Scorching air is the precursor to thunderstorms. This often occurs following prolonged heat spells, resembling heatwaves, throughout which extraordinarily excessive temperatures warmth the Earth and the environment.
Heat air rises by means of the environment, begins to chill, and condenses into droplets of water because it ascends.
When these droplets start to maneuver inside the cloud, they may ascend even larger into the environment if the encircling air is chilly.
Because the environment is unstable, cumulonimbus clouds – the one type of cloud that may produce hail, thunder, and lightning – are fashioned throughout thunderstorms.