|2019 Atlantic hurricane season|
Season summary map
|First system formed||May 20, 2019|
|Last system dissipated||November 24, 2019|
|• Maximum winds||185 mph (295 km/h)|
|• Lowest pressure||910 mbar (hPa; 26.87 inHg)|
|Total fatalities||116 total|
|Total damage||> $11.615 billion (2019 USD)|
The 2019 Atlantic hurricane season was the fourth consecutive year of above-average and damaging seasons dating back to 2016. It is tied with 1969 as the fourth-most active Atlantic hurricane season on record in terms of named storms, named storms and 20 tropical cyclones in total, although many were weak and short-lived, especially towards the end of the season. Six of those named storms achieved hurricane status, while three intensified into major hurricanes. The season officially began on June 1 and ended on November 30. These dates historically describe the period each year when most tropical cyclones form in the Atlantic basin and are adopted by convention. However, tropical cyclogenesis is possible at any time of the year, as demonstrated by the formation of Subtropical Storm Andrea on May 20, marking the record fifth consecutive year where a tropical or subtropical cyclone developed before the official start of the season.with 18
The season's first hurricane, Barry, formed in mid-July in the northern Gulf of Mexico and struck Louisiana. Barry caused one death and produced flooding in Arkansas, Louisiana, and Mississippi, with damage totaling about $600 million (2019 USD). Hurricane Dorian, the most intense tropical cyclone of the season, proved to be the costliest natural disaster in the history of the Bahamas, becoming the only Category 5 hurricane to strike the country. Overall, Dorian caused about $4.72 billion in damage and 84 fatalities, mostly in the Bahamas. The 2019 season was the record fourth consecutive season to feature at least one Category 5 hurricane. Fernand left flooding in Mexico, with approximately $383 million in damage and 1 death. Humberto produced extensive damage in Bermuda, totaling at least $25 million.
Drifting over Texas, Imelda resulted in a devastating flood in the eastern portions of the state, with about $5 billion in damage and 5 fatalities. Lorenzo, which became the easternmost Category 5 Atlantic hurricane on record, caused 14 deaths after sinking the French tugboat Bourbon Rhode and 8 other fatalities from rough surf along the East Coast of the United States. With Dorian and Lorenzo both intensifying into Category 5 hurricanes, the season became one of seven to feature multiple Category 5 hurricanes. Additionally, Tropical Storm Nestor caused a tornado outbreak across west Florida in mid-October, leaving $125 million in damage, while a car crash in South Carolina killed three people. Olga caused moderate damage and heavy flooding over the central Gulf Coast and generated hurricane-force wind gusts as far north as Tennessee. The storm left 2 deaths and around $400 million in damage. Hurricane Pablo became the easternmost hurricane formation on record, besting Hurricane Vince in 2005. The season concluded with Tropical Storm Sebastien, which became extratropical on November 24.
Most forecasting agencies projects a near-average or slightly above season, with many expecting near-normal sea surface temperatures but expressing uncertainty about the intensity of El Niño. Ultimately, activity in regards to number of named storms exceeded all forecasts, but the number of hurricanes and major hurricanes remained within the predicted range.
|Record high activity||28||15||7|
|Record low activity||4||2†||0†|
|TSR||December 11, 2018||12||5||2|
|CSU||April 4, 2019||13||5||2|
|TSR||April 5, 2019||12||5||2|
|NCSU||April 16, 2019||13–16||5–7||2–3|
|TWC||May 6, 2019||14||7||3|
|UKMO||May 21, 2019||13*||7*||3*|
|NOAA||May 23, 2019||9–15||4–8||2–4|
|TSR||May 30, 2019||12||6||2|
|CSU||June 4, 2019||14||6||2|
|UA||June 11, 2019||16||8||3|
|TSR||July 4, 2019||12||6||2|
|CSU||July 9, 2019||14||6||2|
|CSU||August 5, 2019||14||7||2|
|TSR||August 6, 2019||13||6||2|
|NOAA||August 8, 2019||10–17||5–9||2–4|
|* June–November only.|
† Most recent of several such occurrences. (See all)
Ahead of and during the season, several national meteorological services and scientific agencies forecast how many named storms, hurricanes, and major hurricanes (Category 3 or higher on the Saffir–Simpson scale) will form during a season and/or how many tropical cyclones will affect a particular country. These agencies include the Tropical Storm Risk (TSR) Consortium of University College London, the National Oceanic and Atmospheric Administration (NOAA) and Colorado State University (CSU). The forecasts include weekly and monthly changes in significant factors that help determine the number of tropical storms, hurricanes, and major hurricanes within a particular year. Some of these forecasts also take into consideration what happened in previous seasons and the state of the El Niño–Southern Oscillation (ENSO). On average, an Atlantic hurricane season between 1981 and 2010 contained twelve tropical storms, six hurricanes, and three major hurricanes, with an accumulated cyclone energy (ACE) index of between 66 and 103 units.
The first forecast for the year was released by TSR on December 11, 2018, which predicted a slightly below-average season in 2019, with a total of 12 named storms, 5 hurricanes, and 2 major hurricanes, due to the anticipated presence of El Niño conditions during the season. CSU released its first forecast on April 4, 2019, predicting a near-average season with 13 named storms, 5 hurricanes and 2 major hurricanes, citing the persistence of the weak El Niño and slightly colder than average sea surface temperatures. On April 5, TSR released an updated forecast that reiterated its earlier predictions. North Carolina State University released their forecast on April 16, predicting slightly-above average activity with 13–16 named storms, 5–7 hurricanes and 2–3 major hurricanes. On May 6, the Weather Company predicted a slightly-above average season, with 14 named storms, 7 hurricanes, and 3 major hurricanes. The UK Met Office released their forecast on May 21, predicting 13 named storms, 7 hurricanes, 3 major hurricanes, and an accumulated cyclone energy of 109 units. On May 23, NOAA released their first prediction, calling for a near-normal season with 9–15 named systems, 4–8 hurricanes, and 2–4 major hurricanes. TSR released an updated forecast on May 30, which increased the number of forecast hurricanes from 5 to 6.
On June 4, CSU updated their forecast to include a total of 14 named storms, 6 hurricanes, and 2 major hurricanes, including Subtropical Storm Andrea. CSU noted continuing uncertainty about the intensity of the El Niño, but also increasing ocean temperatures, which were near-normal by then. The University of Arizona (UA) predicted on June 11 that the season would feature above-average activity – 16 named storms, 8 hurricanes, 3 major hurricanes, and accumulated cyclone energy index of 150 units. On July 4, the TSR released their first mid-season outlook, still retaining their numbers from the previous forecast. CSU released their second mid-season outlook on July 9, with the same remaining numbers from their previous forecast. On August 5, the CSU released their third mid-season outlook, still retaining the same numbers from their previous forecast, albeit slightly revising the numbers of hurricanes from 6 to 7. TSR released their second and final mid-season outlook on August 6, with the only changes of increasing the number of named storms from 12 to 13. On August 8, NOAA released their second prediction with increasing the chances for 10–17 named storms, 5–9 hurricanes, and 2–4 major hurricanes, suggesting above-average activity.
