HIGHLIGHTS
SUMMARY
Even then, the presence of drops with velocity outside the expected terminal velocity range has been reported by several works: drops with a fall velocity lower than 70% of their terminal velocity are labelled as sub-terminal, whereas drops falling at larger than 130% of the terminal velocity are considered super-terminal. In natural rain, very large raindrops, grown by coalescence, break-up into smaller drops as a result of their unstable nature (hydrodynamical break-up) or, more frequently, after collisions with smaller drops (collisional break-up). To be specific, the quantification of non . . .
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