A dry microburst is a small-scale weather phenomenon characterized by a sudden and intense downdraft of air. This downdraft can occur in thunderstorms, where the rain evaporates before reaching the ground, leading to a rapid descent of dry air. The result is a powerful burst of wind that can cause damage over a localized area, often less than 4 kilometers wide. These events are particularly dangerous for aviation, as the strong winds can create hazardous conditions for takeoffs and landings. Meteorologists study dry microbursts to improve weather forecasting and enhance safety measures for aircraft operating in affected regions.