The 1968 Atlantic hurricane season was a below average hurricane season during which only nine nameable storms developed. The season officially began on June 1 and lasted until November 30, dates which conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. Of the named storms, five strengthened into hurricanes; none however intensified into a major hurricane. Only four other seasons since the start of the satellite era—1972, 1986, 1994, and 2013—did not feature a major hurricane. The first system, Hurricane Abby, developed in the northwestern Caribbean on June 1. Abby moved northward and struck Cuba, bringing heavy rainfall and flooding to western portions of the island. Making landfall in Florida on June 4, Abby caused flooding and spawned four tornadoes, but left behind little damage. Overall, the hurricane resulted in six deaths and about $450,000 (1968 USD) in damage. In late June, Tropical Storm Candy brought minor flooding and spawned several tornadoes across portions of the Southern United States. Overall damage from the cyclone reached approximately $2.7 million. 1968 featured two simultaneously active tropical storms during the month of June, a phenomenon that would not occur again until 2023.
Despite three named storms in June, cyclone activity slowed throughout the subsequent month, with only one tropical depression. During late August and early September, Tropical Depression Eleven brought flooding to the Jacksonville area of Florida. Hurricane Gladys, the final and also the strongest named storm of the season, developed in the southwestern Caribbean Sea on October 13. Peaking as a Category 2 on the Saffir–Simpson hurricane wind scale, the system resulted in flooding across western Cuba, particularly in Havana, where the storm caused six deaths and about $12 million in damage. Rough seas, gusty winds, tornadoes, and heavy rainfall resulted in generally minor impact in Florida, with three fatalities and damage totaling $6.7 million. Gladys also provided relief for one of North Carolina's worst droughts. Several other storms left negligible impact on land. Overall, the storms of the season collectively caused approximately $21.9 million in damage and killed 17 people.
Season summary
The Atlantic hurricane season officially began on June 1, with Hurricane Abby developing that day. It was a below average season in which nine tropical or subtropical storms formed, compared to the 1966–2009 average of 11.3 named storms. Five of these reached hurricane strength, slightly below the 1966–2009 average of 6.2. There were no major hurricanes during the season. Despite an active beginning, this season had the fewest hurricane days since 1962. Four hurricanes and one tropical storm made landfall during the season, causing 17 deaths and about $21.8 million in damage. The last storm of the season, a subtropical depression, dissipated on November 25, five days before the official end of hurricane season on November 30.
Tropical cyclogenesis began in June, with three named storms during that monthhurricanes Abby and Brenda and Tropical Storm Candytying several seasons for the most named storms in June. Despite the quick start, activity abruptly slowed, with only a tropical depression in July. The next named storm, Hurricane Dolly, existed from August 10 to August 17, while a tropical depression formed later that month. September was the most active month, with five tropical depressions, two tropical storms, and one subtropical storm, which peaked with an intensity equivalent to a Category 1. In October, Hurricane Gladys became the strongest tropical cyclone of the season, despite maximum sustained winds of only and a minimum barometric pressure of .
The season's activity was reflected with an accumulated cyclone energy (ACE) rating of 45. ACE is, broadly speaking, a measure of the power of the hurricane multiplied by the length of time it existed, so storms that last a long time, as well as particularly strong hurricanes, have high ACEs. It is only calculated for full advisories on tropical systems at or exceeding , which is tropical storm strength.
Systems
Hurricane Abby
The interaction of a mid-tropospheric trough and a cold front spawned a tropical depression on June 1. The initial circulation was not embedded within the convection, but as it moved slowly north-northeastward, it was able to strengthen and become better organized, reaching tropical storm strength on June 2. It crossed the western tip of Cuba, and upon reaching the southeast Gulf of Mexico, Abby gradually strengthened. It attained winds of 65 mph (100 km/h) prior to landfall near Punta Gorda, Florida, on June 4. Abby moved across the state and then reached the western Atlantic, where it briefly attained hurricane status late on June 5. On June 6, it weakened and made another landfall near Fernandina Beach with winds of 65 mph (100 km/h). Abby weakened to a tropical depression as it moved over Georgia, and over the next six days, it drifted over The Carolinas, finally dissipating on June 13 east of Virginia.
As Abby crossed Cuba, moderate rainfall and relatively high winds were reported. In addition, Abby dropped heavy rainfall across the state of Florida, peaking at in Hart Lake. However, the rain was almost entirely beneficial, as Florida was suffering from a severe drought. Despite winds gusts up to , no significant wind damage was reported. Abby spawned several tornadoes in Florida, though losses rarely exceeded $5,000. One twister in Monroe, North Carolina, damaged 20 cars, and destroyed three homes and impacted 20 others. Elsewhere, the storm dropped relatively light rainfall and produced a few tornadoes throughout the Southeastern United States. Overall, the storm caused approximately $450,000 in damage and led to six indirect fatalities.
