Meteorological history | |
---|---|
Formed | November 7,1980 |
Dissipated | November 16,1980 |
Category 2 hurricane | |
1-minute sustained (SSHWS/NWS) | |
Highest winds | 100 mph (155 km/h) |
Lowest pressure | 986 mbar (hPa);29.12 inHg |
Overall effects | |
Fatalities | None direct |
Damage | Minimal |
Areas affected | Gulf of Mexico,Key West,Florida coast |
IBTrACS | |
Part of the 1980 Atlantic hurricane season |
Hurricane Jeanne was a moderate hurricane that formed and dissipated in the Gulf of Mexico without making landfall,only one of four occurrences in the 20th century. The thirteenth tropical cyclone,tenth named storm,and eighth hurricane of the 1980 Atlantic hurricane season,Jeanne developed over the southern Caribbean on November 7. It moved swiftly northward,and it intensified to a tropical storm on November 9. It entered the southern Gulf of Mexico on November 10. Jeanne turned to the west on November 11,and it rapidly intensified to its peak intensity of 100 mph (160 km/h). It weakened on November 12,and its forward motion slowed;the cyclone weakened further to a tropical storm because of dry air intrusion,and it executed a clockwise loop on November 15. It dissipated on November 16.
At the time,Jeanne was one of three November hurricanes in the Gulf of Mexico;it was the first tropical cyclone to attain hurricane strength in the Gulf of Mexico during November. [1] The late season storm surprised maritime interests,and two barges broke free from towing vessels. Indirectly,the hurricane produced heavy precipitation that peaked at 23.28 inches (591 mm) in Key West. Minor beach erosion occurred along the Texas coast, [2] where tides were two to four feet above normal;coastal flooding affected the state,which was heavily impacted by tropical cyclones in August and September. [3] Jeanne caused no deaths.
On the late afternoon of November 7, an area of disturbed weather organized to a tropical depression 60 miles (97 km) east of Atlántico Norte, Nicaragua. [4] Its origins were traced to a tropical wave that originated over western Africa on October 26. [1] Atmospheric conditions resembled an early fall pattern, and a large ridge was situated over the Gulf of Mexico and Southwestern United States. The depression moved northward into the Caribbean Sea, and the environment supported further development. On November 9, the depression strengthened to a 40 mph (64 km/h) tropical storm and was given the name Jeanne. Later, an Air Force reconnaissance aircraft reported a strengthening system; maximum sustained winds increased to 50 mph (80 km/h), and a minimum pressure of 999 mbar was measured. [1] The tropical cyclone moved northward into the southern Gulf of Mexico on November 10. [4] Jeanne's northward movement was blocked by the ridge, and the cyclone slowly turned to the west. On November 11, Jeanne quickly intensified to a minimal hurricane; later, it attained its peak intensity of 100 mph (160 km/h). [1]
On November 12, Jeanne weakened to a Category 1 hurricane. [4] It entered the western Gulf of Mexico, and its forward motion diminished as the ridge moved east. [1] Later, Jeanne diminished to a 65 mph (105 km/h) tropical storm. A developing trough remained west of Jeanne, and the cyclone was embedded in a weak pressure gradient. Although Jeanne briefly re-intensified to 70 mph (110 km/h), an advancing frontal boundary brought dry air over the western Gulf of Mexico. Jeanne weakened to a depression on November 14. It executed a clockwise loop, and it merged with the frontal boundary on November 16. [2]
Some residents on Dauphin Island voluntarily evacuated, spurred by memories of 1979's Hurricane Frederic and Jeanne's northward motion. 3,000 workers evacuated their oil rigs because of Jeanne's high waves. [5] [6] The National Hurricane Center advised small watercraft to remain in ports from Brownsville to Tarpon Springs. Forecasters expected tides of 2 feet above normal in Louisiana, which increased to 4 feet above normal along coastal Texas. [7] In Terrebonne and Lafourche parishes, schools were closed because of uncertainties regarding Jeanne's path. [6] The hurricane center also expected Jeanne to make landfall in southwestern Louisiana, although the hurricane eventually stayed offshore; thousands of residents moved inland, while Civil Defense officials remained alert. Forecasters expected locally heavy rainfall, although they suggested it would remain below 8 inches (200 mm). [8]
