Precipitation- Bergeron–Findeisen process

Bergeron–Findeisen process.

This theory is commonly called the ice process of precipitation and is a theoretical explanation of the process by which precipitation particles may form within a cloud composed of both ice crystals and liquid water.

How it works- The ice crystals gain mass by vapour deposition (sublimation), as liquid droplets lose mass through evaporation. The transfer of water is not by liquid drops colliding with the ice crystal; the transfer of water comes from…