A meteotsunami was recorded in Florida last week.
Clearwater Beach chairs were toppled last Wednesday, and the National Weather Service issued multiple special marine warnings throughout the day and into the evening.
The agency shared a photo of the incoming storm at around 9:28 a.m. ET.
Water levels peaked at around 4 feet, weather officials told The Associated Press. But what is a meteotsunami?
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Meteotsunamis are large waves caused by storms, according to the National Oceanic and Atmospheric Administration.
While tsunamis are triggered by seismic activity, meteotsunamis are driven by air-pressure disturbances often associated with fast-moving weather events, including severe thunderstorms and squalls.
The storm creates a wave that moves towards the shore and is amplified by a shallow continental shelf and inlet, bay or another coastal feature.
They have been observed to reach heights of 6 feet or even more.
Identifying such events is challenging, the administration notes, because its characteristics are nearly indistinguishable from a seismic tsunami.
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Meteotsunamis can be confused with wind-driven storm surges or a seiche. Seiches are standing waves with longer periods of water-level oscillations, whereas meteotsunamis are progressive waves that are limited to the tsunami frequency band of wave periods. Sometimes they can occur simultaneously, and seiches are usually limited to partially or fully enclosed basins like Lake Erie.
These uncertainties make it difficult to predict a meteotsunami and warn the public of a potential event, but scientists have identified atmospheric conditions that are likely to generate a meteotsunami and continue to work on ways to forecast them.
This Florida meteotsunami was around 2.5 feet higher than the forecast wave height.
The weather service does not issue specific advisories for meteotsunamis.
They occur around the world, including the Great Lakes, Gulf of Mexico, Atlantic Coast and the Mediterranean and Adriatic Seas.
The Associated Press contributed to this report.
