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An easterly wave is a region of low atmospheric pressure that moves from east to west. These waves are crucial in meteorology as they are the precursors to tropical cyclones in the Atlantic and eastern North Pacific.1

An easterly wave is characterized by a weak circulation and is typically found at an altitude of about 3,600 meters (12,000 feet), extending horizontally for approximately 2,400 km (1,500 miles). When favorable conditions are present, such as warm ocean waters (at least 26.5°C or 80°F to a depth of 50 meters), an easterly wave can intensify and contract, eventually developing into a tropical storm and then a tropical cyclone. These conditions include a pre-existing atmospheric circulation, rapid cooling with height to support deep convective clouds, and sufficient humidity in the middle atmosphere.12

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