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Hasznos link: contrailscience.com
This phenomenon can often be observed on condensation trails, and is a little similar to mammatus clouds. When the airplane flies at more than 500 mph, it creates wake turbulence, made up of regularly patterned wake vortices. When the contrail is denser, we can see pendules clinging from it. Their formation depends on several factors, such as the speed and size of the aircraft and the characteristics of the air that it flies through. The above photos were taken this summer and autumn in Vecsés, Hungary.
Useful link: contrailscience.com
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