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1910 Cuba hurricane

Category 4 Atlantic hurricane

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Through Cuba and High-pressure area

Due to its unusual loop, initial reports suggested it was two separate storms that developed and hit land in rapid succession. Its track was subject to much debate at the time; eventually, it was identified as a single storm. Analysis of the event gave a greater understanding of weather systems that took similar paths.

The hurricane is considered one of the worst natural disasters in Cuban history. Damage was extensive, and thousands were left homeless. It also had a widespread impact in Florida, including the destruction of houses and flooding. Although total monetary damage from the storm is unknown, estimates of losses in Havana, Cuba exceed $1 million and in the Florida Keys, $250,000. At least 100 deaths occurred in Cuba alone.

Meteorological history

On October 9, the fifth tropical depression of the 1910 season formed from a tropical disturbance in the extreme southern Caribbean, to the north of Panama. It tracked steadily northwestward, and attained tropical storm intensity on October 11. It continued to strengthen, and became a hurricane the next day. On October 13, the storm was observed to the southwest of Cuba. Early on October 14, the hurricane briefly reached an intensity corresponding to Category 4 status on the modern-day Saffir–Simpson hurricane scale before tracking ashore along the western tip of Cuba. However, it weakened somewhat after crossing the island. Upon emerging into the Gulf of Mexico, the hurricane slowed considerably.

Steered by currents from an area of high pressure to the north, the storm began to drift northwestward and rapidly deepen over warm waters of the Gulf. It executed a tight counterclockwise loop, and continued to mature; on October 16 it reached peaked winds of 150 mph (240 km/h) with a minimum barometric pressure of 924 mbar (hPa; 27.29 inHg). The hurricane turned northeastward, again approaching western Cuba, and began to accelerate towards the Florida Peninsula on October 17. Its center passed west of Key West and made landfall near Cape Romano. The storm moved due north for a time as it moved inland, and deteriorated into a tropical storm. From northeastern Florida, the cyclone curved northeastward and hugged the coast of the Southeast United States before heading out to sea. The storm is estimated to have dissipated on October 23.

The storm is unusual in that due to its loop near Cuba, initial reports suggested that it was actually two separate cyclones. The Monthly Weather Review describes the event as multiple disturbances and reports that the first hurricane dissipated in the central Gulf of Mexico after crossing Cuba, while the second formed subsequently and hit Florida. At the time, the storm's track was subject to much debate. It was later identified as a single storm, although observations on the hurricane led to advances in the understanding of tropical cyclones with similar paths. On October 19, The Washington Post wrote, "Whether two storms have been raging in Cuban waters within the past week, or whether the same storm has revisited Cuba, traversing southern Florida in its backwards course, remains to be determined. If the later supposition be correct, the recurve of the storm, after its entrance into the Gulf of Mexico, must have been unusually sudden and sharp."

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