The 1969 Atlantic hurricane season was the most active Atlantic hurricane season since the 1933 season, and was the last year in a positive Atlantic multidecadal oscillation (AMO) period, which would not occur again until 1995. The hurricane season officially began on June 1, and lasted until November 30. Altogether, 12 tropical cyclones reached hurricane strength, the highest number on record at the time; a mark not surpassed until 2005. The season was above-average despite an El Niño, which typically suppresses activity in the Atlantic Ocean, while increasing tropical cyclone activity in the Pacific Ocean. Activity began with a tropical depression that caused extensive flooding in Cuba and Jamaica in early June. On July 25, Tropical Storm Anna developed, the first named storm of the season. Later in the season, Tropical Depression Twenty-Nine caused severe local flooding in the Florida Panhandle and southwestern Georgia in September.
The most significant storm of the season was Hurricane Camille, which peaked as a Category 5 hurricane on August 17 and devastated the Gulf Coast of the United States upon striking Mississippi the next day. Strong winds and storm surge heights especially impacted Mississippi and Louisiana. Later in its duration, the storm caused severe flooding Virginia and West Virginia. Camille alone was responsible for 259 deaths and $1.43 billion. It was the costliest United States hurricane at the time, until Hurricane Agnes in 1972. In early September, Hurricane Francelia caused deadly floods in Central America, with 271 people killed in Central America. Hurricane Inga had the third longest duration of an Atlantic tropical cyclone. The last storm, Hurricane Martha, was the only known tropical cyclone to make landfall in Panama. Martha caused minor flooding in the former and Costa Rica. Overall, the systems of the season collectively caused 535 deaths and over $1.5 billion in losses.
Season summary
The 1969 Atlantic hurricane season officially began on June 1. Of the twenty-three tropical cyclones that developed in the North Atlantic Ocean in 1969, eighteen of them intensified into tropical storms; this was above the 1950–2000 average of 9.6 named storms. In terms of tropical storms, it was the busiest season since 1933. Twelve systems reached hurricane status, a record that stood until there were fifteen named storms in 2005. Three of the hurricanes deepened into major hurricanes, which are Category 3 or higher on the Saffir–Simpson hurricane wind scale. Between 1950 and 2000, there was an average of 2.3 major hurricanes per season. Throughout the season, the U.S. Weather Bureau issued more advisories than in any previous season. Additionally, reconnaissance aircraft were utilized for more flight hours than in any year in the Atlantic basin until that point. The season officially ended on November 30.
Hurricane Camille made landfall in Mississippi on August 18 as a Category 5 hurricane, one of only four tropical cyclones on record to strike the continental United States at that strength, after the 1935 Labor Day hurricane, and addition to: Hurricane Andrew in 1992, and Hurricane Michael in 2018. During the 1969 season, Project Stormfury conducted seeding experiments on Hurricane Debbie, which declined in wind speed by 31% on the first day and by 18% of the following day. With a duration of almost 25 days from September 20 to October 15, Hurricane Inga became the third longest-lasting tropical cyclone on record in the Atlantic, behind only the 1899 San Ciriaco hurricane, and Hurricane Ginger in 1971. On November 24, Hurricane Martha became the first tropical cyclone on record to strike Panama.
The season was above average despite an El Niño, which typically suppresses tropical cyclogenesis in the Atlantic Ocean while increasing activity in the eastern Pacific Ocean. 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. However, the opposite periphery of the shear line inhibits the divergent outflow of a disturbance. This may have increased the number of tropical cyclones developing, while causing other storms to remain weak or dissipate over the deep tropics. Additionally, an abnormally strong mid-tropospheric ridge replaced the southward-displaced westerlies that deterred tropical cyclone formation in 1968. Five hurricanes and two tropical storms made landfall, causing 535 deaths and $1.5 billion in damage; Tropical Depression Twenty-Nine also resulted in damage.
Tropical cyclogenesis began early, with a tropical depression that affected Jamaica. Activity briefly went dormant between June 15 and July 25, when the next depression originated. That same day, the season's first named storm, Anna, developed over the eastern Atlantic. There were five tropical cyclones that formed in the month of August – Blanche, Camille, Debbie, Eve, and Francelia. 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).
September was the most active month of the season, with six tropical cyclones, five of which intensified into a tropical storm – Gerda, Holly, Inga, and an unnamed hurricane. Of the five named storms that originated in October, three intensified into hurricanes, including Kara, Laurie, and an unnamed storm. While an unnamed hurricane existed into November, Martha was the only tropical cyclone to originate in that month. Martha, the last storm of the season, dissipated over Panama on November 25.
The season's activity was reflected with an accumulated cyclone energy (ACE) rating of 149. 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 39 mph (63 km/h), which is the threshold for tropical storm status.
Systems
June tropical depression
A tropical depression developed near the Yucatan Peninsula on June 7. It moved north, reaching western Cuba by the following day. As the depression moved towards Florida, small-craft warnings were issued for the southern coast. The depression made landfall in Florida on June 9 and dissipated shortly thereafter. As a result of 2 to 3 in (51 to 76 mm) rain in Cuba, Radio Havana warned of a flash flood and later reported that three rivers were overflowing in Camagüey. Flooding also forced 1,801 people from their homes. Sustained winds of 15 to 25 mph (24 to 40 km/h) and gusts up to 40 mph (64 km/h) were observed on the island. Impact from the depression in Florida is unknown.
