Later in the season, Tropical Depression Twenty-Nine caused severe local flooding in the Florida Panhandle and southwestern Georgia in September.

The Atlantic upper tropospheric shear line, a semi-permanent feature that extended southeastward into the Caribbean Sea, which enhances outflow from disturbances, remained persistent throughout the season.

Camille was the most intense tropical cyclone of the season, peaking as a Category 5 hurricane with maximum sustained winds of 175 mph (282 km/h) and a minimum barometric pressure of 900 mbar (27 inHg).

[4] Damage was catastrophic in Jamaica with landslides, flooding, broken communication lines, cancellation of its railway service and evacuation of hundreds of people from their homes.

The Jamaica Railway Corporation's trains were disrupted by landslides blocking the tracks from Spanish Town to Port Antonio and floodwaters inundating a bridge in Gregory Park.

On June 9, the Church Welfare Organization of the West Indies Junior Seventh Day Adventists set out food, money and blankets the victims.

By 12:00 UTC on July 31, Anna degenerated into a surface-based trough while situated north of the Lesser Antilles, but continued to produce gale-force winds.

Under the influence of a trough, Blanche headed rapidly north to north-northeastward while significantly intensifying, becoming a hurricane by 18:00 UTC on the same date, based on Navy reconnaissance reports.

While passing to the south of Newfoundland, the extratropical remnants of Blanche turned eastward and east-southeastward, eventually to be absorbed by a frontal zone late on August 14.

Between August 16–17, the storm rapidly deepened, attaining a minimum barometric pressure of 905 mb (26.7 inHg), along with maximum sustained winds of 175 mph (282 km/h), making it a Category 5 hurricane.

[25] While remaining nearly stationary offshore Central America, heavy precipitation fell in some countries, especially Guatemala where severe flooding killed 269 people and caused $15 million in damage.

In neighboring Honduras, the hurricane caused damage in the northern portions of the country, with the offshore Bay Islands Department being particularly hard hit.

[26] Coastal areas of Belize lost electricity and telephone service, and high winds resulted in extensive damage to banana crops.

[4] Moving westward to west-northwestward, it developed into a tropical depression at 1200 UTC on September 14, while located about 1,250 mi (2,010 km) southeast of Puerto Rico,[2] based on Hurricane Hunter observations of an organized circulation.

[35] Due to the lack of good upper-level outflow, as well as unfavorable water, Holly quickly weakened to tropical storm status on September 18, as confirmed by the Hurricane Hunters.

[2] Ship reports on September 19 indicated the presence of low pressure area in the Gulf of Mexico, centered about 300 mi (480 km) west-northwest of Key West, Florida.

[38] In addition, a tornado spawned by the depression destroyed a trailer, damaged 30 homes, and toppled ballpark bleachers, fences, lights, and electrical poles.

[2] Heading westward, Inga was downgraded to a tropical depression,[42] before dissipating fully on October 15,[2] while located about 290 mi (470 km) from where it initially attained hurricane status.

The storm curved northeastward by September 24 and transitioned into a hurricane that day, peaking with maximum sustained winds of 75 mph (121 km/h) and a minimum barometric pressure of 987 mbar (29.1 inHg).

[2] Rainfall was relatively light and the heaviest amounts were displaced far east of the track, with precipitation peaking at 6.74 inches (171 mm) in Saint Augustine, Florida.

[45] United States Coast Guard planes searched for three people in a light aircraft that went missing as it traveled from DeFuniak Springs to Sebring.

[43] On October 1, a tropical depression developed over the northwestern Caribbean Sea from the same cut-off low pressure that spawned the previous subtropical storm on September 29.

[2] Jenny emerged into the western Atlantic as a tropical depression, but increased ridging forced the storm to track west-southwestward back over Florida.

[47] Rainfall along the lower Kissimmee River and the Lake Okeechobee basin caused some pastures and flood plain areas to be inundated by water.

[4] A cold core trough of low pressure over the western Atlantic Ocean warmed on the eastern end, becoming a tropical depression on October 7 about 135 mi (217 km) north of Punta Cana, Dominican Republic.

[2] A low pressure area developed into a tropical depression while located about 75 mi (121 km) northeast of Guanaja in the Bay Islands Department of Honduras.

It then curved eastward over the central Gulf of Mexico and continued to deepen, peaking as a Category 1 hurricane with sustained winds of 90 mph (140 km/h) and a minimum barometric pressure of 973 mbar (28.7 inHg).

It moved northwestward, reaching tropical storm strength on October 29, and after turning sharply east, the system attained its peak of 70 mph (110 km/h) winds.

It reached hurricane strength on November 4, peaking as a minimal Category 1 storm while approaching the Azores, but weakened prior to passing through the islands.

Agricultural land was flooded in Almirante, Bocas del Toro and streets became inundated in low-lying areas of Puerto Armuelles, Chiriquí.