Mid-June tropical storm Satellite imagery and ship data indicated that Subtropical Depression Three formed at 18:00
UTC on June 14 to the northeast of the northeastern Bahamas, Conditions were not favorable for strengthening, with cool air and minimal outflow, although the cyclone acquired
gale-force winds by 12:00 UTC on August 16, becoming a
subtropical storm.
Hurricane Beulah A tropical wave exited the coast of Africa on August 28. Moving westward, it organized into Tropical Depression Seven at 12:00 UTC on September 5, while located about northeast of
Barbados. On September 7, the depression intensified into Tropical Storm Beulah, which crossed into the Caribbean Sea that day. After continued strengthening, Beulah became a hurricane on September 8, and two days later reached an initial peak of to the southwest of Puerto Rico. An
anticyclone over the Bahamas turned the hurricane westward, as changing upper-level conditions from a passing trough to the north, as well as land interaction with Hispaniola, greatly weakened Beulah. The track shifted to the southwest and weakened further to a tropical storm. Flooding rains damaged roads, bridges, and houses on Martinique and neighboring
Saint Lucia. In the Lesser Antilles, Beulah caused $7.65 million in damage and 17 deaths. The storm caused minor damage and one death in southern Puerto Rico. After the severe impacts of
Hurricane Inez a year prior, about 200,000 people evacuated the southern coast of the Dominican Republic. There, Beulah left heavy damage to roads, bridges, and the banana and coffee crops, but the evacuations led to a low death toll of two in the nation. Minor water damage occurred along Haiti's southern
Tiburon Peninsula. On Cozumel, Beulah's strong winds destroyed 40% of the houses and heavily damaged many hotels, severely impacting the tourism industry. Along the northern Yucatán Peninsula, the winds wrecked a clock tower in
Tizimín, killing five. The rains caused record river flooding, with a peak crest of along the
San Antonio River at
Goliad. In northeastern Mexico, Beulah killed 19 people, left 100,000 people homeless, and caused $26.9 million in damage. In Texas, damage reached $200 million, and there were 15 deaths, 5 of whom related to a
then-record-breaking
tornado outbreak that generated 115 tornadoes. A nearby ship reported waves on September 27, potentially indicating stronger winds during periods without meteorological observations, although unfavorable conditions prevented initial development. It was not until 12:00 UTC that Edith attained tropical storm force winds. Twelve hours later, the storm reached peak winds of , a trend that spurred
hurricane watches from
Dominica northward through the
Leeward Islands. The storm failed to intensify due to its proximity to a cold upper-level trough and releasing too much latent heat. On September 30, Edith passed over Dominica as a weakened tropical storm and dissipated the next day over the eastern Caribbean Sea. It caused gusty winds and minor damage during its passage through the Lesser Antilles. As the system organized more, it tracked northward, although a ridge to the north steered the nascent system to the west. On October 2, the British ship
Plainsman observed gale-force winds, prompting the NHC to upgrade the depression to Tropical Storm Fern. The rains caused additional flooding along the
Pánuco River, which became swollen during Hurricane Beulah two weeks prior. Three people drowned in the floodwaters. Damage was minor related to Fern.
Tropical Storm Ginger An area of convection developed off the west coast of Africa following the westward passage of Tropical Depression Sixteen. On October 5, it is estimated that Tropical Depression Seventeen developed from this system, At the time, the storm was located about north-northwest of
Dakar, Senegal, well east of
35° W where the NHC began issuing formal tropical cyclone advisories. Instead, the
Rota, Spain Naval Fleet Station issued gale warnings in relation to the storm. Later on October 6, it was estimated that Ginger reached peak winds of and a minimum barometric pressure of . On October 7, the storm curved west-southwestward and quickly weakened into a tropical depression. Ginger dissipated on October 8 to the north of Cabo Verde.
October tropical storm A tropical wave moved through the northeastern Caribbean on October 10, with a large area of associated thunderstorms. The wave interacted with a stalled frontal boundary, developing a broad circulation by October 13 to the northeast of the Bahamas. A day later, the system developed into a subtropical storm – its classification was because the system was co-located with a trough. There was another area of convection along the front northeast of the subtropical storm, which accelerated northeastward. Meanwhile, the subtropical storm turned westward. It had a small circulation with thunderstorms sheared north of the center, which gradually became more organized. On October 17, an approaching front turned the storm northward and later northeastward. On the same day, the subtropical storm transitioned into a tropical cyclone. On the next day, the storm attained peak winds of , before it transitioned into an extratropical cyclone over
Atlantic Canada, where it was ultimately absorbed by the cold front on October 19. with the strongest winds near the center, spurring gale warnings for Bermuda. However, winds there only reached about during the storm's passage. The NHC initially anticipated that Heidi would become extratropical within two days. Early on October 23, the agency upgraded the storm to hurricane status about 105 mi (175 mi) southeast of Bermuda. Heidi moved quickly eastward with the approaching trough until October 25, when a building ridge caused the hurricane to move slowly northeastward in an area of light wind shear. Early on October 26, Heidi attained peak winds of about halfway between Bermuda and the
Azores. After stalling on October 29, Heidi turned westward and weakened to tropical storm status. Another approaching trough turned the storm back to the northeast on October 31. Later that day, Heidi started losing tropical characteristics, transitioning into an extratropical cyclone by November 1. Later that day, the remnants of Heidi were absorbed into the prevailing weather conditions of the north Atlantic Ocean.
Other systems There were also five non-developing tropical depressions during the season. On June 10, Tropical Depression One developed in the western Caribbean Sea, near the
Gulf of Honduras. It moved northwestward, dissipating over the eastern Yucatán Peninsula on June 12. A tropical wave exited Senegal on September 18 and progressing westward near Cabo Verde. A day later, it developed into Tropical Depression Fifteen. It moved across the Atlantic, dissipating on September 27 after entering the eastern Caribbean. A tropical wave exited Africa on September 25. A day later, it became Tropical Depression Seventeen while moving near Cabo Verde. It dissipated on September 28. From October 7–10, Tropical Depression Twenty-Two existed in the western Atlantic. From October 15–17, Tropical Depression Twenty-Four existed in the central Atlantic. == Storm names ==