The combination of a large high pressure system and Jeanne produced rough seas over the northern Gulf of Mexico; [9] wave heights reached 15 feet (4.6 m). [5] On November 11, a ship reported sustained winds of 110 mph (180 km/h), although this reading was discarded and attributed to intense squalls. [2] In Key West, the storm's outer fringes produced a record-breaking 24-hour rainfall total of 23.28 inches (591 mm); 13.58 inches (345 mm) fell within six hours. [10] It remains the record 24-hour November rainfall total for the city as of 2018. [11] The previous record was set in 1954. [12] The heavy precipitation was attributed to a mesoscale feature; [1] an inflow band intersected with an adjacent stationary front, which also contributed to the deluge. [10] Schools and most businesses were closed, while flights were grounded at Key West International Airport; authorities urged residents to stay home. Telephone and power services were cut to some areas of the city. [12]
Elsewhere, several ships were caught off guard by the late arrival of Jeanne. The cyclone entered the Gulf of Mexico, and two barges broke loose from towing vessels via strong winds and high waves. One barge was an oil rig tender that contained 16 people; it was carried several hundred miles across the central Gulf of Mexico. [1] All crew members survived, and there were no maritime deaths related to the hurricane. [2] Jeanne produced a prolonged period of rough surf and heavy swells along the Texas coast. Tides reached 2 to 4 feet (0.61 to 1.22 m) above normal. [2] The hurricane caused coastal flooding; the worst flooding occurred near Galveston. [3]
Jeanne was one of only four tropical cyclones in the 20th century to attain hurricane status in the Gulf of Mexico without making landfall; the others were Laurie of 1969, [4] Henri of 1979, [13] and Alberto of 1982. [4]
The 2004 Atlantic hurricane season was a very deadly, destructive, and active Atlantic hurricane season, with over 3,200 deaths and more than $61 billion in damage. More than half of the 16 tropical cyclones brushed or struck the United States. Due to the development of a Modoki El Niño – a rare type of El Niño in which unfavorable conditions are produced over the eastern Pacific instead of the Atlantic basin due to warmer sea surface temperatures farther west along the equatorial Pacific – activity was above average. The season officially began on June 1 and ended on November 30, though the season's last storm, Otto, dissipated on December 3, extending the season beyond its traditional boundaries. The first storm, Alex, developed offshore of the Southeastern United States on July 31, one of the latest dates on record to see the formation of the first system in an Atlantic hurricane season. It brushed the Carolinas and the Mid-Atlantic, causing one death and $7.5 million (2004 USD) in damage. Several storms caused only minor damage, including tropical storms Bonnie, Earl, Hermine, and Matthew. In addition, hurricanes Danielle, Karl, and Lisa, Tropical Depression Ten, Subtropical Storm Nicole and Tropical Storm Otto had no effect on land while tropical cyclones. The season was the first to exceed 200 units in accumulated cyclone energy (ACE) since 1995, mostly from Hurricane Ivan, the storm produced the highest ACE. Ivan generated the second-highest ACE in the Atlantic, only behind 1899 San Ciriaco Hurricane.
The 2000 Atlantic hurricane season was a fairly active hurricane season, but featured the latest first named storm in a hurricane season since 1992. The hurricane season officially began on June 1, and ended on November 30. It was slightly above average due to a La Niña weather pattern although most of the storms were weak. It was also the only Season to Include 2 storms in Ireland. The first cyclone, Tropical Depression One, developed in the southern Gulf of Mexico on June 7 and dissipated after an uneventful duration. However, it would be almost two months before the first named storm, Alberto, formed near Cape Verde; Alberto also dissipated with no effects on land. Several other tropical cyclones—Tropical Depression Two, Tropical Depression Four, Chris, Ernesto, Nadine, and an unnamed subtropical storm—did not impact land. Five additional storms—Tropical Depression Nine, Florence, Isaac, Joyce, and Leslie—minimally affected land areas.