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. A train bound for Kingston was disrupted by the flooded bridge, as was a diesel tram, isolating both trains at Richmond. Furthermore, the former train did not reach its destination due to landslides. The Jamaica Telephone Company reported troubles due to waterlogged telephone lines. Schools and colleges in Kingston suspended classes and motorists in the area had difficulty traveling due to flooded roads. Correspondents from The Gleaner reported heavy rains, which inundated roads, washed away livestock and destroyed crops. On June 9, the Church Welfare Organization of the West Indies Junior Seventh Day Adventists set out food, money and blankets the victims.
July tropical depression
A tropical wave situated about 400 mi (640 km) east of Trinidad developed into a tropical depression on July 25. The depression moved northwestward toward the Lesser Antilles and later that day crossed Barbados with winds of 35 mph (56 km/h). It continued to the northwest and may have struck Martinique on July 26. At 0000 UTC on the following day, the depression dissipated about 30 mi (48 km) west-southwest of Basseterre, Guadeloupe.
Tropical Storm Anna
On July 23, a tropical wave emerged into the Atlantic from the west coast of Africa. By 06:00 UTC on July 25, the system developed into Tropical Depression Twelve. Initially, the depression strengthened slowly while moving west-northwestward. Eventually, it was upgraded to Tropical Storm Anna at 06:00 UTC on July 27. Modest intensification ensued during the next 18 hours, after which Anna maintained winds of 60 mph (97 km/h) for nearly two days. At 12:00 UTC on July 30, Anna began to weaken and moved in a more northwesterly direction. 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.
Anna reorganized into a tropical storm by 12:00 UTC on August 1, but weakened to a tropical depression as it re-curved northeastward on August 2, while situated offshore of the East Coast of the United States. By 18:00 UTC, however, Anna once again regained tropical-storm status, and underwent steady intensification on the following day. At 18:00 UTC on August 3, Anna peaked with winds of 70 mph (110 km/h), and six hours later attained its minimum central pressure of 1,001 mb (29.6 inHg). Anna subsequently weakened and merged with an extratropical low-pressure area on the same day, while centered near Sable Island. The remnants continued rapidly east-northeastward across the Atlantic until becoming unidentifiable on August 5.
August tropical depression
A trough in the western Gulf of Mexico produced an area of thunderstorms. On August 7, a Hurricane Hunters flight observed a circulation, indicating that a tropical depression developed. The system moved southwestward, making landfall near Tuxpan in northeastern Mexico early on August 8. It quickly dissipated after moving ashore.
Hurricane Blanche
A tropical wave was initially tracked about 1,300 mi (2,100 km) east of the Lesser Antilles on August 6. The system curved west-northward on August 6 and eventually moved around the western periphery of the Bermuda high. Late on August 10, a closed circulation developed, indicative of a tropical depression, and by 00:00 UTC on August 11 the system became a tropical storm while located about 530 mi (850 km) east of Wabasso Beach, Florida. 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.
At 00:00 UTC on August 12, Blanche peaked at 85 mph (137 km/h). Afterward, the strong southwesterly current in which Blanche was embedded caused the storm to accelerate northeastward. By 12:00 UTC Blanche lost its tropical characteristics near Sable Island, having developed an asymmetrical wind field. At Sable Island, a weather station reported sustained winds of 51 mph (82 km/h) and gusts up to 69 mph (111 km/h). 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.
Hurricane Debbie
On August 14, a tropical wave developed into a tropical depression while located about midway between the Lesser Antilles and the coast of Africa. The following day, the depression strengthened into Tropical Storm Debbie. By 12:00 UTC on August 16, Debbie became a Category 1 hurricane, and continued intensification led to its first peak of 105 mph (169 km/h) by 18:00 UTC on August 17. Debbie then began oscillating between a Category 1 and a Category 2 hurricane for the next few days, possibly due to being seeded by silver iodide as part of Project Stormfury, though reanalysis suggested that an eyewall replacement cycle was the culprit instead. Debbie was chosen as a test for Project Stormfury because it did not threaten any land, it passed within range of seeding aircraft, and was intense with a distinct eye.
Moving northwestward, Debbie began re-intensifying on August 19, becoming Category 3 hurricane with winds of 115 mph (185 km/h) by 18:00 UTC. By 00:00 UTC on August 20, Debbie peaked with winds of 125 mph (201 km/h), which it maintained for a full day. The storm's minimum barometric pressure of 950 mbar (28 inHg) was measured by hurricane hunters during this timeframe. Debbie curved northeastward as Hurricane Camille moved offshore the East Coast of the United States, weakening to a Category 2 hurricane early on August 21. Gradually losing strength, Debbie passed well to the southeast of Bermuda, although it is believed that if not for the presence of nearby Hurricane Camille, which emerged into the Atlantic from the United States on August 20, Debbie would have likely ended up further west, closer to the island. Debbie accelerated and fell to below Category 2 intensity by 12:00 UTC on August 23. Six hours later Debbie became extratropical while still bearing hurricane-force winds, shortly before passing just offshore Newfoundland. The remnants of Debbie turned northeastward and deteriorated to gale strength late on August 24. About three days later, Debbie's remnants dissipated about 225 mi (362 km) east-northeast of Cape Farewell, Greenland. In Newfoundland, wind gusts up to 85 mph (137 km/h) were observed in St. John's, while rainfall up to 0.98 in (25 mm) was recorded along the Avalon and Bonavista peninsulas. The remnants of Debbie began to lose definition as they accelerated northeastward, while moving over increasingly cold waters. Debbie's remnants finally dissipated west of Norway on August 27.