The 2019 Atlantic hurricane season officially began on June 1. The season featured twenty tropical depressions, eighteen of which became tropical or subtropical storms. With eighteen named storms, the season tied with 1969 as the fourth most active since records began. Six of those intensified into hurricanes, with three further strengthening into major hurricanes. It was the fourth consecutive Atlantic hurricane season with above average activity, tying the period of 1998-2001. Five systems developed in the Gulf of Mexico, tying with 1957 and 2003 for the highest number of tropical cyclones forming in that body of water. Factors contributing to abnormally high activity included a stronger west-African monsoon, warmer than average ocean temperatures, and low wind shear, particularly over the western Atlantic and Gulf of Mexico. Overall, the Atlantic tropical cyclones of 2019 collectively resulted in 116 deaths and around $11.62 billion in damage. The season officially ended on November 30, 2019.
Activity began before the official start of the season when Subtropical Storm Andrea formed on May 20. This marked the fifth consecutive year with a pre-season named storm, surpassing the previous record of four between 1951 and 1954. No storms formed in the month of June, but activity resumed in July when Hurricane Barry developed on July 11 and Tropical Depression Three formed on July 22. However, tropical cyclogenesis ceased again for nearly one month, until Tropical Storm Chantal developed on August 20. The month of August featured two other systems, Hurricane Dorian and Tropical Storm Erin, with the former being the most intense tropical cyclone of the season. Dorian peaked as a Category 5 hurricane with maximum sustained winds of 185 mph (295 km/h) and a minimum barometric pressure of 910 mbar (27 inHg ). The 2019 season also marked the fourth consecutive year with at least one Category 5 hurricane in the Atlantic basin, exceeding the previous record of three seasons between 2003 and 2005.
September was the most active month of the season, featuring seven named storms, including Fernand, Gabrielle, Humberto, Imelda, Jerry, Karen, and Lorenzo. 29, Lorenzo became the easternmost Category 5 hurricane on record. The season became only the seventh to feature multiple Category 5 hurricanes, other than in 1932, 1933, 1961, 2005, 2007, and 2017. October featured above average activity, with the formation of Melissa, Nestor, Olga, Pablo, and Rebekah, though none remained a tropical or subtropical cyclone for more than three days. Pablo became the easternmost hurricane on record, reaching that intensity east of the previous record-holder, Vince in 2005. Aside from Rebekah existing into November, the month featured one other system, Tropical Storm Sebastien. Activity during the 2019 Atlantic hurricane season concluded when Sebastian transitioned into an extratropical cyclone on November 24.On September
The seasonal activity was reflected with an Accumulated Cyclone Energy (ACE) index value of 132 units. ACE is, broadly speaking, a measure of the power of a hurricane multiplied by the length of time it existed; therefore, long-lived storms and particularly strong systems result in high levels of ACE. The measure is calculated at full advisories for cyclones at tropical storm strength—storms with winds in excess of 39 mph (63 km/h).
|Subtropical storm (SSHWS)|
|Duration||May 20 – May 21|
|Peak intensity||40 mph (65 km/h) (1-min) 1006 mbar (hPa)|
An upper-level trough originating in the mid-latitudes cut off into a broad upper-level low over Florida on May 17. The low moved eastward over the western Atlantic during the next day as a large area convection formed to its east. It began interacting with low-level vorticity along the western edge of a dissipating cold front on May 19, with the two systems coalescing into a broad area of low pressure by 12:00 UTC on May 20. Convection associated with the low became better organized throughout that day as the system moved northward, with an Air Force reconnaissance later that day flight finding that the system had acquired a well-defined center of circulation, and was producing gale-force winds well away from the center. Based on the aircraft data and the structure of the system, the system became Subtropical Storm Andrea at 18:00 UTC on May 20 about 370 mi (595 km) southwest of Bermuda. However, the cyclone soon began to entrain dry air into its circulation while southwesterly wind shear increased, resulting in a rapid waning of the convection. By 12:00 UTC on May 21, the cyclone degenerated into a remnant low after convection diminished. The remnant low moved east-northeastward through the following day until being absorbed by a cold front about 24 hours later roughly 70 mi (115 km) southwest of Bermuda.
|Category 1 hurricane (SSHWS)|
|Duration||July 11 – July 15|
|Peak intensity||75 mph (120 km/h) (1-min) 993 mbar (hPa)|
A mesoscale convective vortex formed over the Central United States on July 2 and moved slowly eastward, southeastward, and then southwestward, reaching the Gulf of Mexico about a week later. The low, which had a large area of deep convection, gradually organized, becoming a tropical depression around 00:00 UTC on July 11 roughly 190 mi (305 km) south of Mobile, Alabama. With an increase in convective banding on the south side of the cyclone's circulation, the system quickly intensified into Tropical Storm Barry just six hours later. The cyclone moved westward and then west-northwestward along the periphery of a low- to mid-level ridge. Barry's convective structure remained asymmetrical, with nearly all of the convection location south of the circulation due to wind shear and dry air. Around 12:00 UTC on July 13, Barry intensified into a hurricane and peaked with winds of 75 mph (120 km/h). Three hours later, Barry made landfall near Intracoastal City, Louisiana. The system weakened to a tropical storm later on July 13 and to a tropical depression early on July 15, before transitioning into a remnant low over Arkansas by 12:00 UTC on July 15. The low continued north-northeastward until degenerating into a trough over Missouri on the next day.
