In which direction does the Coriolis effect deflect winds in the northern hemisphere?

In the northern hemisphere, the Coriolis effect causes winds to deflect to the right of their direction of motion. This phenomenon occurs due to the rotation of the Earth, which causes moving air to turn as it travels over the surface. The effect is strongest at the poles and diminishes to zero at the equator, which is why winds are not significantly affected by the Coriolis effect near the equator.

As air moves in the northern hemisphere, the rotation of the Earth influences the path of the wind, creating a right-hand turn relative to its original direction. This principle plays a crucial role in the formation of weather patterns and the direction of ocean currents. Understanding the Coriolis effect is essential for predicting weather systems and recognizing how large-scale wind patterns will behave across the globe.