A cloud burst is an intense, highly localized precipitation phenomenon characterized by extremely high rainfall rates, typically on the order of several centimeters per hour, occurring over a small spatial scale and short duration. It is usually associated with deep convective clouds, strong updrafts, and rapid condensation of large quantities of atmospheric moisture, often in orographic or monsoonal settings. The resulting precipitation can exceed the infiltration capacity of soils and the drainage capacity of channels, producing flash floods, rapid surface runoff, and geomorphologically significant erosion. Cloud bursts are important in hydrometeorology and disaster risk assessment due to their extreme intensity and limited predictability at fine spatial and temporal scales.
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