Barry caused one fatality, with a man killed by a rip current off the coast of the Florida Panhandle on July 15. In Mississippi, abnormally high tides caused minor coastal flooding in the vicinity of Biloxi. Widespread, but minor wind and flood damage occurred across southern Louisiana. However, dozens of homes received extensive flood damage in Calcasieu Parish, where more than 20 people were rescued from floodwaters. Over 300,000 people throughout the state lost electricity. In Arkansas, the storm dropped 16.59 in (421 mm) of precipitation in Dierks. As a result, Barry became the rainiest tropical cyclone in the state's history. Flooding damaged a number of homes, businesses, and roads in a narrow swath of southwestern Arkansas, while several roadways were closed, including a portion of Interstate 30. Damage from Barry totaled roughly $600 million.
|Tropical depression (SSHWS)|
|Duration||July 22 – July 23|
|Peak intensity||35 mph (55 km/h) (1-min) 1013 mbar (hPa)|
A tropical wave moved off the west coast of Africa on July 12, producing minimal convection as it moved westward across the tropical Atlantic for several days thereafter. The wave fractured as it approached the Lesser Antilles on July 18, with the northern portion turning northwestward and the southern portion continuing westward across the Caribbean Sea. The northern portion of the wave produced intermittent disorganized convection until reaching the southeastern Bahamas on July 21. Early the following day, a concentrated area of deep convection developed, resulting in the formation of a tropical depression just east of Andros at 12:00 UTC on July 22. However, environmental conditions caused deep convection to decrease substantially shortly after formation. Although a small area of convection re-developed on July 23, it was insufficient to maintain the cyclone, and it degenerated into an open trough at 12:00 UTC on July 23 about 35 mi (55 km) east-northeast of Cape Canaveral, Florida.
Numerous thunderstorms developed across South Florida on July 23 in association with the tropical depression. A woman was injured by a lightning strike in Aventura by one such storm.
|Tropical storm (SSHWS)|
|Duration||August 20 – August 23|
|Peak intensity||40 mph (65 km/h) (1-min) 1007 mbar (hPa)|
On August 14, a cold front moved across the Southeastern United States, becoming nearly stationary over subsequent days. A small area of low pressure formed over South Carolina early on August 17, progressing northeast into the Atlantic the next day. By 18:00 UTC on August 20, the small system gained enough organization to be declared a tropical depression about 370 mi (595 km) southeast of Halifax, Nova Scotia; six hours later, the depression intensified into Tropical Storm Chantal. The system failed to intensify further and soon encountered colder waters and increasing southwesterly wind shear. Instead, Chantal weakened to a tropical depression early on August 22 and ultimately degenerated to a remnant low by 18:00 UTC the next day The remnant low executed a clockwise loop and dissipated three days later about 830 mi (1,335 km) southeast of Cape Race, Newfoundland.
|Category 5 hurricane (SSHWS)|
|Duration||August 24 – September 7|
|Peak intensity||185 mph (295 km/h) (1-min) 910 mbar (hPa)|
A tropical wave exited the west coast of Africa on August 19 and organized as it moved westward, becoming a tropical depression early on August 24 approximately 805 mi (1,295 km) east-southeast of Barbados. The depression quickly developed curved banding features and intensified into Tropical Storm Dorian later that day while heading west-northwestward. Dry air prevented any significant further intensification and organization for several days. Early on August 27, Dorian struck Barbados as a very compact cyclone with winds of 50 mph (85 km/h) and then passed over Saint Lucia later that day. The mountainous terrain of Saint Lucia disrupted the storm's circulation, though a new circulation formed farther to the north. Dorian resumed organizing while moving northeastward over the Caribbean, with a partial eyewall and inner core developing by August 28. The cyclone reached hurricane intensity at 15:30 UTC on August 28 while striking the eastern tip of Saint Croix in the U.S. Virgin Islands; another landfall occurred on Saint Thomas a few hours later. After emerging into the Atlantic on August 28, Dorian eventually began moving west-northwestward due to an upper-level low moving to the south and a subtropical ridge expanding westward.
Encountering very warm water temperatures, ample moisture, and low wind shear, Dorian began rapidly intensifying on August 30, reaching major hurricane intensity around 18:00 UTC that day. Strengthening further, the cyclone became a Category 5 hurricane at 12:00 UTC on September 1, a few hours prior to making landfall on Elbow Cay in the Abaco Islands with winds of 185 mph (295 km/h); Dorian became the strongest tropical cyclone on record to strike the Bahamas. A weakening high pressure area to the north and collapsing steering currents caused Dorian to move very slowly. The cyclone struck Grand Bahama early on September 2 while still a Category 5 hurricane. The storm weakened due to land interaction and upwelling, falling below major hurricane late on September 3. An eastward-moving, large mid-level trough forced Dorian to move north-northwestward and then northward, causing it to remain offshore Florida. The cyclone re-strengthened into a Category 3 hurricane over the Gulf Stream on September 5, but weakened back to a Category 2 later that day. Dorian then curved northeastward and scraped the Outer Banks of North Carolina on September 6 before moving ashore at Cape Hatteras with winds of 100 mph (155 km/h). Embedded within the mid-latitude flow, the cyclone accelerated northeastward and transitioned into an extratropical cyclone late on September 7. The remnant extratropical storm struck Nova Scotia and later Newfoundland before being absorbed by a extratropical cyclone on September 9.
Throughout the Windward Islands, the storm produced wind gusts up to 61 mph (98 km/h), observed on Martinique. Approximately 4,000 homes lost electricity and many streets became impassable due to flooding. Mostly minor damage occurred in Barbados. Some areas of the U. S. Virgin Islands reported hurricane-force winds, with Buck Island observing sustained winds of 82 mph (132 km/h). Winds from Dorian left island-wide blackouts on Saint Thomas and Saint John, while 25,000 customers lost power on Saint Croix. In the British Virgin Islands, the storm caused flood and wind damage in the outskirts of Road Town. One death occurred in Puerto Rico during preparations for the storm. Gusty winds left roughly 23,000 households without electricity across the island. Dorian inflicted catastrophic damage in some regions of the Bahamas. Approximately 87 percent of the damage nationwide occurred in the Abaco Islands, where the storm struck at peak intensity and generated winds of at least tropical storm-force for more than three days. Around 75 percent of homes there were damaged to some degree. Further, Dorian damaged about 90 percent of infrastructure in Marsh Harbour and obliterated shanty-type homes in the town. Grand Bahama also experienced extreme impacts, with storm surge submerging at least 60 percent of the island. The hurricane severely damaged or destroyed around 300 homes on the island. Throughout the Bahamas, an estimated 13,000 homes suffered severe damage or were completely destroyed, while at least 70,000 people were left homeless. Dorian killed at least 70 people and caused at least $3.4 billion in damage, making it the costliest hurricane in the country's history.
