from two ships. After attaining peak winds of , the cyclone quickly transitioned to an extratropical cyclone by 12:00 UTC on September 28 as multiple fronts became intertwined with the circulation. The extratropical cyclone continued to parallel the U.S. East Coast, eventually making landfall in Newfoundland early on September 30. It strengthened into a hurricane-force low on October 1 but ultimately dissipated two days later as it merged with another cyclone and became increasingly elongated. Tropical Storm Ten In late September, a tropical wave moved westward across the Caribbean. An initial area of low pressure formed over the northwestern portion of the region on September 29, but this feature dissipated within two days. A new low formed and organized into a tropical storm around 00:00 UTC on October 2 while positioned about south of Mobile, Alabama. It reached peak winds of after six hours, with steady weakening thereafter as the storm moved west-northwest and then north. The system made two landfalls in central Louisiana near the Atchafalaya Basin between 12:00–14:00 UTC on October 3, both with winds of . The system continued to degrade once inland, dissipating after 06:00 UTC on October 4 over southeastern Arkansas. The tropical storm caused the wettest 48-hour period in New Orleans's history, with of rainfall recorded as the storm made landfall; the maximum 24-hour rainfall total of nearly broke the city's record for maximum daily rainfall. City streets were submerged under as much as of water. Blue laws were suspended for half a day to allow grocery store food supplies to reach stranded areas. Damage was estimated at several thousands of dollars and the flooding was considered the city's most severe since the Great Mississippi Flood of 1927. Crops around the city sustained considerable damage. At Belle Chasse, Louisiana, the of rain recorded in 24 hours set the state record for the highest 24-hour rainfall in October. The strongest recorded winds from the tropical cyclone occurred at Port Eads, Louisiana, where a 33-mph (53 km/h) wind gust was documented as the system was developing on October 2. Hurricane Eleven Similar to Tropical Storm Five, a new tropical cyclone that was not recognized in real time was found to have existed over the northern Atlantic. From October 16–17, a cold front moved eastward across the basin. An area of low pressure formed along the southern end of the dissipating boundary, initially harboring characteristics of an