In which direction do upper air in anticyclones circulate in the Southern Hemisphere?

In anticyclones, upper air circulation is influenced by the Coriolis effect, which results from the rotation of the Earth. In the Southern Hemisphere, this effect causes the air to circulate in a counterclockwise direction. This circulation pattern occurs because the high pressure at the center of an anticyclone pushes air outward, and as the air moves away from the center, the Coriolis force deflects it to the left, resulting in a counterclockwise motion overall.

Understanding this concept is crucial for weather forecasting and analysis, as the circulation patterns associated with anticyclones can significantly impact weather conditions, such as stable weather and increased sunshine in the areas affected. The other options do not accurately reflect the behavior of air in anticyclones.