Clouds float because the tiny water droplets within them have a terminal velocity close to zero, allowing them to be supported by rising air currents. When these droplets grow larger, they eventually fall as rain. The discussion also touches on the presence of ice crystals in clouds, which may have a larger surface area to mass ratio, potentially aiding in their buoyancy. Additionally, there is curiosity about the movement of air molecules during storms, questioning whether they are pushed across the continent or simply move temporarily with the storm front. Overall, the complexities of cloud formation and behavior are acknowledged, indicating varying conditions across different types of clouds.