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The Meteorological Department explains that the "Kelaid Al-Wasmi" phenomenon refers to the formation of localized cumulonimbus clouds known as "Haqban." These clouds appear before the monsoon season and present opportunities for scattered, sometimes thunderstormed rains. They form when the sea breeze coming from the eastern coast meets the wind from the western coast in the central areas. This process is accompanied by strong downdrafts that stir up dust and reduce horizontal visibility.
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