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A macroburst is an intense downdraft from rain clouds that hits the ground and spreads out horizontally. It is larger than a microburst, with a diameter exceeding 4 km (2.5 miles), and can generate winds up to 215 km/h (135 mph). Macrobursts, like microbursts, are often associated with thunderstorms and can cause significant damage on the ground. They pose a serious hazard to aircraft, particularly during takeoff and landing, due to the abrupt changes in wind speed and direction they create, known as wind shear. In dry environments, the rain may evaporate before reaching the ground, resulting in a dry macroburst with no visible precipitation.1

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