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1926 Nassau hurricane : ウィキペディア英語版 | 1926 Nassau hurricane
The 1926 Nassau hurricane, known as the San Liborio hurricane in Puerto Rico, was a destructive Category 4 hurricane that affected the Bahamas at peak intensity. Although it weakened considerably before its Florida landfall, it was one of the most severe storms to affect the Bahamian capital Nassau and the island of New Providence in several years until the 1928 Okeechobee hurricane, which occurred just two years later. The storm also delivered flooding rains and loss of crops to the southeastern United States and Florida. ==Meteorological history==
The system was first spotted east of the Lesser Antilles as a weak tropical storm on July 22. Moving northwest, the tropical storm passed near Dominica with winds of before entering the eastern Caribbean. It reached hurricane status at 06:00 UTC on July 23, and a short while later passed just south of Puerto Rico. The cyclone attained its first peak of before hitting Cabo Rojo early on July 24. San Juan recorded maximum winds of around and a low barometric pressure of as the eye of the hurricane passed near the extreme southwest corner of Puerto Rico. The storm continued northwest and tracked just east of Hispaniola, losing some intensity to land interaction; by 18:00 UTC on July 24 its winds diminished to . However, the storm began rapid re-intensification as it moved over the Turks and Caicos Islands early on July 25. The storm continued strengthening, attaining the equivalence of major hurricane status by 12:00 UTC that day. By the time it reached the central Bahamas at 00:00 UTC on July 26, it reached winds of . After 12:00 UTC, while still moving northwest, the cyclone made landfall on New Providence and crossed over Nassau, where winds were unofficially estimated at . Reducing its forward speed, the storm weakened considerably after passing New Providence, losing major hurricane status by 06:00 UTC on July 27. As the storm neared the Florida coast, it curved somewhat to the north-northwest and passed just east of Cape Canaveral early on July 28. It made landfall at 10:00 UTC near present-day Edgewater, near the Canaveral National Seashore just south of New Smyrna Beach, with winds of . Prior to reanalysis in 2010, the storm was estimated to have made landfall farther south, near Cocoa Beach. In Florida, the storm's lowest known barometric pressure of was estimated, although it was likely deeper near the Bahamas. After landfall, the storm curved northwestward and weakened rapidly as it moved inland, weakening to a tropical storm southwest of Jacksonville. On July 29, it moved across Georgia as a weakening tropical storm and entered Alabama as a tropical depression. It continued across the southeastern United States while losing tropical characteristics, gradually beginning to curve northeastward over Arkansas, Missouri, and the Ohio Valley, becoming extratropical by 00:00 UTC on August 1. It finally dissipated the following day as it moved northeastward over Lake Ontario.
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