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What (who) is static instability - definition
![Rain water flux from a canopy. Among the forces that govern drop formation: Plateau–Rayleigh instability, [[Surface tension]], [[Cohesion (chemistry)]], [[Van der Waals force]].](https://commons.wikimedia.org/wiki/Special:FilePath/RainDrops1.jpg?width=200 "Rain water flux from a canopy. Among the forces that govern drop formation: Plateau–Rayleigh instability, [[Surface tension]], [[Cohesion (chemistry)]], [[Van der Waals force]].")
Wikipedia
The Plateau–Rayleigh instability, often just called the Rayleigh instability, explains why and how a falling stream of fluid breaks up into smaller packets with the same volume but less surface area. It is related to the Rayleigh–Taylor instability and is part of a greater branch of fluid dynamics concerned with fluid thread breakup. This fluid instability is exploited in the design of a particular type of ink jet technology whereby a jet of liquid is perturbed into a steady stream of droplets.
The driving force of the Plateau–Rayleigh instability is that liquids, by virtue of their surface tensions, tend to minimize their surface area. A considerable amount of work has been done recently on the final pinching profile by attacking it with self-similar solutions.
