Tropical Storm One A
broad area of low pressure in the central
Caribbean Sea developed into a
tropical depression early on May 22. The circulation moved northward, and it made landfall in southwest
Haiti around 1200
UTC with winds of . Over the next day, the system crossed
Hispaniola and the
Turks and Caicos Islands with winds unchanged. Turning to the northeast, it strengthened into a tropical storm at 1200 UTC on May 24 while over the southwest
Atlantic. Shortly afterward, the tropical cyclone turned to the north. On May 25, the storm's forward motion slowed to a crawl; within a few hours, the storm attained its estimated peak intensity of , as reported by
reconnaissance aircraft, though no ships reported
gale-force winds. The storm ranks as the deadliest recorded Atlantic tropical cyclone to form in the off-season.
Tropical Storm Two After nearly two months of inactivity, an area of disturbed weather developed in the northern
Gulf of Mexico. was first identified on August 26 about northeast of
Saint John, as ship reports indicated winds of
Force 9. However, it is likely that Able formed much farther east, possibly as a
Cape Verde-type hurricane. The tropical cyclone quickly intensified to a hurricane, and it continued to steadily progress northwest. The storm strengthened into a Category 2 hurricane on August 27, and while turning west-northwestward it continued to intensify. The cyclone peaked as a Category 3 hurricane by 1800 UTC on August 28, which was measured by a
reconnaissance aircraft flight. High tides occurred along the North Carolina coastline, which prompted evacuations and precautions in the area.
Tropical Storm Four (Baker) On August 30, a tropical storm named Baker by the Air Weather Service in real time, was first detected about east of
Barbados, by a ship that reported high easterly seas and winds of
Force 10.
Hurricane Five (Charlie) An area of disturbed weather organized into a tropical storm – named Charlie by the Air Weather Service in real time – on September 1 over the western
Gulf of Mexico. On the morning of September 2, the poorly defined center moved northeast, and Charlie gradually intensified. It attained hurricane intensity on September 3 and then slowly accelerated toward the upper
Gulf Coast. It rapidly reached its peak intensity of , and it crossed the coastline west of
Golden Meadow, Louisiana, on September 4. The center moved inland over
Orleans Parish, and the weakening tropical cyclone diminished to a strong tropical storm prior to moving over southern
Mississippi. Charlie continued to weaken and fell to tropical depression intensity on September 5. The remnants turned to the north, and the circulation dissipated over northwestern
Indiana on September 6. The weather service also noted that abnormally high tides were expected from the
Mississippi River to
Pensacola, as the center was predicted to pass east of New Orleans and move to the west of
Biloxi shortly before dawn. About 1,000 people left their homes in
Terrebonne Parish and took shelter in a courthouse and school buildings in
Houma. Offshore, oil drilling platforms and equipment were destroyed by high seas near Grand Isle. Throughout southeastern Louisiana, beans were destroyed north of
Lake Pontchartrain, while sugar cane and corn were flattened, especially in
Lafourche,
Jefferson,
St. Charles, and
Terrebonne parishes. Pecan and tung nut crops also suffered damage in southeastern
Mississippi. The hurricane produced gusts of at
Moisant Airport, and tides ranged from along the coast from Mississippi to the
Florida panhandle. The maximum tide reached in New Orleans, and winds caused damage to small boats, trees, and power and communication lines. Total damage in the United States reached $900,000. In the former, the hurricane brought winds in excess of , downing power lines and trees. Property damage also resulted from the strong winds, totaling about $400,000. After passing west of Bermuda, the tropical cyclone tracked across numerous shipping lanes. Two ships, the
Leicester and
Gaspar, encountered the hurricane and became stricken in open waters. Though most people were rescued from both ships, six people perished on the former while one died on the latter. Beginning on September 15, the hurricane tracked east of Newfoundland, producing heavy rainfall on land. The precipitation flooded roads and caused streams to overflow, inundating additional areas. On the island, one person were killed. Overall, the hurricane caused eight fatalities. Ten deaths occurred and damage totaled at least $2 million, while other sources estimate "several million dollars." Throughout the state, 1,200 homes were severely damaged or destroyed, while 40 businesses were demolished and 237 suffered impact. There were three deaths and about $12 million in damage, over half of which was inflicted on crops. Throughout the state, 674 homes were severely damaged or destroyed, while 45 other buildings were demolished. Overall, damage in Florida reached $5.5 million and there were no deaths, but 36 injuries, none of which were serious.
Hurricane Ten (George) A tropical storm developed about midway between Bermuda and Puerto Rico on November 8. Designated as George by the Air Weather Service in real time, the storm moved quickly west-northwestward. Early on November 10, George is believed to have reached hurricane intensity after reconnaissance aircraft flights recorded a small area of winds ranging from .
Other systems In addition to the ten systems that became a tropical storm there five other tropical cyclones that failed to strengthen beyond tropical depression strength. A weak broad low pressure area formerly associated with a trough developed into a tropical depression well northeast of the
Lesser Antilles on April 15. A barometric pressure of was observed that day. The depression moved northward and then became stationary by April 17, before degenerating into a trough on the next day. The next tropical depression developed from a northward moving tropical wave over the eastern Gulf of Mexico on July 31. Although the depression continued northward, it cannot be determined if the system made landfall in the
Florida panhandle before dissipating on August 2.
Tampa recorded a 5-minute sustained wind speed of on July 31. On August 13, another tropical depression formed from area of disturbed weather well offshore the
Mid-Atlantic. The system moved rapidly northeastward and became extratropical early on August 14. It may have been a tropical storm, based on barometric pressure of observed by a ship shortly after extratropical transition. On September 16, a trough of low pressure developed into a tropical depression over the western Gulf of Mexico. Unfavorable conditions caused the depression to dissipated by the following day. On September 25, a westward moving tropical wave near the Lesser Antilles began appearing in historical weather map. A reconnaissance aircraft flight into the system when it was over the central Caribbean Sea indicated wind gusts up to , but no circulation. During a separate fight on September 29, it was noted that, "[a] complete search of area shows well-organized circle of storm but open to west and northwest". Although no circulation was detected, westerly winds were reported, making it likely that a tropical depression developed that day over the western Caribbean. Subsequently, the depression moved over the northern
Yucatán Peninsula, which may have disrupted the poorly defined circulation. By October 1, the system entered the Gulf of Mexico, where it began degenerating into an open trough on October 3. Cold air and the development of Hurricane Fox in the western Caribbean prevented re-generation. The remnant low continued northeastward into
North Florida and deepened while producing strong gales along the coasts of North Carolina and
Virginia. It may have lingered until October 8, before being absorbed by Fox. == Season effects ==