On February 2, a non-frontal low formed in the western Caribbean Sea two months after the end of the hurricane season. It moved quickly north-northwestward and acquired gale-force winds as it brushed the northern coast of Cuba. Early on February 3, the storm struck Cape Sable, Florida and quickly crossed the state. The Miami National Weather Service office recorded a wind gust of 68 mph (110 km/h) during its passage. The winds damaged windows and power lines, catching residents and tourists off-guard. The cyclone also dropped 2–4 inches (50–100 mm) of precipitation along its path, causing crop damage in Miami-Dade County.
After leaving Florida, the storm continued rapidly northeastward and transitioned into a tropical storm during the afternoon of February 3. While off the coast of the Southeastern United States, it attained peak winds of 70 mph (110 km/h). On February 4 it evolved into an extratropical cyclone off the coast of North Carolina. Later that day, it passed over Cape Cod, and early on February 5 dissipated after crossing into Maine. The storm caused scattered power outages and gusty winds across New England. The cyclone remains the only tropical or subtropical storm on record during the month of February.
Over six months after the previous storm dissipated, a tropical depression developed just off the west coast of Africa on August 18. It moved generally west- to west-northwestward for much of its duration, intensifying into a tropical storm on August 24 east of the Lesser Antilles. The next day, Hurricane Hunters confirmed the presence of Tropical Storm Able. Passing north of the islands, the storm attained hurricane status on August 27. On August 30, Able turned to the north-northwest due to an approaching cold front, and the next day made landfall near Beaufort, South Carolina as a Category 2 hurricane with peak winds of 100 mph (160 km/h). The town was heavily damaged, and was briefly isolated after winds downed power and telephone lines. Across South Carolina, the hurricane caused two indirect deaths, as well as moderate damage totaling $2.2 million (1952 USD, $19.8 million 2017 USD).
As Able turned north and northeastward over land, the winds quickly weakened to tropical storm force, although it retained gale force winds through North Carolina, Virginia, and Maryland; this was due to remaining over the flat terrain east of the Appalachian Mountains, as well as retaining a plume of tropical moisture from its south. It left light damage in North Carolina, some of it due to a tornado. In Maryland, heavy rainfall caused widespread flooding, which washed out the tracks of the Baltimore and Ohio Railroad near Baltimore. In Ellicott City, Maryland, the rains flooded several houses, forcing families to evacuate. Two tornadoes were also reported in the region, and damage in the Washington, D.C. area reached $500,000 (1952 USD, $4.51 million 2017 USD). Further northeast, the storm continued to produce heavy rainfall, causing flooding, as well as one indirect death in Pennsylvania. After moving through New England, Able dissipated on September 2 near Portland, Maine.
A cold front was located north of the Bahamas on August 26, with a broad area of cyclonic turning located east of northern Florida. Atmospheric pressures were falling in the region, and gale force winds were recorded by 12:00 UTC on August 27. Based on the structure, it is estimated that the frontal low developed into a tropical storm by 18:00 UTC that day. Ship reports in the region suggested peak winds of 50 mph (85 km/h). There was very dry air on the west side of the system, unusual for August, and the radius of maximum winds was around 115 mi (185 km), suggesting that the structure could have been akin to a subtropical cyclone. The storm continued to the northwest, making landfall very near Myrtle Beach, South Carolina at 02:00 UTC on August 28. It spread rainfall across the Carolinas, later enhanced by Hurricane Able just days later, while cities reported winds of around 35 mph (55 km/h). The storm weakened over land and dissipated late on August 28 over eastern Kentucky.
The third tropical cyclone of the season developed on August 31 a short distance east of the northern Lesser Antilles. Its presence was reported by a ship the next day that encountered rough seas and gale force winds. As a result, the Weather Bureau sent the Hurricane Hunters to investigate the system, which reported a strengthening hurricane moving northwestward. Given the name Baker, the hurricane passed north of the Lesser Antilles, reaching peak winds of 110 mph (175 km/h) late on September 3. For several days, the Hurricane Hunters reported similar winds, along with gusts up to 140 mph (230 km/h).