Over 160,000 electrical customers in Florida lost power during the storm. Dorian caused coastal flooding in some areas, especially in immediate oceanfront or riverfront sections of St. Augustine and Jacksonville. Six deaths occurred in the state. Strong winds in South Carolina downed numerous trees and power lines, leaving more than 270,000 residences and workplaces without power. Coastal flooding and flash flooding impacted the Charleston and Georgetown areas. Three tornadoes in Horry County also caused damage. The eastern portions of the state experienced storm surge ranging from 4 to 7 ft (1.2 to 2.1 m), wind gusts up to 110 mph (180 km/h), rainfall totals between 5 and 10 in (130 and 250 mm), and 25 tornadoes. Dare County was particularly hard hit, with 1,126 structures damaged. The storm also destroyed 20-25 percent of the state's tobacco crop. Three deaths were reported in North Carolina. Gusty winds and beach erosion occurred in other states along the East Coast, especially in Delaware and New Jersey. Damage in the United States totaled roughly $1.6 billion. In Canada, the extratropical remnants of Dorian left about 412,000 customers without power in Nova Scotia and another 80,000 in New Brunswick, with the former representing approximately 80 percent of the province. The storm damaged homes, buildings, and boats, as well as downed trees, across Canadian Maritimes, though the worst impacts occurred in Halifax, Moncton, and much of Prince Edward Island. Insured damage alone reached $78.9 million.
|Tropical storm (SSHWS)|
|Duration||August 26 – August 29|
|Peak intensity||40 mph (65 km/h) (1-min) 1002 mbar (hPa)|
On August 20, a large upper-level trough with a large area of disorganized convection formed over the southwestern Atlantic. As the trough weakened, a shortwave moved into the western side of the trough over the Gulf of Mexico, resulting in the formation of a broad area of low pressure on August 22. The low drifted northwestward, moving over southeastern Florida on August 24 and degenerating into a trough of low pressure. However, deep convection increased along the trough early on August 26, and a new low developed, with a tropical depression forming at 12:00 UTC that day about 345 mi (555 km) south-southeast of Cape Hatteras, North Carolina. The depression moved southwestward in response to a mid-level high near Florida. Initially poorly-organized due to northwesterly wind shear, the depression strengthened into Tropical Storm Erin late on August 27 following the development of a large burst of convection. Erin then turned sharply northwestward as the mid-level high weakened and a subtropical ridge strengthened to its northeast. Strong upper-level winds weakened the storm to a tropical depression late on August 28. Accelerating northeastward, Erin became extratropical at 12:00 UTC on August 29, and was absorbed by a larger extratropical low 12 hours later.
In Nova Scotia, precipitation from the remnants of Erin was higher than for all of July and August combined before the storm. According to the Meteorological Service of Canada, the Annapolis Valley and the Bay of Fundy region received the most precipitation with a maximum of 6.4 in (162 mm) at Parrsboro and 5.0 in (127 mm) at Greenwood. Several stations reported rates greater than 1.2 in (30 mm), resulting in increased runoff, causing flash floods and the wash out of roads. Rain affected the southern part of New Brunswick with maximum totals of 2.2 in (56 mm) in Fredericton, 2.0 in (50 mm) in Moncton, and 1.7 in (44 mm) in Saint John. In Prince Edward Island, accumulations reached 2.6 in (66 mm) in Summerside. In Quebec, regions near the Gulf of St. Lawrence observed about 2.0 in (50 mm) of rain.
|Tropical storm (SSHWS)|
|Duration||September 3 – September 5|
|Peak intensity||50 mph (85 km/h) (1-min) 1000 mbar (hPa)|
Throughout the latter half of August, an upper-level low progressed eastward from the southeastern United States to Bermuda, southward to Puerto Rico, and westward across Hispaniola and Cuba. A weak and broad area of low pressure formed near western Cuba on August 30 and drifted slowly west across the Gulf of Mexico. Deep convection coalesced within curved bands around the center, leading to the formation of Tropical Storm Fernand around 12:00 UTC on September 3. Despite the influence of moderate east-southeasterly wind shear, the cyclone attained peak winds of 50 mph (85 km/h) by early on September 4 before beginning a steady weakening trend. Fernand progressed south of a ridge over the south-central United States, making landfall about 30 mi (50 km) north-northeast of La Pesca, Tamaulipas, at 15:30 UTC on September 4. It weakened quickly once inland and dissipated over the rugged terrain of Mexico by 06:00 UTC on September 5.
Fernand brought torrential rainfall to the Mexican states of Coahuila, Nuevo León, Tamaulipas, and San Luis Potosí. Fernand also dumped heavy rainfall over South Texas. In preparation for the storm, the Mexican government activated Plan DN-III-E, sending 4,000 troops to the northeastern states to assist in disaster relief. In Nuevo León, schools and public transport lines were closed on September 5 but resumed operations the next day. Of the states, Nuevo León was the hardest hit, suffering at least MX$4.2 billion (US$213 million) in damage. In some places, six months of rain fell in six hours. Landslides were reported near the state's capital, Monterrey. Homes, roads, bridges, and at least 400 schools were damaged. In García, a Venezuelan man died after he was swept away by floodwaters while attempting to clear a drain; the two people he was working with managed to escape. On September 7, governor of Nuevo León, Jaime Rodríguez Calderón, declared a state of emergency to request for state funds to address the damage. Elsewhere, in Tamaulipas, 12 in (300 mm) of rain fell in 48 hours, leading to some localized flooding. Damage throughout Mexico totaled approximately $383 million.
|Tropical storm (SSHWS)|
|Duration||September 3 – September 10|
|Peak intensity||65 mph (100 km/h) (1-min) 995 mbar (hPa)|
A tropical wave moved westward from Africa on August 30, organizing into a tropical depression around 18:00 UTC on September 3 about 455 mi (730 km) west of the northern Capo Verde Islands. The nascent cyclone tracked northwest in an environment of moderate southwesterly wind shear and dry mid-level air, but it nonetheless intensified into Tropical Storm Gabrielle six hours after genesis. Interaction with an upper-level low further compounded negative environmental factors, causing the system to lose a majority of its convection for nearly a day. As the steering regime transitioned to be dictated by a break in the subtropical ridge, Gabrielle curved west-northwest and then north. A decrease in upper-level winds led to the formation of a well-defined inner core, and Gabrielle attained peak winds of 65 mph (100 km/h) on September 8. Thereafter, the influence of mid-latitude westerlies caused the cyclone to turn northeast and begin extratropical transition, a process it completed by 12:00 UTC on September 10 490 mi (790 km) northwest of the western Azores islands. The post-tropical cyclone persisted for a day before degenerating to an open trough.
|Category 3 hurricane (SSHWS)|
|Duration||September 13 – September 19|
|Peak intensity||125 mph (205 km/h) (1-min) 950 mbar (hPa)|
A tropical wave left Africa on August 27 and moved steadily westward for several days. Throughout early September, the wave underwent prolonged interaction with an upper-level trough in the central and southwestern Atlantic that culminated in the formation of a tropical depression at 18:00 UTC on September 13 east of Eleuthera in The Bahamas. The depression intensified into Tropical Storm Humberto six hours later and tracked northwest, where steadily improving environmental conditions allowed it to become a hurricane by September 16. After turning sharply northeast, the storm continued to intensify. At 00:00 UTC on September 18, Humberto attained peak winds of 125 mph (205 km/h), and the Category 3 hurricane passed about 65 mi (100 km) northwest of Bermuda at that intensity. Hostile wind shear and dry air caused Humberto to embark on a weakening trend thereafter, and it transitioned into an extratropical cyclone by 00:00 UTC on September 20 about 575 mi (925 km) south-southwest of Cape Race after being stripped of its convection. The extratropical low was absorbed by a larger non-tropical feature eighteen hours later.
