How does upper air in anticyclones circulate in the Northern Hemisphere?

In the Northern Hemisphere, the circulation of upper air in anticyclones is characterized by a clockwise movement. This phenomenon is primarily due to the Coriolis effect, which arises from the rotation of the Earth. As air flows outward from the center of high pressure (the anticyclone), it is deflected to the right, resulting in a clockwise pattern.

This behavior is distinctly different from cyclones, where the air circulates counterclockwise in the Northern Hemisphere. An understanding of the pressure systems and how they influence wind patterns is crucial for meteorology, as these patterns affect weather conditions significantly. Therefore, recognizing that anticyclones create a clockwise circulation helps to explain various atmospheric phenomena associated with high-pressure systems.