With a large anticyclone located over the Ohio Valley, Baker turned to the northeast on September 5, passing about halfway between Bermuda and North Carolina. The hurricane slowly weakened as it moved through the north Atlantic Ocean, just missing Newfoundland while maintaining winds of 80 mph (130 km/h). Wind gusts on Avalon Peninsula reached 70 mph (110 km/h), and heavy fishing damage was reported in Lower Island Cove. After affecting the island, Baker transitioned into an extratropical storm, which lasted another day before dissipating south of Greenland.
A dissipating cold front stalled across the northeastern Atlantic Ocean on September 7, northeast of the Azores. That day, a closed circulation developed and quickly became independent of the front. Based on a uniform thermal structure, as well as ship reports in the region of gale-force winds near the center, it is estimated that the system became a tropical storm early on September 8. That day, the system moved west-southwestward, atypical for cyclones in that region during September. On September 9, the storm turned to the southeast, reaching estimated peak winds of 50 mph (85 km/h), based on ship observations. Moving slowly through the northern Azores, the storm produced winds of 35 mph (55 km/h) along Terceira Island. It slowly weakened, and by late on September 10 the system degraded into a tropical depression. By the next day, the system was interacting with an approaching cold front, indicating that the depression had transitioned into an extratropical cyclone. Around 20:00 UTC, the storm moved ashore the southwestern tip of Portugal with gale-force winds. The storm turned to the northwest through the Iberian Peninsula, dissipating on September 14 over southwestern France.
On September 22, a tropical wave moved into the eastern Caribbean Sea, spawning a tropical depression near Hispaniola early on September 24. As it tracked west-northwestward, the low dropped heavy rainfall, peaking at 4.42 in (112 mm) in Christiansted, United States Virgin Islands, as well as 11.9 in (300 mm) in Garzas, Puerto Rico. In Puerto Rico, the rains caused and landslides that affected seven towns, notably Ponce, the island's second-largest city. There, at least 14 buildings were destroyed. The floods left more than 1,000 people homeless, 300 of whom took refuge in a Red Cross shelter. Overall, the flooding on the island killed four people and left moderate damage of around $1 million (1952 USD, $9.02 million 2017 USD).
After affecting Puerto Rico, the low continued to organize, and subsequently struck the Dominican Republic on September 23. The circulation became disrupted while crossing Hispaniola, although it reorganized near the Turks and Caicos Islands and became Tropical Storm Charlie before reaching those islands. On September 25, Charlie attained hurricane status,, and due to its continued northwest motion, the Weather Bureau advised small craft to remain at port in the southeastern United States coast. However, the hurricane turned to the north and northeast on September 26, during which the Hurricane Hunters recorded peak winds of 120 mph (195 km/h). It briefly threatened Bermuda, prompting the United States Air Force to evacuate its fleet of airplanes from Kindley Air Force Base. Charlie ultimately northwest of Bermuda, and later began weakening. On September 29 it turned eastward, and later that day transitioned into an extratropical cyclone. The remnants lasted two more days before dissipating 400 mi (640 km) southeast of Newfoundland.
On September 25, a tropical wave spawned a tropical storm about 700 mi (1,100 km) east of the Lesser Antilles. Given the name Dog, the storm moved northwestward for its entire duration. On September 26, Hurricane Hunters observed winds of 78 mph (126 km/h), which indicated that Dog strengthened to just below hurricane intensity. The plane also estimated winds of around 100 mph (160 km/h), although they were unable to locate a closed center of circulation. After approaching hurricane status,, Dog began a marked weakening trend, with winds of only 50 mph (85 km/h) by September 27. Continuing to weaken, the storm dissipated on September 29. The Weather Bureau advised ships to avoid the storm, but overall Dog did not affect land. As the Hurricane Hunters did not reported a well-defined circulation, there was a possibility Dog was not a tropical cyclone; the report of the 1952 season assessed that Dog remained a tropical wave.