The 1998 Atlantic hurricane season was a catastrophic and deadly Atlantic hurricane season, featuring the highest number of storm-related fatalities in over 218 years and some of the costliest ever at the time. The season had above average activity, due to the dissipation of an El Niño event and transition to La Niña conditions. It officially began on June 1 and ended on November 30, dates which conventionally delimit the period during which most tropical cyclones form in the Atlantic Ocean. The season had a rather slow start, with no tropical cyclones forming in June. The first tropical cyclone, Tropical Storm Alex, developed on July 27, and the season's final storm, Hurricane Nicole, became extratropical on December 1.
The 1959 Atlantic hurricane season featured near normal tropical cyclone activity overall. The season officially began on June 15, 1959 and lasted until November 15, 1959. These dates historically described the period in each year when most tropical cyclogenesis occurs in the Atlantic basin. However, the formation of a tropical cyclone is possible at any time of the year, as shown in 1959, by the formation of Tropical Storm Arlene on May 28. Arlene struck Louisiana and brought minor flooding to the Gulf Coast of the United States. The next tropical storm, Beulah, formed in the western Gulf of Mexico and brought negligible impact to Mexico and Texas. Later in June, an unnamed hurricane, caused minor damage in Florida, and then devastated parts of Maritime Canada, resulting in what became known as the Escuminac disaster. Hurricane Cindy brought minor impact to The Carolinas. In late July, Hurricane Debra produced flooding in the state of Texas. Tropical Storm Edith in August and Hurricane Flora in September caused negligible impact on land.
The 1975 Atlantic hurricane season was a near average hurricane season with nine named storms forming, of which six became hurricanes. Three of those six became major hurricanes, which are Category 3 or higher systems on the Saffir–Simpson scale. The season officially began on June 1 and lasted until November 30. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic Ocean.
The 1979 Atlantic hurricane season was the first Atlantic hurricane season to include both male and female names on its list of tropical cyclone names. The season officially began on June 1, and lasted until November 30. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. It was slightly below average, with nine systems reaching tropical storm intensity. The first system, an unnumbered tropical depression, developed north of Puerto Rico on June 9. Two days later, Tropical Depression One formed and produced severe flooding in Jamaica, with 40 deaths and about $27 million (1979 USD) in damage. Tropical Storm Ana caused minimal impact in the Lesser Antilles. Hurricane Bob spawned tornadoes and produced minor wind damage along the Gulf Coast of the United States, primarily in Louisiana, while the remnants caused flooding, especially in Indiana. Tropical Storm Claudette caused extensive flooding in Texas due to torrential rainfall, resulting in two deaths and about $750 million in damage.
The 1980 Atlantic hurricane season featured nine hurricanes, the most since 1969. This hurricane season was fairly active, with sixteen tropical cyclones forming, eleven of which strengthened into named tropical storms. The season officially began on June 1, 1980, and lasted until November 30, 1980. It was the first time since the 1971 season that there were no active tropical cyclones in the Atlantic basin during the month of June. The season occurred during an ENSO-neutral phase, having neither an El Niño nor a La Niña.
The 1949 Atlantic hurricane season was the last season that tropical cyclones were not publicly labeled by the United States Weather Bureau. It officially began on June 15, and lasted until November 15. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. The first storm, a tropical depression, developed in the northern Gulf of Mexico on August 14. The final system, Tropical Storm Sixteen, dissipated in the southwestern Caribbean Sea on November 5. It was a fairly active season, featuring 16 tropical storms and seven hurricanes. Two of these strengthened into major hurricanes, which are Category 3 or higher on the Saffir–Simpson hurricane wind scale.