Breezy winds and light rainfall were recorded in The Bahamas, where Hurricane Dorian caused devastation two weeks prior. Humberto's large size contributed to choppy seas along the East Coast of the United States for several days; rip currents killed one person in Florida and a second in North Carolina. In addition, 21 water rescues were performed in St. Johns County, Florida. Tropical storm-force wind gusts, light rainfall, and minor storm surge were felt along the eastern shores of the state. Extensive beach erosion and minor structural damage were reported along the northwestern coast of Puerto Rico. mph (177 km/h), causing widespread damage to trees, roofs, crops, and power lines. As many as 600 buildings—including L.F. Wade International Airport, Royan Naval Dockyard, and the Bermuda Weather Service—suffered damage, around 28,000 customers were left without power, and the island's banana crop suffered a 90 percent loss. Overall, Bermuda reported at least $25 million in damage.On Bermuda, the most significant impacts were wrought by sustained winds up to 110
|Category 2 hurricane (SSHWS)|
|Duration||September 17 – September 24|
|Peak intensity||105 mph (165 km/h) (1-min) 976 mbar (hPa)|
A tropical wave crossed Africa's western coast late on September 11. It spawned an elongated area of low pressure four days later, and that feature gradually organized into a tropical depression by 06:00 UTC on September 17 while located about 1,100 mi (1,770 km) east of the Windward Islands. A strong ridge steered the system west-northwest for several days. Although moderate northeasterly wind shear initially hampered its development, the depression intensified into Tropical Storm Jerry by 06:00 UTC on September 18 and began rapid intensification eighteen hours later. Jerry attained hurricane strength early on September 19 and reached its peak at Category 2 intensity, with winds of 105 mph (165 km/h), early on September 20; this peak was attained despite a fairly asymmetric cloud pattern. Shortly thereafter, increasing upper-level winds and dry air caused the cyclone to weaken while it curved northwest. Jerry fell to tropical storm intensity early on September 21, and it degenerated to a post-tropical cyclone by 18:00 UTC on September 24 roughly 280 mi (450 km) west-southwest of Bermuda, having lost organized deep convection over its center. The remnants of Jerry passed near Bermuda before dissipating northeast of the island on September 28.
|Tropical storm (SSHWS)|
|Duration||September 17 – September 19|
|Peak intensity||45 mph (75 km/h) (1-min) 1003 mbar (hPa)|
An upper-level low detached from a broader trough over the eastern United States in early September, moving southwestward into the eastern Gulf of Mexico by September 12. A weak trough formed in the vicinity of this feature and moved toward the west, ultimately leading to the formation of a tropical depression around 12:00 UTC a short distance southwest of Freeport, Texas, despite the NHC highlighting a low chance of tropical cyclone development. The depression quickly intensified into Tropical Storm Imelda three hours later and peaked with maximum sustained winds of 45 mph (75 km/h) before striking Freeport at 17:45 UTC. Imelda drifted slowly northward once inland, weakening to a tropical depression by 00:00 UTC on September 18 and degenerating into a trough 24 hours later. The remnants of Imelda drifted from southeastern Texas into southeastern Oklahoma over subsequent days before dissipating.
Imelda brought catastrophic flooding to Southeast Texas, with a peak total of 44.29 in (1,125 mm) near Fannett. The storm ranks as the fifth-wettest tropical cyclone to strike the continental United States. Numerous roadways in Greater Houston and eastward became submerged, including Interstate 10, with floodwaters entering thousands of cars. In Jefferson County, flooding resulted in several hundreds of high-water rescues. Approximately 5,100 homes suffered water damage in Jefferson County alone, while roughly 3,100 others were damaged in Harris, Liberty, and Montgomery counties combined. An EF-1 tornado in Harris County ripped off a metal roof and a few tree branches while destroying a barn. Damage from Imelda totaled close to $5 billion. Heavy rainfall also extended eastward into Louisiana, though flooding impact was mostly minor. In Cameron Parish, an EF-0 tornado damaged two recreational vehicles and toppled several trees. The storm caused at least five deaths, all in Texas.
|Tropical storm (SSHWS)|
|Duration||September 22 – September 27|
|Peak intensity||45 mph (75 km/h) (1-min) 1003 mbar (hPa)|
On September 14, a tropical wave emerged into the Atlantic from the west coast of Africa. By early on September 21, a low developed along the axis of the wave, resulting in an increase in deep convection. The system developed a closed center of circulation and became a tropical depression around 00:00 UTC on September 22 roughly 115 mi (185 km) east of Trinidad. About six hours later, the depression intensified into Tropical Storm Karen. The cyclone moved west-northwestward around the southwestern periphery of an Atlantic subtropical ridge and passed through the Windward Islands as a minimal tropical storm late on September 22. Dry air and strong wind shear weakened Karen back to a tropical depression early on September 23 as it turned northward, before re-intensifying into a tropical storm about 24 hours later after encountering favorable conditions again. Late on September 24, Karen struck the Puerto Rican islands of Culebra and Vieques before entering the Atlantic. Tracking north-northeastward, the cyclone eventually began interacting with a surface trough and encountered strong wind shear again. As a result, Karen weakened to a tropical depression on September 27 and dissipated about six hours later approximately 345 mi (555 km) southeast of Bermuda.
