In the Southern Hemisphere, how do winds behave around surface highs?

In the Southern Hemisphere, winds around surface high-pressure systems flow clockwise and outward. This phenomenon occurs due to the Coriolis effect, which influences the direction of wind flow based on the rotation of the Earth. In high-pressure areas, air moves away from the center of the high in a rotating manner, and the Coriolis effect causes this outward flow to shift to the right relative to the motion. As a result, the winds spiral out from the high-pressure center in a clockwise direction.

It is helpful to note that in high-pressure systems, the air is typically descending and creating clear skies, leading to fair weather, which is further influenced by the outward movement of winds. Understanding this behavior is essential for interpreting weather patterns and forecasting in the Southern Hemisphere.