A microburst is characterized by:

A microburst is characterized by small-scale intense downdrafts, which result from a column of air that rapidly descends and spreads out upon hitting the ground. This phenomenon typically occurs during thunderstorms and can produce strong gusts of wind. The rapid downdraft creates a very localized and intense area of turbulence, leading to potential hazards such as damaging surface winds that can challenge aviation and result in property damage.

The intensity of the downdraft in a microburst can reach speeds of over 100 miles per hour and usually lasts for a short duration, making it a critical concern for pilots during takeoff and landing. Understanding the dynamics of microbursts helps meteorologists and safety professionals mitigate associated risks.