Meteorological history | |
---|---|
Formed | September 14,1979 |
Remnant low | September 21,1979 |
Dissipated | September 24,1979 |
Category 1 hurricane | |
1-minute sustained (SSHWS/NWS) | |
Highest winds | 85 mph (140 km/h) |
Lowest pressure | 983 mbar (hPa);29.03 inHg |
Overall effects | |
Fatalities | None |
Damage | Minimal |
Areas affected | Mexico,Florida,Texas |
IBTrACS | |
Part of the 1979 Atlantic hurricane season |
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. [1] 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.
Hurricane Henri developed as Tropical Depression Eighteen in the extreme northwestern Caribbean Sea on September 14 from a tropical wave, which had previously moved off the coast of Africa. [2] The formation of a tropical depression was confirmed by reports from Hurricane Hunters. [3] The depression tracked northward, brushing the eastern portion of the Yucatán Peninsula. After reaching the Gulf of Mexico it turned sharply westward, with a ridge preventing further northward movement. The depression turned southwestward, and intensified into Tropical Storm Henri on September 16. [2]
Tropical Storm Henri continued to intensify as it tracked through the Bay of Campeche. On September 17, the storm turned northwestward after the ridge to its north weakened, and later that day Henri reached hurricane status; six hours later, it reached peak winds of 85 mph (140 km/h) about 150 miles (245 km) northeast of Veracruz. Subsequently, a broad low pressure area developed over the western Gulf of Mexico, causing the motion of Henri to become erratic. On September 18, the cyclone began a steady weakening trend, believed to have been caused by land interaction and the funneling of moisture toward a developing disturbance near the Texas coast. [2] Henri turned eastward on September 19 and weakened to tropical depression status. It failed to regain significant convection, and it turned northeastward along an extended cold front. On September 21, Henri weakened into a remnant low. On September 24, Henri merged with the frontal trough in the northeastern Gulf of Mexico. [4]
Hurricane Henri was one of only four hurricanes to enter the Gulf of Mexico without making landfall during the 20th century. [1] The others were Laurie of 1969, Jeanne of 1980, and Alberto of 1982. [5]
Although Henri did not affect land in any way as a hurricane, the developing system threatened several states along the southwestern coastline in Mexico. [4] Mexican forecasting officials issued an advisory for the Gulf coast towns of Tampico in Tamaulipas, and Tuxpan and Nautla in Veracruz, to evacuate to higher ground. [6] The government of Veracruz issued warnings on radio and television of possible flooding in oil-rich coastlines. [7] The storm affected cleanup operations of the Ixtoc I oil spill as it passed over the spill area, damaging a 310-ton steel cap designed to stop the blowout. [8] Henri caused driving rains, strong winds, and floods in Ciudad del Carmen, Campeche, forcing over 2000 people from their homes. Waters swelled in the town to about 12 inches (305 mm) above sea level. [9] Maximum rainfall recorded in Mexico in association with Henri was 19.59 inches (498 mm) at Solosuchiapan. [10]
The remnants of Henri brought showers and thunderstorms to west-central Florida, causing river flooding and some evacuations. [11]
The 2001 Atlantic hurricane season was a fairly active Atlantic hurricane season that produced 17 tropical cyclones, 15 named storms, nine hurricanes, and four major hurricanes. The season officially lasted from June 1, 2001, to November 30, 2001, dates which by convention limit the period of each year when tropical cyclones tend to form in the Atlantic Ocean basin. The season began with Tropical Storm Allison on June 4, and ended with Hurricane Olga, which dissipated on December 6. The most intense storm was Hurricane Michelle, which attained Category 4 strength on the Saffir–Simpson Hurricane Scale.
The 1959 Atlantic hurricane season had a then record-tying number of tropical cyclones – five – develop before August 1. The season was officially to begin on June 15, 1959 and last until November 15, 1959, the period of each year when most tropical cyclones form in the Atlantic basin, however in actuality the season began early when Tropical Storm Arlene formed on May 28. Tropical Storm Arlene struck Louisiana and brought minor flooding to the Gulf Coast of the United States. The next storm, Beulah, formed in the western Gulf of Mexico and brought negligible impact to Mexico and Texas. Later in June, an unnamed hurricane, nicknamed the Escuminac disaster, caused minor damage in Florida and devastated coastal Nova Scotia and New Brunswick, after becoming extratropical. 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 1963 Atlantic hurricane season featured one of the deadliest tropical cyclones on record in the Atlantic basin: Hurricane Flora. The season 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. It was a slightly below average season in terms of tropical storms, with a total of ten nameable storms. The first system, an unnamed tropical storm, developed over the Bahamas on June 1. In late July, Hurricane Arlene, developed between Cape Verde and the Lesser Antilles. The storm later impacted Bermuda, where strong winds resulted in about $300,000 (1963 USD) in damage. Other storms such as hurricanes Beulah and Debra, as well as an unnamed tropical storm, did not impact land. During the month of September, Tropical Storm Cindy caused wind damage and flooding in Texas, leaving three deaths and approximately $12.5 million in damage. Hurricane Edith passed through the Lesser Antilles and the eastern Greater Antilles, causing 10 deaths and about $43 million in damage, most of which occurred on Martinique.
