A macroburst is a powerful and localized weather phenomenon characterized by a strong downdraft that descends from a thunderstorm. When this downdraft reaches the ground, it spreads out in all directions, creating damaging winds that can exceed 100 miles per hour. Macrobursts typically last for about 5 to 30 minutes and can cause significant destruction, including uprooted trees and damaged buildings. These events are often associated with severe thunderstorms and can be mistaken for tornadoes due to their intense winds. Unlike tornadoes, which have a rotating column of air, macrobursts are straight-line winds. Meteorologists use radar technology to detect and predict macrobursts, helping to issue warnings to minimize damage and ensure public safety.