The convection pattern between thirty degrees south and thirty degrees north latitude is known as the Hadley Cell. In this region, warm air rises near the equator, creating a low-pressure area and leading to the formation of thunderstorms and rain. As the air rises, it eventually cools and descends back towards the surface around 30 degrees latitude, creating a high-pressure area and resulting in dry conditions. This circulation pattern is driven by the Earth's rotation and the uneven heating of the Earth's surface by the sun.
