The formation of thermal thunderstorms is due to

Thermal thunderstorms are caused by thermal uplift, and most of them occur in a single air mass.

The two most basic elements of thunderstorm formation are moisture and warm air that climbs rapidly, because moisture and temperature are essential factors for backpack formation. When the humidity and temperature are high, a large amount of warm and humid air will rise into the atmosphere, thus forming thunderstorms.

Thunderstorm is a natural weather phenomenon that produces lightning, which usually occurs in spring and summer.

Thunderstorm is the product of atmospheric instability, and it is the general name of cumulonimbus and all kinds of strong weather in its half-life.

Thunderstorms often occur in warm moisture masses in front of the front. Warm and humid air is forced to rise, forming high cumulonimbus clouds.

The rising air becomes cold, and water vapor gradually condenses into water droplets or ice crystals. As they collide with each other, their volume becomes larger and larger, and finally they penetrate the clouds and land on the surface. They will still collide with each other and get bigger during the landing.

Raindrops will lower the temperature of the surrounding air, while cold air will sink. The interaction between sinking cold air and strong rising warm air will bring strong winds and produce thunderstorms.