyclopedia article consists of approximately 2 pages of information about Coriolis Effect.
This section contains 566 words
(approx. 2 pages at 300 words per page)
Buy the Coriolis Effect Encyclopedia Article

The Coriolis effect (sometimes called the Coriolis force) is the apparent deflection of air masses and fluids caused by Earth's rotation. Named after the French mathematician Gustave-Gaspard Coriolis, (1792-1843), who developed the concept in 1835, the Coriolis force is a pseudoforce (false force) and should properly be termed the Coriolis effect. As a result of the Coriolis effect, there is an apparent deflection of all matter in motion to the right of their path in the Northern Hemisphere, and to the left in the Southern Hemisphere. In the Northern Hemisphere, air is deflected counterclockwise (to right of its established path of motion) as it moves inward toward a low-pressure area (zone of convergence). In the Northern Hemisphere, air is deflected clockwise (again, to the right of its established path of motion) as it moves outward toward a low-pressure area (zone of convergence). These deflections and rotations are...

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This section contains 566 words
(approx. 2 pages at 300 words per page)
Buy the Coriolis Effect Encyclopedia Article
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