City, Belize, around 20:00 UTC on August 15 with slightly weaker winds of 50 mph (85 km/h). While the system fell to tropical depression intensity while over land, it intensified into a tropical storm over the Bay of Campeche early on August 17, regaining peak strength as it made landfall north of Veracruz, Veracruz, just after 12:00 UTC on August 18. The cyclone quickly weakened once inland and dissipated after 00:00 UTC on August 19. While land stations in Mexico did not observe gale force winds, the Honduran steamship Morazan recorded sustained winds of while stationed at the harbor in Frontera, Tabasco. After the cyclone emerged into the Gulf of Mexico, several ports in the state of Veracruz closed to boat traffic in anticipation of the storm. Tropical Storm Four A tropical depression developed about 70 miles (110 km) north of Barbados around 06:00 UTC on August 16. It moved northwest through the Leeward Islands over the next few hours. While officially recognized as a tropical storm beginning at 06:00 UTC the next morning, there are no conclusive indications that the system ever attained winds of 40 mph (65 km/h); the lack of substantive evidence simply prevented a downgrade during the Atlantic hurricane reanalysis project. Nevertheless, the weak cyclone progressed through the U.S. Virgin Islands and into the southwestern Atlantic, where it fell to tropical depression intensity early on August 18. The cyclone curved to the north-northeast and dissipated after 06:00 UTC on August 21. A station at the Dominica Botanical Gardens in Roseau, Dominica, recorded of rainfall, accompanied by gusty, albeit non-damaging winds. The storm generated abnormally high tides in New Jersey. At Atlantic City, about 150 people were caught in the undertows, with 1 death occurring, 4 others suffering serious injuries, and 1 person missing. Tropical Storm Five As part of the Atlantic hurricane reanalysis project, a previously unidentified tropical cyclone was found to have developed just north of the Leeward Islands by 00:00 UTC on September 1, although this could have occurred sooner. It moved nearly due west throughout its lifespan, intensifying to a tropical storm early on September 3 and making landfall along the coastline of northeastern Hispaniola around 14:00 UTC that day with winds of 45 mph (75 km/h). Weakening ensued over the island, and the system degenerated into an open trough after 00:00 UTC on September 4. The remnants of the cyclone were later