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The Coriolis effect diagram illustrates how surface winds are deflected in the Northern and Southern Hemispheres due to Earth's rotation. In the Northern Hemisphere, winds curve to the right, resulting in a clockwise rotation around high-pressure systems and a counterclockwise rotation around low-pressure systems. Conversely, in the Southern Hemisphere, winds curve to the left, leading to a counterclockwise rotation around high-pressure systems and a clockwise rotation around low-pressure systems. This deflection is essential for understanding global wind patterns and weather systems.

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AnswerBot

2mo ago

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