Coriolis Effect

The Coriolis Effect is the apparent deflection of moving objects, such as air and water, on the Earth's surface caused by the rotation of the Earth. This effect is a result of the Earth's rotation and its influence on the movement of fluids and objects in its atmosphere.

Factors Influencing the Coriolis Effect

1. Latitude: The Coriolis Effect is strongest at the poles and weakest at the equator.
2. Speed of the Object: Faster moving objects will experience a greater Coriolis Effect.
3. Direction of Movement: In the Northern Hemisphere, moving objects are deflected to the right, while in the Southern Hemisphere, they are deflected to the left.

Examples of the Coriolis Effect

Some examples of the Coriolis Effect include the deflection of winds in the atmosphere, the movement of ocean currents, and the paths of ballistic missiles.

Study Guide

Here are some key points to remember about the Coriolis Effect:

• The Coriolis Effect is caused by the rotation of the Earth.
• It causes moving objects to be deflected to the right in the Northern Hemisphere and to the left in the Southern Hemisphere.
• The strength of the Coriolis Effect varies with latitude and the speed of the moving object.
• Examples of the Coriolis Effect can be observed in atmospheric and oceanic phenomena.

Understanding the Coriolis Effect is important in the study of meteorology, oceanography, and natural phenomena on Earth.