On September 24, a tropical wave moved off the west coast of Africa. It is estimated that a closed circulation developed on the next day, suggesting the formation of a tropical depression. On September 26, Santiago island within Cape Verde recorded winds of 30 mph (45 km/h) as the system was passing to the southwest. A minimum pressure of 1,000 mbar (30 inHg) and ship reports of 35 mph (55 km/h) winds indicate that the system reached peak winds of 45 mph (75 km/h), or a minimal tropical storm. It turned to the north on September 27 and likely weakened, although observations were sparse. By September 30, the system lost its circulation and degenerated into an open trough.
On October 6, a tropical depression formed about 700 mi (1,100 km) east of Antigua, near where the previous hurricane developed. The depression proceeded northward, and was detected by the Hurricane Hunters on October 7. The next day, a plane flew into Easy and reported peak winds of 110 mph (180 km/h), indicating the storm had rapidly intensified. By the time it reached peak intensity, the hurricane had turned sharply to the east, and later began to move toward the south. As quickly as it strengthened, Easy began to weaken, and an aircraft reported winds of only 48 mph (77 km/h) on October 9. The storm headed southwest, ultimately dissipating on October 11 about 155 mi (249 km) southwest of where it formed. Easy never affected land.
The strongest tropical cyclone of the season formed on October 20 in the Caribbean Sea off the northwest coast of Colombia, believed to have been from the Intertropical Convergence Zone. It moved northwestward, intensifying into a tropical storm on October 21 and a hurricane the following day. Fox subsequently turned to the north, intensifying to a major hurricane as it passed west of the Cayman Islands. Late on October 24, the cyclone struck the small island of Cayo Guano del Estes in the Archipelago de los Canarreos, south of Cienfuegos, Cuba. It struck the island with peak winds of 145 mph (233 km/h), and the island reported a minimum pressure of 934 mbar (27.59 inHg). Shortly thereafter, Fox crossed the mainland coast of Cuba west of Cienfuegos, and it weakened while crossing the island.
Hurricane Fox crossed Cuba in a rural area dominated by sugar plantations, with heavy damage reported to 36 mills. In one town, the hurricane destroyed about 600 homes and damaged over 1,000 more. Across the island, the strongest winds downed large trees and washed a large freighter ashore. Heavy rainfall affected all but the extreme eastern and western end of the island, with a peak of 6.84 in (174 mm) near Havana. The rains flooded low-lying areas and caused rivers to exceed their banks. Throughout Cuba, Hurricane Fox injured 70 people, killed 40, and heavy damage totaling $10 million (1952 USD, $90.2 million 2017 USD). Fox was among the strongest hurricanes to strike the country.
After crossing Cuba, Fox emerged into the Atlantic Ocean with winds of 100 mph (160 km/h), crossing central Andros and turning eastward though the Bahamas. On New Providence, the hurricane dropped 13.27 in (337 mm) of rainfall, Strong winds caused severe crop damage, leaving 30% of the tomato crop destroyed. After briefly restrengthening to a major hurricane, Fox began a steady weakening trend. It turned abruptly to the north-northwest, followed by another turn to the northeast. On October 28, Fox was absorbed by a cold front west-southwest of Bermuda.
A cold front stalled north of the Virgin Islands on November 23, spawning an extratropical storm the next day. The system strengthened while moving northward, attaining gale force winds on November 25. It was a large system, and a ship in the vicinity reported a pressure of 994 mbar (29.4 inHg). The observation, within a warm environment and in concurrence with gale force winds, suggested that the system became a tropical storm on November 26, although the system likely was a subtropical cyclone due to the structure. Turning to the west-northwest along a dissipating cold front, the storm reached peak winds of 60 mph (95 km/h) on November 27. Another front in the region steered the storm to the south and east in a counterclockwise circle. Weakening slightly, the system briefly transitioned into an extratropical storm on November 30 before dissipating later that day within the front.
These names were used to name storms during the 1952 season, the third and final time storm names were taken from the Joint Army/Navy Phonetic Alphabet. Names that were not used to designate tropical cyclones are marked in gray.