The three phenomena: wind, rain and hail
How clouds freeze and heat, and the birth of wind, rain and hail
In two dense columns Leonardo analyses the three phenomena of wind, rain and hail. He argues that a cloud, borne upward by its enclosed heat toward the sphere of fire, meets the cold region of the air and freezes on the outside but not within; from this arise wind (from moisture that vaporizes), rain (from vapour particles that collide, cling together and grow heavy, falling as large drops), and hail (from moisture that freezes into globules). He also states general rules, that a body grows lighter as it heats and heavier as it cools, and heats more the more it is condensed and the nearer it comes to the source of heat. The torn fragment carries further faded lines not included here.
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Why a cloud freezes above and at the sides, not in the middle
Leonardo reasons that a cloud freezes above, below and at its sides but not in its middle, because heat acts more strongly upward than sideways, and more sideways than downward. The part of the body that travels the greater distance is the one that comes nearest to the cold.
Heat makes bodies lighter, cold heavier
A set of rules states that a thing becomes lighter the more it is heated and gains weight the more it is cooled. It heats more the more it is condensed and the nearer it comes to the source of heat, and less the further it is removed from it.
The generation of wind, rain and hail
The moisture enclosed in the heated cloud breaks up and vaporizes to make a furious wind; vapour particles collide, cling together and grow heavy, falling as large raindrops; and at the outer edge the moisture freezes into globules that run together into round hailstones.
