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1898 Georgia hurricane

Category 4 Atlantic hurricane in 1898

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Through Atmospheric pressure

Meteorological history

On September 28, 1898, island stations in the Lesser Antilles indicated the presence of a tropical cyclone, which was confirmed by the next day. Modern researchers determined that the system developed on September 25 about 220 miles (350 km) east of Guadeloupe. For most of its duration, the system maintained a northwest track, reaching hurricane status on September 27. Later that day, a barometric pressure of 977 mbar, suggesting winds of 90 mph (140 km/h). Its intensification rate slowed on September 28, before strengthening continued on October 1. The winds reached 115 mph (185 km/h), which is the equivalent of a major hurricane, or Category 3 on the Saffir-Simpson scale. Around that time, the hurricane turned toward more to the west-northwest, due to a large ridge across the western Atlantic.

On October 2, the hurricane continued toward the west-northwest, approaching the southeastern United States. That day, it made landfall on Cumberland Island in Camden County, Georgia, and initially was thought to have done so as a Category 2 on the Saffir-Simpson scale. A storm surge of 16 ft (4.9 m) was observed in Brunswick, Georgia, suggesting a central pressure of 938 mbar based on the SLOSH model. Such intensity ranked the hurricane tied for the 16th strongest United States landfall, as well as the strongest in the state of Georgia. It is also the most recent major hurricane to hit the state. Additionally, its radius of maximum wind was estimated at 20 miles (32 km). Almost a century after the hurricane, researchers estimated the hurricane made landfall with winds of 135 mph (217 km/h), a Category 4 on the Saffir-Simpson scale. After making landfall, the hurricane quickly weakened, deteriorating to tropical storm status within 12 hours. After moving across Georgia, the storm weakened further to tropical depression status over northeastern Alabama on October 3. It continued northwestward through the Ohio Valley before recurving northeastward, accelerating through southeastern Canada and later dissipating over Newfoundland on October 6.

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