Tornadoes form when a strong downdraft of cool air interacts with an updraft of warm air, creating a vortex that extends downward from the storm cloud. The inward airflow at the base of the tornado compresses, causing the vortex to descend rather than ascend. This phenomenon is similar to how whirlpools form in water, where the vortex appears to grow downward due to the dynamics of fluid motion. The discussion highlights that while tornadoes are often thought to be purely upward phenomena, their formation involves complex interactions of air currents. Understanding these dynamics is crucial for grasping why tornadoes develop as they do.