Final answer:
Wind moves towards areas of low pressure in a high pressure outside and low pressure inside system, influenced by the Coriolis force, which causes counterclockwise rotation in the Northern Hemisphere and clockwise rotation in the Southern Hemisphere.
Step-by-step explanation:
In a system with high pressure on the outside and low pressure on the inside, such as in a tropical cyclone or hurricane, the wind will move towards the area of low pressure or the center of the system. This movement of wind is due to the pressure gradient force that drives air from regions of higher pressure to regions of lower pressure. Furthermore, the Coriolis force affects the direction of the wind flow: in the Northern Hemisphere, this deflection is to the right, causing a counterclockwise rotation around low pressure systems, while in the Southern Hemisphere, the deflection is to the left, causing a clockwise rotation.
These principles not only explain the convergence of winds towards a low-pressure center but also the characteristic patterns of weather systems in both hemispheres. The information provided here helps us understand large-scale atmospheric circulation, including the rotation and movement of air around high and low-pressure systems as well as the implications for weather and climate.