The 1973 Atlantic hurricane season was the first season to use the Saffir–Simpson hurricane scale, a scale developed in 1971 by Herbert Saffir and Robert Simpson to rate the intensity of tropical cyclones. The season produced 24 tropical and subtropical cyclones, of which only 8 reached storm intensity, 4 became hurricanes, and only 1 reached major hurricane status. Although more active than the 1972 season, 1973 brought few storms of note. Nearly half of the season's storms affected land, one of which resulted in severe damage.
The 1974 Atlantic hurricane season was a near average hurricane season in terms of overall activity, with eleven named storms, of which four became hurricanes. Two of those four 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 1988 Atlantic hurricane season was a near average season that proved costly and deadly, with 15 tropical cyclones directly affecting land. The season officially began on June 1, 1988, and lasted until November 30, 1988, although activity began on May 30 when a tropical depression developed in the Caribbean. The June through November dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. The first cyclone to attain tropical storm status was Alberto on August 8, nearly a month later than usual. The final storm of the year, Tropical Storm Keith, became extratropical on November 24. The season produced 19 tropical depressions of which 12 attained tropical storm status. One tropical storm was operationally classified as a tropical depression but was reclassified in post-analysis. Five tropical cyclones reached hurricane status of which three became major hurricanes reaching Category 3 on the Saffir–Simpson scale.
Hurricane Roxanne was a rare and erratic tropical cyclone that caused extensive flooding in Mexico due to its unusual movement. The seventeenth storm, tenth hurricane, and the fifth and final major hurricane of the very active 1995 Atlantic hurricane season, Roxanne developed in the southwestern Caribbean Sea from an area of low pressure on October 7. The depression curved northward, causing it to avoid landfall in Central America. By October 9, the depression intensified enough to be upgraded to Tropical Storm Roxanne. On the following day, Roxanne turned west-northward, where it promptly intensified into a hurricane. As Roxanne headed generally westward, it began to rapidly deepen and reached Category 3 intensity less than 24 hours after becoming a hurricane. Shortly thereafter, Roxanne made landfall near Cozumel, Mexico at its peak intensity, which caused severe damage.
Hurricane Anita was a powerful Atlantic hurricane during the otherwise quiet 1977 Atlantic hurricane season, and the latest first named storm on record since tropical cyclones were first named in 1950. The first tropical cyclone of the season, Anita developed from a tropical wave on August 29 in the north-central Gulf of Mexico. It tracked westward into an area with conditions favorable for further development, and quickly intensified into a hurricane by late on August 30. Initially, Anita was forecast to strike Texas, though a building ridge turned it to the west-southwest. The hurricane rapidly strengthened to attain peak winds of 175 mph (280 km/h), and on September 2 Anita made landfall in eastern Tamaulipas as a Category 5 hurricane. It quickly weakened as it crossed Mexico, and after briefly redeveloping into a tropical depression in the eastern Pacific Ocean, Anita dissipated on September 4 to the south of the Baja California Peninsula. Anita was the first major hurricane to form in The Gulf of Mexico since Hurricane Ethel of 1960.
The 1956 Atlantic hurricane season featured a decent number of tropical cyclones, although most tropical storms and hurricanes affected land. There were twelve tropical storms, a third of which became hurricanes. One of the hurricanes strengthened to the equivalent of a major hurricane, which is a Category 3 or greater on the Saffir–Simpson scale. The strongest hurricane of the season was Betsy, which was also the most damaging storm of the season: it destroyed 15,000 houses and left $40 million in damage in Puerto Rico. Betsy was also the deadliest of the season, having killed 18 people in the French West Indies, two from a shipwreck in the Caribbean Sea, and 16 in Puerto Rico. Tropical Storm Dora struck Mexico in September and killed 27 people.
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 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.
Tropical Storm Larry was the twelfth named tropical storm in the 2003 Atlantic hurricane season. It was one of eight storms to impact Mexico from either the Pacific or Atlantic oceans in the season. Larry formed in early October from an extratropical storm in the Bay of Campeche, and reached a peak intensity of 65 mph (105 km/h). Due to weak steering currents, the storm moved southward, which resulted in the storm making landfall on the Tabasco coastline. It was the first tropical storm to strike the region since Tropical Storm Brenda in 1973.
Hurricane Irene–Olivia was the first actively tracked tropical cyclone to move into the eastern Pacific Ocean from the Atlantic basin. It originated as a tropical depression on September 11, 1971, in the tropical Atlantic. The cyclone tracked nearly due westward at a low latitude, passing through the southern Windward Islands and later over northern South America. In the southwest Caribbean Sea, it intensified to a tropical storm and later a hurricane. Irene made landfall on southeastern Nicaragua on September 19, and maintained its circulation as it crossed the low-lying terrain of the country. Restrengthening after reaching the Pacific, Irene was renamed Hurricane Olivia, which ultimately attained peak winds of 115 mph (185 km/h). Olivia weakened significantly before moving ashore on the Baja California Peninsula on September 30; the next day it dissipated.
