Playa del Carmen, Quintana Roo — Tourists and residents of Playa del Carmen witnessed a waterspout that formed on August 12 off the coast of Playacar. The funnel of air, visible over the Caribbean Sea and connected to a cloud formation, could be observed from various points in the city, including the parking lot of the Centro Maya shopping mall and the elevated bridge of the federal highway, according to local media reports.
Meteorological Explanation
Municipal meteorologist Antonio Morales Ocaña stated that the phenomenon originated from a cumulus cloud with vertical development, known as a cumulonimbus, whose base generated the waterspout. Morales explained that as the formation approached the coast, it began to dissipate due to intense rainfall associated with the weather system.
The specialist noted that such events are relatively common in the region during the hot and rainy season, when humidity and atmospheric instability contribute to the formation of vertically developed clouds. He estimated that the waterspout reached a height of between 600 and 900 meters and was linked to a storm cloud associated with a squall line along the coast.
Definition and Characteristics
According to the World Meteorological Organization, a waterspout is a type of tornado that occurs over bodies of water. Typically, it consists of a small, low-intensity rotating column of air over open water, beneath cumulonimbus or cumulus congestus clouds.
These phenomena are equivalent to land-based tornadoes but form over the sea and are more frequent in tropical or subtropical regions, as well as in areas with horizontal wind shear.
No injuries or property damage were reported in connection with the Playa del Carmen waterspout.
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