Hurricane Brenda
The trough that spawned Abby persisted, with another tropical depression developing over the Straits of Florida on June 17. Early the following day, the depression crossed the Florida Keys and later made landfall in a rural area of Monroe County. Wind shear levels became increasingly favorable, causing the depression to maintain its intensity while crossing Florida. Because the heaviest shower and thunderstorm activity remained well offshore the state, little impact was reported. Up to of precipitation fell at the Homestead Experiment Station. At 18:00 UTC on June 19, the depression intensified into a tropical storm while still inland over Central Florida, and six hours later emerged into the Atlantic Ocean near Flagler Beach. Shortly thereafter, a weak trough in the westerlies forced the storm to curve eastward. Intensification then occurred, with Brenda nearing hurricane intensity late on June 21.
At that time and into June 22, the Bermuda high built southwestward as a weak trough passed to the north, resulting in Brenda turning northeastward. With persistent favorable conditions, the storm reached hurricane status at 12:00 UTC on June 23. Early the next day, Brenda attained its peak intensity with maximum sustained winds of 80 mph (130 km/h) and a minimum barometric pressure of . Thereafter, a ridge of high pressure blocked moist air from reaching the storm, causing it to weaken. By June 25, Brenda fell to tropical storm intensity and deteriorated further to a tropical depression on June 26. Later that day, it was absorbed by a large extratropical cyclone, while located about west-southwest of Flores Island in the Azores.
Tropical Storm Candy
A tropical disturbance located in the southwestern Gulf of Mexico developed into a tropical depression on June 22. Gradual strengthening occurred, with the depression being upgraded to Tropical Storm Candy on the following day. At 22:45 UTC, the storm peaked with maximum sustained winds of 70 mph (110 km/h) and a minimum barometric pressure of as it made landfall near Port Aransas, Texas. Moving inland, Candy quickly weakened to a tropical depression late on June 24. However, it persisted for a few more days, until transitioning into an extratropical cyclone over Michigan on June 26.
Due to rainfall from a previous weather system, the ground was already saturated throughout Texas. As a result, Candy caused flooding, with precipitation exceeding in some areas. Minor damage to crops, roads, and bridges was reported in the eastern portions of the state. Agricultural losses alone were slightly less than $2 million. Storm surge along the coast of Texas caused "cuts" on Padre Island. The storm spawned 24 tornadoes, though only one caused significant impact. Candy and its remnants dropped rainfall in 24 other states, reaching as far north as New Hampshire. Overall, Candy caused $2.7 million in damage and no fatalities.
Hurricane Dolly
In late July, a tropical wave emerged into the Atlantic Ocean from the west coast of Africa. After tracking west-northwestward and westward, the wave reached the Straits of Florida on August 9, where it began interacting with an upper-level low. Early on August 10, the system developed into a tropical depression, while located near Andros Island in the Bahamas. By 18:00 UTC that day, the depression strengthened into a tropical storm while heading generally northward over the western Atlantic. Initially, Dolly did not strengthen significantly and was nearly absorbed by a cold front. After paralleling part of the East Coast of the United States, Dolly moved further out to sea. By 12:00 UTC on August 12, Dolly developed into a hurricane, and six hours later attained its initial peak of 85 mph (140 km/h).
Dolly briefly weakened back to a tropical storm on August 13 amid unfavorable atmospheric conditions, only to reattain hurricane intensity on the following day. By 12:00 UTC on August 14, Dolly once again peaked with winds of 85 mph (140 km/h). After maintaining its strength for 18 hours, Dolly began to rapidly weaken and became extratropical on August 16, while about north of the Azores. Impact from Hurricane Dolly was minimal, with only rainfall being reported on land. Precipitation peaked at at Palm Beach International Airport in West Palm Beach, Florida. Although it was mostly limited to the east coast of Florida, isolated areas of rain were reported in the Panhandle and on the west coast. Elsewhere, rainfall from Dolly was also recorded in North and South Carolina, though it did not exceed or reach .
Unnamed tropical storm
An upper-level trough and attendant frontal boundary moved into the western Atlantic on September 8. The next day, an area of low pressure formed on the tail-end of this front and began to organize as it moved westward. Surface observations suggested the formation of a tropical depression by 00:00 UTC on September 10. The newly formed system curved north-northeast in advance of another trough and intensified into a tropical storm while passing offshore the Carolinas. On September 11, it attained peak winds of 65 mph (100 km/h), a strength it maintained while making landfall in Long Island, New York, around 10:00 UTC that day. A few hours later, the storm transitioned into an extratropical cyclone as it became intertwined with a front. It crossed Newfoundland into the North Atlantic, interacting with another non-tropical low before dissipating on September 17.
While the storm passed just offshore the Outer Banks of North Carolina, the depression dropped of precipitation on Bodie Island. Tropical storm-force winds overspread Long Island and Connecticut, including a peak measurement of 58 mph (93 km/h) at Falkner Island.
Tropical Storm Edna