Hail in Le Kang

Hail is most common in summer or at the turn of spring and summer. It is some ice particles as small as mung beans and soybeans and as big as chestnuts and eggs. The water on the local surface is vaporized by the sun and then rises into the air. A lot of water vapor condenses into clouds, and after being liquefied by cold air, the dust in the air is used as the condensation core to form raindrops, and the raindrops are getting bigger and bigger. If there are more clouds, it will rain. If exposed to cold air without condensation nuclei, water vapor will condense into ice or snow, which is snow. If the temperature drops sharply, it will form a bigger ice mass, which is hail.