on October 14, the storm made landfall on Isla de la Juventud, Cuba, with winds of , shortly before striking modern-day Artemisa Province at the same intensity. After emerging into the Gulf of Mexico, the storm intensified further, peaking with winds of early on October 15. The cyclone then decelerated and weakened, falling to tropical depression status by late the following day. Around 09:00 UTC on October 17, it made landfall near Orange Beach, Alabama, with winds of . The storm quickly lost tropical characteristics and was absorbed by a frontal boundary several hours later. It may have been a subtropical storm due to some hybrid characteristics. The system left minimal impact in Cuba and the Gulf Coast of the United States. Tropical depressions In addition to the five cyclones reaching at least tropical storm intensity, nine other tropical depressions formed during the season. A trough moving westward through the southwestern Caribbean developed into a tropical depression on May 12. The depression moved northwestward for a few days and failed to intensify. It made landfall in Nicaragua on May 15 and dissipated later that day. On June 14, a low-pressure area developed along the tail-end of a frontal boundary just offshore northeast Florida. By the following day, the low acquired tropical characteristics and likely became a tropical depression. The depression moved generally eastward and dissipated on June 16. A tropical wave developed into a tropical depression just southwest of the Cape Verde Islands on August 1. The depression moved slowly northward and then north-northeastward, before dissipating on August 3 about south of São Vicente. On August 17, a tropical depression developed in the eastern Gulf of Mexico. Moving northeastward, the system struck Florida, before emerging in the Atlantic on August 18. The storm moved along the East Coast of the United States and transitioned into an extratropical cyclone by August 20. Its remnants crossed Nova Scotia later that day and Newfoundland on the following day. A weak circulation developed along the axis of a trough situated offshore North Carolina in early September, with a tropical depression forming on September 3. The depression moved southward and likely dissipated by the next day. An inverted trough and a tropical wave merged and briefly developed into a tropical depression well offshore Georgia on September 11. By the next day, the circulation had either dissipated or merged with a cold front. A strong tropical