The 1948 Atlantic hurricane season featured the first tropical cyclone before the month of June since 1940. The season officially began on June 15, 1948, and lasted until November 15, 1948. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. There were 10 tropical cyclones; six storms attained hurricane status, and four storms intensified into major hurricanes, which are Category 3 or higher on the modern-day Saffir–Simpson hurricane wind scale. Operationally, it was believed that a weak tropical disturbance formed over the southeast Bahamas in May and moved northwest into the Georgia coast near Savannah. This system was later excluded from HURDAT. The seventh tropical cyclone was not operationally considered a tropical cyclone, but was later added to HURDAT.
The 1942 Atlantic hurricane season was one of seven seasons to feature multiple hurricane landfalls in Texas. The season officially lasted from June 16, 1942, to October 31, 1942. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. A total of 11 tropical storms from 1943 are listed in the Atlantic hurricane database, with two additional tropical depressions. The first system of the year, a tropical depression, developed over the central Gulf of Mexico on June 3, while the last system, the Belize hurricane, dissipated over the Yucatán Peninsula on November 11. After the depression dissipated on June 3, the season remained dormant until the next system developed two months later. In mid-August, a hurricane struck Texas, causing about $790,000 (1942 USD) in damage.
The 1935 Atlantic hurricane season was a near-normal hurricane season. Altogether, ten tropical cyclones developed, eight of which intensified into tropical storms. Five of those tropical storms strengthened into hurricanes, while three of those reached major hurricane intensity. The season ran from June 1 through November 15, 1935.
The 1922 Atlantic hurricane season was the first season since 1914 in which no hurricanes made landfall in the United States. Although no "hurricane season" was defined at the time, the present-day delineation of such is June 1 to November 30. The first system, a tropical depression, developed on May 12, while the last, also a tropical depression, dissipated on October 31. Of note, seven of the fourteen cyclones co-existed with another tropical cyclone during the season, including three systems being simultaneously active on September 22.
The 1921 Atlantic hurricane season was an active hurricane season, with 12 tropical cyclones forming. Among them, seven became tropical storms, of which five strengthened into hurricanes. Furthermore, two of these strengthened into a major hurricane, Category 3 or higher on the modern-day Saffir–Simpson hurricane wind scale, the most since the 1917 season. The first system, a tropical depression, developed on June 1, while the last, a tropical storm, dissipated on November 25. Of note, three tropical cyclones co-existed with another during the season.
The 1909 Atlantic hurricane season was an average Atlantic hurricane season. The season produced thirteen tropical cyclones, twelve of which became tropical storms; six became hurricanes, and four of those strengthened into major hurricanes. The season's first storm developed on June 15 while the last storm transitioned into an extratropical cyclone on November 14. The most notable storm during the season formed in late August, while east of the Lesser Antilles. The hurricane devastated the Lesser Antilles, the Greater Antilles, and Mexico, leaving around 4,000 fatalities and more than $50 million (1909 USD) in damage.
The 1906 Atlantic hurricane season was an average season. It featured twelve tropical cyclones, eleven of which became storms, six became hurricanes and three became major hurricanes. The first storm of the season, a tropical storm in the northern Caribbean, formed on June 8; although it struck the United States, no major impacts were recorded. July saw a period of inactivity, with no known storms. However, in August, the streak of inactivity ended with two storms, including a powerful hurricane. September brought three storms, including a deadly hurricane, with catastrophic impacts in Pensacola and Mobile. October included three storms, with a powerful hurricane that killed over 200 people. The final storm of the season impacted Cuba in early November and dissipated on November 9. The season was quite deadly, with at least with 381 total recorded deaths.