Tropical Storm Delia was the first tropical cyclone on record to make landfall in the same city twice. Forming out of a tropical wave on September 1, 1973, Delia gradually strengthened into a tropical storm as it moved north by September 3. After reaching this strength, the storm turned more westward and further intensified, nearly attaining hurricane status the next day. The storm peaked with winds of 70 mph (110 km/h) and a barometric pressure of 986 mbar. Several hours later, Delia made landfall near Freeport, Texas; however, the storm began to execute a counterclockwise loop, causing it to move back over the Gulf of Mexico. On September 5, the storm made another landfall in Freeport before weakening to a depression. The remnants of Delia eventually dissipated early on September 7 over northern Mexico.
The 2010 Atlantic hurricane season was the first of three consecutive very active Atlantic hurricane seasons, each with 19 named storms. This above average activity included 12 hurricanes, equaling the number that formed in 1969. Only the 2020 and 2005 seasons have had more, at 14 and 15 hurricanes respectively. Despite the high number of hurricanes, not one hurricane hit the United States making the season the only season with 10 or more hurricanes without a United States landfall. The overall tropical cyclone count in the Atlantic exceeded that in the West Pacific for only the second time on record. The season officially began on June 1 and ended on November 30, dates that conventionally delimit the period during each year when tropical cyclone formation is most likely. The first cyclone, Alex intensified into the first June hurricane since Allison in 1995. The month of September featured eight named storms. October featured five hurricanes, including Tomas, which became the latest on record in a calendar year to move through the Windward Islands. Activity was represented with an accumulated cyclone energy (ACE) value of 165 units, which was the eleventh highest value on record at the time. The activity in 2010 was heightened due to a very strong La Niña, which also led to an inactive Pacific hurricane season.
Tropical Storm Hermine caused significant flooding in Mexico during September 1980. The eleventh tropical cyclone and eight named storm of the 1980 Atlantic hurricane season, Hermine developed from a tropical wave that emerged into the Atlantic from the west coast of Africa on September 11. After uneventfully crossing the Atlantic Ocean, the system developed a well-defined circulation while in the Caribbean Sea on September 20 and was then classified as a tropical depression. After becoming a tropical cyclone, the depression steadily strengthened as it tracked nearly due westward. By September 21, it strengthened into Tropical Storm Hermine and brushed the northern coast of Honduras shortly thereafter. It nearly became a hurricane before it made landfall in Belize on September 22. After weakening over the Yucatan Peninsula, Hermine restrengthened to near-hurricane status again over the Gulf of Mexico before making landfall in the Mexican state of Veracruz. Hermine steadily weakened inland and eventually dissipated on September 26.
Tropical Storm Fernand was a short-lived but deadly tropical cyclone that struck parts of Veracruz state, Mexico, causing flash flooding and landslides. The sixth tropical storm of the 2013 Atlantic hurricane season, Fernand developed from the merger of two tropical waves that had moved off the coast of Africa in the Bay of Campeche on August 25. Quickly organizing, the cyclone strengthened into a tropical storm and eventually made landfall on the coast of Mexico as a moderate to strong tropical storm. Fernand persisted for another day inland before dissipating over the mountainous terrain of the country. During its relatively short lifespan, Fernand caused numerous flash floods in its wake which resulted in the deaths of 14 people in and around the areas of Veracruz.
Hurricane Ingrid was one of two tropical cyclones, along with Hurricane Manuel, to strike Mexico within a 24-hour period, the first such occurrence since 1958. Ingrid was the ninth named storm and second hurricane of the 2013 Atlantic hurricane season. It formed on September 12 in the Gulf of Mexico from a broad disturbance that also spawned Manuel in the eastern Pacific. After initially moving westward toward Veracruz, Ingrid turned northeastward away from the coast. Favorable conditions allowed it to attain hurricane status on September 14, and the next day Ingrid attained peak winds of 140 km/h (85 mph). Subsequently, increased wind shear weakened the convection as the storm turned more to the northwest and west. On September 16, Ingrid made landfall just south of La Pesca, Tamaulipas in northeastern Mexico as a strong tropical storm, and dissipated the next day. The hurricane was also the last one to form in the Gulf of Mexico until Hurricane Hermine in 2016.
Hurricane Katia was a strong Atlantic hurricane which became the most intense storm to hit the Bay of Campeche since Karl in 2010. The eleventh named storm and sixth hurricane of the exceptionally active 2017 Atlantic hurricane season, Katia originated on September 5, out of a broad low-pressure area that formed in the Bay of Campeche. Located in an area of weak steering currents, Katia meandered around in the region, eventually intensifying into a hurricane on September 6. The nascent storm eventually peaked as a 105 mph (165 km/h) Category 2 hurricane on the Saffir–Simpson scale while it began to move southwestward. However, land interaction began to weaken the hurricane as it approached the Gulf Coast of Mexico. Early on September 9, Katia made landfall near Tecolutla at minimal hurricane intensity. The storm quickly dissipated several hours later, although its mid-level circulation remained intact and later spawned what would become Hurricane Otis in the Eastern Pacific.