Beaver tail (meteorology)

from Wikipedia, the free encyclopedia

The beaver tail (English Beaver Tail or Beaver's Tail) is a meteorological phenomenon.

It is a special variant of the inflow band . The inflow band is flattened, flat and is reminiscent of the shape of a beaver's tail, hence the name. The clouds move with the updraft.

Individual evidence

  1. ↑ Weather knowledge lexicon - SKYWARN AUSTRIA | Severe weather warnings & messages, non-profit association and weather platform. In: www.skywarn.at. Retrieved November 24, 2016 .