With the formation of Karen, tropical storm warnings and red alerts were issued for Trinidad and Tobago. 23. Swells generated by Karen in Venezuela caused flooding and power outages in Caracas and La Guaira. Tropical storm watches were issued for Puerto Rico and the Virgin Islands in anticipation of Karen. Puerto Rico governor Wanda Vázquez Garced declared a state of emergency on September 23 and ordered schools and government offices. The Virgin Islands also closed their schools as the storm approached. People who were living in flood-prone areas were asked to seek shelter. The U.S. Virgin Islands and Puerto Rico experienced heavy rains, mudslides, and power outages, with more than 29,000 people losing power in the latter. Mudslides and runoff blocked several roads in Puerto Rico, especially in Barranquitas, Cayey, and Guayama.Karen brought severe flash floods to Tobago, trapping some people in their houses, as well as uprooting trees and causing several power outages. Several roads were blocked due to mudslides and downed trees. In addition, seven boats in Plymouth sank after a jetty broke. It was also announced that all schools would be closed on September
|Category 5 hurricane (SSHWS)|
|Duration||September 23 – October 2|
|Peak intensity||160 mph (260 km/h) (1-min) 925 mbar (hPa)|
A tropical wave emerged into the Atlantic from the west coast of Africa on September 22. The wave rapidly organized into a tropical depression around 00:00 UTC on September 23 about 320 mi (515 km) southwest of Dakar, Senegal. Six hours later, the depression strengthened into Tropical Storm Lorenzo. A subtropical ridge to the north initially steered the storm westward to west-northwestward. Wind shear interrupted further strengthening on September 24. However, decreasing wind shear on the following day allowed rapid intensification to commence. Lorenzo attained hurricane intensity early on September 25 and then reached an initial peak as a Category 4 hurricane with winds of 145 mph (230 km/h). The system then curved northwestward due to a break in the subtropical ridge. An eyewall replacement cyclone and intruding dry air caused the storm to weaken to a Category 3 hurricane late on September 27. The storm then curved northward across the western end of the subtropical ridge.
After completing the eyewall replacement cyclone, Lorenzo underwent a second bout of rapid intensification. At 03:00 UTC on September 29, the cyclone peaked as a Category 5 hurricane with maximum sustained winds of 160 mph (260 km/h). This made Lorenzo the easternmost Category 5 Atlantic hurricane on record. After reaching peak intensity, Lorenzo began weakening due to upwelling and rapidly increasing southwesterly wind shear. Lorenzo dropped below major hurricane intensity at 18:00 UTC on September 29, only 15 hours after its peak intensity. Lorenzo slowly weakened as it passed the Azores and its windfield expanded the storm began an extratropical transition. Lorenzo became fully extratropical at 12:00 UTC on October 2 roughly 240 mi (385 km) north of Graciosa. On October 3 and October 4, as an extratropical cyclone, the system impacted the British Isles before dissipating entirely.
The French tugboat Bourbon Rhode sank on September 26 near the storm's center with 14 crew members. Search and recovery operations led to the rescue of three people, though four bodies were found and the other seven people were presumed to have drowned. Although the storm remained more than 2,000 mi (3,220 km) offshore the United States, swells and rip currents resulted in eight deaths, with one in Florida, four in North Carolina, two in New York, and one in Rhode Island. In the Azores, Lorenzo caused the worst impacts on Corvo and Flores, with both islands reporting many downed trees and power lines. On the latter, the storm destroyed destroyed the commercial port at Lajes Field. Corvo recorded sustained winds of 74 mph (119 km/h) and gusts reaching 101 mph (163 km/h). Rough seas resulted in the evacuations of about 100 people from their homes throughout the Azores, with waves approaching streets and homes in the city of Horta. In Ireland, the remnants of Lorenzo produced wind gusts up to 66 mph (105 km/h) at the Mace Head Atmospheric Research Station. Downed trees and power lines left roughly 20,000 customers without electricity throughout Ireland.
|Tropical storm (SSHWS)|
|Duration||October 11 – October 14|
|Peak intensity||65 mph (100 km/h) (1-min) 994 mbar (hPa)|
A potent nor'easter, with its origins from the tail-end of a cold front across the southwestern Atlantic on October 6, detached from the boundary and attained maximum winds of 65 mph (100 km/h) by October 10. Deep convection formed north of the low's center, leading to the formation of Subtropical Storm Melissa by 06:00 UTC on October 11 about 205 mi (330 km) south-southeast of Nantucket, Massachusetts. Although peak winds decreased over the next day, the radius of winds contracted significantly while thunderstorm activity became concentrated over the center. This marked Melissa's transition into a tropical storm by 12:00 UTC on October 12. As the system moved east-northeast, it lost its associated convection under the influence of moderate westerly shear and colder water temperatures early on October 14. Melissa soon merged with a nearby front and became extratropical by 12:00 UTC about 370 mi (595 km) south of Cape Race. The post-tropical low degenerated to a trough a few hours later.
The nor'easter and subsequent (sub)tropical storm caused heavy surf and storm surge along the coast of the Mid-Atlantic States. In Maryland, flooding from increased high tides from the storm forced street closures in Crisfield and Salisbury. 3.43 in (87 mm) in Nantucket, Massachusetts. Parts of southeastern Massachusetts experienced sustained tropical-storm-force winds, with a peak sustained wind of 49 mph (80 km/h) and a peak gust of 66 mph (106 km/h) recorded at Wellfleet.In Delaware, waves from the storm caused beach erosion and flooded streets in Bethany Beach while homes and streets were flooded in Dewey Beach. Waves from the storm caused coastal flooding in various parts of the Jersey Shore, including Long Beach Island and Atlantic City. The flooding forced the cancellation of the first day of the LBI International Kite Festival. Rainfall accumulations from the system peaked at
|Tropical depression (SSHWS)|
|Duration||October 14 – October 16|
|Peak intensity||35 mph (55 km/h) (1-min) 1006 mbar (hPa)|
A vigorous late-season tropical wave, accompanied by a broad area of low pressure and a large mass of deep convection, moved off the west coast of Africa on October 13. The broad low separated from the parent wave, moving slowly northwestward as the wave continued westward across the tropical Atlantic. Thunderstorm activity associated with the low became better organized early the following day, resulting in the formation of a tropical depression at 12:00 UTC on October 14 roughly 345 mi (555 km) southeast of the Cabo Verde Islands. As the depression moved northwestward toward the Cape Verde islands, it encountered a hostile environment of high wind shear and abundant dry air, which prevented further strengthening. The depression quickly became poorly organized, and it degenerated into a broad area of low pressure by 06:00 UTC on October 16. The remnant low continued northwestward, producing intermittent convection until its dissipation late on October 17.
|Tropical storm (SSHWS)|
|Duration||October 18 – October 19|
|Peak intensity||60 mph (95 km/h) (1-min) 996 mbar (hPa)|
A tropical wave exited the west coast of Africa on October 3. Convection increased slightly as the wave entered the eastern Caribbean on October 8. Another increase in convection occurred as the wave crossed Central America, partially due to interaction with the Central American gyre. The wave split, with the southern portion becoming Tropical Storm Priscilla in the eastern Pacific basin and the northern portion reaching the Bay of Campeche. A gale-force low formed over the Gulf of Mexico on October 17, which became Tropical Storm Nestor late on October 18. With sustained winds already at 60 mph (95 km/h), the storm moved rapidly northeastward toward the Florida Panhandle. However, an approaching mid- to upper-level trough and associated frontal system caused Nestor to become elongated and left little convection near the center. As a result, Nestor became extratropical around 12:00 UTC on October 19. About five hours later, the extratropical storm made landfall near St. Vincent Island. The remnants of Nestor continued northeastward across the Southeastern United States before dissipating offshore the Delmarva Peninsula on October 21.
