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Cloudburst

Short and very intense rain

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  • 4 chapters
Iceland , Heavy downburst over Selfoss
Hansueli Krapf · CC BY-SA 3.0

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Through Precipitation, Flood and Condensation

Cloudbursts are infrequent as they occur only via orographic lift or occasionally when a warm air parcel mixes with cooler air, resulting in sudden condensation. At times, a large amount of runoff from higher elevations is mistakenly conflated with a cloudburst. The term "cloudburst" arose from the notion that clouds were akin to water balloons and could burst, resulting in rapid precipitation. Though this idea has since been disproven, the term remains in use.

Properties

Specific definitions of a cloudburst vary. In India the definition is rainfall with a rate equal to or greater than 100 millimetres (3.9 in) per hour, while the Swedish weather service SMHI defines the corresponding Swedish term "skyfall" as 1 millimetre (0.039 in) per minute for short bursts and 50 millimetres (2.0 in) per hour for longer rainfalls. The associated convective cloud can extend up to a height of 15 kilometres (9.3 mi) above the ground.

During a cloudburst, more than 20 millimetres (0.79 in) of rain may fall in a few minutes. The results of cloudbursts can be disastrous and can be responsible for flash flood creation.

Rapid precipitation from cumulonimbus clouds is possible due to the Langmuir precipitation process in which large droplets can grow rapidly by coagulating with smaller droplets which fall down slowly. It is not essential that cloudbursts occur only when a cloud clashes with a solid body like a mountain, they can also occur when hot water vapor mingles into the cold resulting in sudden condensation.

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