The 1890 Atlantic hurricane season was among the least active Atlantic hurricane seasons on record. The first tropical cyclone of the season was initially observed on May 27 and the last storm, Hurricane Four, dissipated over Central America on November 1. These dates fall within the period with the most tropical cyclone activity in the Atlantic. The first storm moved slowly north-northwestward, bringing heavy rains and extensive flooding to Cuba, which caused at least three fatalities and at least $1 million (1890 USD) in damage. It dissipated in the Gulf of Mexico on May 29. Tropical cyclogenesis went dormant for nearly two and a half months, until another system was observed near the Windward Islands on August 18. It traversed the Caribbean Sea and Gulf of Mexico, grazing the Yucatan Peninsula and making landfall in Louisiana before dissipating on August 28. Impact from the storm was minimal.
Hurricane Caroline was one of two tropical cyclones to affect northern Mexico during the 1975 Atlantic hurricane season. The third named storm and second hurricane of the season, Caroline developed on August 24 north of the Dominican Republic. The system crossed Cuba and briefly degenerated into a tropical wave due to land interaction. However, upon emergence into the western Caribbean Sea, it was once again designated as a tropical depression after a well-defined circulation was observed on satellite imagery. Moving towards the west-northwest, the cyclone clipped the northern portion of the Yucatán Peninsula before entering the Gulf of Mexico. Caroline was upgraded to a tropical storm on August 29 in the central Gulf of Mexico before rapid intensification began. Early on August 31, Caroline reached its peak intensity with winds of 115 mph (185 km/h), before landfall south of Brownsville, Texas with winds of 105 mph (169 km/h) shortly thereafter. After moving inland, Caroline quickly weakened and dissipated over the mountainous terrain of northeastern Mexico on September 1. There were only two deaths from Caroline, both indirect. However, there was heavy rainfall in southern Texas and Mexico, including almost 12 in (300 mm) at Port Isabel.
Hurricane Henri was a rare tropical cyclone that entered the Gulf of Mexico without having made landfall; it was the second of four times this occurred during the 20th century. The eighth named storm and fifth hurricane of the 1979 Atlantic hurricane season, it formed on September 14 in the northwestern Caribbean Sea. Throughout much of its duration, Henri moved erratically and initially maintained a general westward track. On September 16 it attained tropical storm status, and a day later it reached hurricane status. By two days later, after experiencing hostile conditions, Henri weakened to tropical depression status as it turned to the northeast, before degenerating into a remnant low on September 21. On September 24, it merged with a frontal low in the northeast Gulf of Mexico. Due to its slow and erratic motion, the hurricane forced evacuations along the Mexican coastline. Its remnants brought rainfall and flooding to the Florida Panhandle.
The 1924 Atlantic hurricane season featured the first officially recorded Category 5 hurricane, a tropical cyclone with maximum sustained winds exceeding 155 mph (249 km/h) on the modern-day Saffir–Simpson scale. The first system, Tropical Storm One, was first detected in the northwestern Caribbean Sea on June 18. The final system, an unnumbered tropical depression, dissipated on November 24. These dates fall within the period with the most tropical cyclone activity in the Atlantic. Of the 13 tropical cyclones of the season, six existed simultaneously. The season was average with 11 tropical storms, five of which strengthened into hurricanes. Further, two of those five intensified into major hurricanes, which are Category 3 or higher on the Saffir–Simpson scale.
The meteorological history of Hurricane Jeanne lasted for about two weeks in September 2004. Hurricane Jeanne was the eleventh tropical cyclone, tenth named storm, seventh hurricane, and sixth major hurricane of the 2004 Atlantic hurricane season. It formed from a tropical wave on September 13 near the Lesser Antilles, and encountered favorable enough conditions to reach tropical storm status. Jeanne strengthened further in the eastern Caribbean, becoming a strong tropical storm and developing an eye before striking Puerto Rico on September 15. Remaining well-organized, it attained hurricane status before hitting the eastern tip of the Dominican Republic on September 16.