Rainfall and storm surge from Nestor caused coastal flooding and flash flooding across the Florida Panhandle and the state's gulf coast. Freshwater flooding inundated several roads in the St. Petersburg area. However, tornadoes also caused significant damage, minutes for a distance of about 11.45 mi (18.43 km)—an uncommonly long track for the region—through western Polk County, from the Lakeland Linder International Airport to northwest Polk County. The twister caused modest damage to homes, overturned a semi-truck on Interstate 4, and ripped off a large portion of a roof of a middle school. In Pinellas County, an EF0 tornado damaged several mobile parks and downed trees in Seminole. An EF1 tornado briefly touched down in northwest Cape Coral, causing damage to 18 homes and vehicles. The fourth tornado, EF0 twister in Brevard County, caused no damage. Heavy rains from Nestor caused a car crash in South Carolina, which killed three people and left five injured. The storm inflicted approximately $125 million in damage throughout the United States.with the storm spawning four in the state. The strongest was rated EF2 and remained on the ground for roughly 30
|Category 1 hurricane (SSHWS)|
|Duration||October 25 – October 28|
|Peak intensity||80 mph (130 km/h) (1-min) 977 mbar (hPa)|
On October 22, a baroclinic low developed over the central Atlantic. The low soon generated gale-force winds, while vorticity centers formed by the following day. The easternmost center became dominate, with convection developing around it by early on October 25. As a result, the low became Subtropical Storm Pablo approximately 405 mi (650 km) west-southwest of the western Azores. Pablo moved east-northeastward and acquired tropical characteristics, becoming a tropical storm late on October 25 after developing central dense overcast and anticyclonic outflow. An eye-like feature also briefly appeared on satellite imagery around this time. The system then curved east-southeastward early on October 26, before turning east-northeastward later that day and then northeastward by October 27. After passing just southeast of the Azores, the storm intensified further and developed more convection and a small eye. Pablo reached hurricane intensity on October 27 and peaked with maximum sustained winds of 80 mph (130 km/h). Pablo reached hurricane intensity at 18.8°W, farther east than any other, breaking Hurricane Vince of 2005's record of 18.9°W. Pablo then weakened due to cold sea surface temperatures, falling to tropical storm intensity early on October 28. The storm then became extratropical after merging with a cold front about 720 mi (1,160 km) north-northeast of the Azores, before dissipating completely on October 29.
|Tropical storm (SSHWS)|
|Duration||October 25 – October 25|
|Peak intensity||45 mph (75 km/h) (1-min) 998 mbar (hPa)|
A well-organized tropical wave crossed the west coast of Africa on October 8 and entered the Atlantic. The wave headed westward with intermittent convection, reaching the Caribbean on October 17 and Central America by October 22. After reaching the Gulf of Mexico, a low-pressure formed on October 24. After scatterometer data and satellite imagery indicated the presence of a closed circulation, the system developed into Tropical Storm Olga at 12:00 UTC on following day roughly 390 mi (630 km) south-southwest of Lake Charles, Louisiana. Olga moved north-northeastward and peaked with winds of 45 mph (75 km/h). However, the storm transitioned into an extratropical cyclone by 00:00 UTC on October 26 after becoming embedded within a cold front. The remnants of the cyclone struck central Louisiana about seven hours later and continued across the Eastern United States and into Ontario, where it dissipated on October 28.
In Louisiana, the remnants of Olga produced sustained winds of 55 mph (89 km/h) and gusts up to 72 mph (116 km/h), the former observed in Baton Rouge and the latter in Mendeville. Gusty winds resulted in 132,000 customers losing electricity. Louisiana also reported up to 10.24 in (260 mm) of precipitation near Ponchatoula, with lesser amounts elsewhere in the state. Hurricane-force wind gusts impacted parts of Mississippi, where the remnants of Olga damaged or destroyed 772 homes, 26 businesses, and 27 roads; Tupelo was particularly hard hit. At least 154,000 power outages occurred in Mississippi. One person died in Newton County when a tree struck him while he while cleaning-up debris. In Tennessee, a wide swath of winds up to 96 mph (154 km/h) caused almost 65,000 power outages, forcing school closures for up to two weeks in several counties. Falling trees resulted in one death in Adamsville. Total damage along the path of the cyclone was estimated at $400 million.
|Subtropical storm (SSHWS)|
|Duration||October 30 – November 1|
|Peak intensity||50 mph (85 km/h) (1-min) 982 mbar (hPa)|
On October 27, a large extratropical cyclone formed about 460 mi (760 km) south of Cape Race. Moving eastward, the cyclone quickly gained hurricane-force winds, before weakening as it turned north and west in a large counterclockwise loop, making another smaller loop on its way. A smaller low-pressure area formed on near the center of the original extratropical cyclone on October 29, possessing a small wind field more characteristic of a tropical cyclone. Deep convection formed around the center of the new low on October 30 due to increased atmospheric instability despite sea surface temperatures of only 70 °F (21 °C), leading to the development of Subtropical Storm Rebekah at 12:00 UTC. The system was designated as a subtropical storm due to a lack of both separation with the parent upper-level low and significant outflow, which are common characteristic of tropical cyclones. At this time, Rebekah possessed sustained winds of 50 mph (85 km/h), representing the system's peak intensity. On October 31, Rebekah turned to the east then east-northeast, entering a region of low relative humidity, increasing wind shear, and even colder sea surface temperatures. The system rapidly weakened as a result of these unfavorable environmental factors. Rebekah became extratropical once again on November 1 at 06:00 UTC and dissipated later that day about 115 mi (185 km) north of the Azores.
|Tropical storm (SSHWS)|
|Duration||November 19 – November 24|
|Peak intensity||70 mph (110 km/h) (1-min) 991 mbar (hPa)|
In late November, a series of mid- to upper-level troughs progressed across the central subtropical Atlantic, giving way to a large area of disturbed weather. Enhanced by a convectively-coupled kelvin wave, the disturbance coalesced over the next few days and was designated as Tropical Storm Sebastien around 06:00 UTC on November 19 to the northeast of the Leeward Islands. The system, initially moving west-northwest, curved toward the east-northeast ahead of an approaching upper-level trough. At the same time, Sebastien gradually intensified despite an impinging cold front and moderate wind shear. The cyclone attained peak winds of 70 mph (110 km/h) early on November 23, when it exhibited a mid-level eye feature. Significantly colder waters and strong shear soon took their toll on Sebastien, causing it to become an extratropical cyclone by 00:00 UTC on November 25. The post-tropical cyclone continued northeast, crossing southwestern Ireland before turning southeast into the Irish Sea and across western England by November 27. The low dissipated just west of London around 18:00 UTC that day.
