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A cloud burst is a period of very heavy rainfall. Usually it occurs under a strong thunderstorm cell and are more likely to occur with storms that are associated with tropical moisture. Cloud burst can result from several different right ingredients that comes together. Below is just one example of how a cloud burst can form.

Usually with a strong thunderstorm, the updraft will keep the water droplets up in the clouds. With non-tropical thunderstorms, these droplets will be push higher into the atmosphere where it will go above the freezing level and turn into ice. This ice stone is known as a hail stone. As the ice pellets circulate pu and down high above in the cloud, it will grow until the it gets too heavy for the updraft to keep in from falling or the storm and updraft weakens and the hailstone will be able to fall all the way to the ground. What you would usually end up with is a good hail storm.

With tropical large storms, there are usually more moisture for the storm to work with. But the other factor is the height of the freezing level. With the air being more tropical, the freezing levels are very high that the strong updraft of the storms are still not able to push the water droplet above the freezing level. So instead of hail growing in size, you have liquid water droplets growing in size, If the thunderstorm suddenly weakens or the weight of all that water combine with gravity finally overpowers the force of the updraft, the whole mass of water will start falling toward the surface. This is when huge tall thunderstorm will suddenly fall apart as the downdraft takes over as the dominate flow. When this large volume of water finally reach the surface, that will be your cloudburst and also the end of this strong thunderstorm cell.

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∙ 16y ago
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