The following list of names was used for named storms that formed in the North Atlantic in 2019. The names not retired from this list will be used again in the 2025 season. This was the same list used in the 2013 season, with the exception of the name Imelda, which replaced Ingrid. The names Imelda, Nestor, and Rebekah were used for the first time this year. The name Nestor replaced Noel after 2007, but was not used in 2013, while the name Rebekah replaced Roxanne after 1995, but was not used in previous seasons. 30 to April 3, 2020 in Panama, but it was cancelled due to the COVID-19 pandemic.Retired names, if any, will be announced at the 42nd Session of the RA IV Hurricane Committee (also including any names to be retired from the subsequent 2020 season), in the spring of 2021. Originally, retired names were supposed to be announced at the previous session slated to be held from March
This is a table of all the storms that have formed in the 2019 Atlantic hurricane season. It includes their duration, names, affected areas, damages, and death totals. Deaths in parentheses are additional and indirect (an example of an indirect death would be a traffic accident), but were still related to that storm. Damage and deaths include totals while the storm was extratropical, a tropical wave, or a low, and all the damage figures are in USD. Potential tropical cyclones are not included in this table.
|Dates active||Storm category |
at peak intensity
|Andrea||May 20 – 21||Subtropical storm||40 (65)||1006||Bermuda||None||None|
|Barry||July 11 – 15||Category 1 hurricane||75 (120)||993||Midwestern United States, Eastern United States, Louisiana, Arkansas, Oklahoma, Great Lakes region||$600 million||0 (1)|
|Three||July 22 – 23||Tropical depression||35 (55)||1013||The Bahamas, Florida||None||None|
|Chantal||August 20 – 23||Tropical storm||40 (65)||1007||East Coast of the United States||None||None|
|Dorian||August 24 – September 7||Category 5 hurricane||185 (295)||910||Windward Islands, Leeward Islands, Puerto Rico, The Northwestern Bahamas, East Coast of the United States, Eastern Canada||>$4.72 billion||77 (7)|
|Erin||August 26 – 29||Tropical storm||40 (65)||1002||Cuba, The Bahamas, East Coast of the United States, Atlantic Canada||Minimal||None|
|Fernand||September 3 – 5||Tropical storm||50 (85)||1000||Northeastern Mexico, South Texas||$383 million||1|
|Gabrielle||September 3 – 10||Tropical storm||65 (100)||995||Cape Verde, Ireland, United Kingdom||None||None|
|Humberto||September 13 – 19||Category 3 hurricane||125 (205)||950||Hispaniola, Cuba, Bahamas, Southeastern United States, Bermuda, Atlantic Canada, Ireland, United Kingdom||>$25 million||2|
|Jerry||September 17 – 24||Category 2 hurricane||105 (165)||976||Leeward Islands, Puerto Rico, Bermuda||None||None|
|Imelda||September 17 – 19||Tropical storm||45 (75)||1003||Texas, Louisiana, Oklahoma, Arkansas||$5 billion||4 (1)|
|Karen||September 22 – 27||Tropical storm||45 (75)||1003||Windward Islands, Trinidad and Tobago, Venezuela, U.S. Virgin Islands, British Virgin Islands, Puerto Rico||Minimal||None|
|Lorenzo||September 23 – October 2||Category 5 hurricane||160 (260)||925||West Africa, Cape Verde, Azores, Ireland, United Kingdom||$362 million||19|
|Melissa||October 11 – 14||Tropical storm||65 (100)||994||Mid-Atlantic States, New England, Nova Scotia||Minimal||None|
|Fifteen||October 14 – 16||Tropical depression||35 (55)||1006||West Africa, Cape Verde||None||None|
|Nestor||October 18 – 19||Tropical storm||60 (95)||996||Central America, Mexico, Southeastern United States||$125 million||0 (3)|
|Olga||October 25||Tropical storm||45 (75)||998||United States Gulf Coast, Louisiana, Alabama, Mississippi||$400 million||1|
|Pablo||October 25 – 28||Category 1 hurricane||80 (130)||977||Azores||None||None|
|Rebekah||October 30 – November 1||Subtropical storm||50 (85)||982||Azores||None||None|
|Sebastien||November 19 – 24||Tropical storm||70 (110)||991||Leeward Islands, Azores, British Isles||None||None|
|20 systems||May 20 – November 24||185 (295)||910||>$11.62 billion||104 (12)|
The 1995 Atlantic hurricane season is the third-most active Atlantic hurricane season on record, tied with 1887, 2010, 2011, and 2012, and only behind the 1933 and the 2005 season. It is also considered to be the start of an ongoing era of high-activity tropical cyclone formation. The season produced twenty-one tropical cyclones, nineteen named storms, as well as eleven hurricanes and five major hurricanes. The season officially began on June 1 and ended on November 30, dates which conventionally delimit the period of each year when most tropical cyclones develop in the Atlantic basin. The first tropical cyclone, Hurricane Allison, developed on June 2, while the season's final storm, Hurricane Tanya, transitioned into an extratropical cyclone on November 1. The very active Atlantic hurricane activity in 1995 was due to La Niña conditions, that influenced a very inactive Pacific hurricane season.
The 2004 Atlantic hurricane season was a very deadly, destructive, and hyperactive 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 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. 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 1991 Atlantic hurricane season was the first season since 1984 in which no hurricanes developed from tropical waves, which are the source for most North Atlantic tropical cyclones. The hurricane season officially began on June 1, and ended on November 30. It was the least active in four years due to higher than usual wind shear across the Atlantic Ocean. The first storm, Ana, developed on July 2 off the southeast United States and dissipated without causing significant effects. Two other tropical storms in the season – Danny and Erika – did not significantly affect land. Danny dissipated east of the Lesser Antilles, and Erika passed through the Azores before becoming extratropical. In addition, there were four non-developing tropical depressions. The second depression of the season struck Mexico with significant accompanying rains.
The 1945 Atlantic hurricane season produced multiple landfalling tropical cyclones. It officially began on June 16 and lasted until October 31, dates delimiting the period when a majority of storms were perceived to form in the Atlantic Ocean. A total of 11 systems were documented, including a late-season cyclone retroactively added a decade later. Five of the eleven systems intensified into hurricanes, and two further attained their peaks as major hurricanes. Activity began with the formation of a tropical storm in the Caribbean on June 20, which then made landfalls in Florida and North Carolina at hurricane intensity, causing one death and at least $75,000 in damage. In late August, a Category 3 hurricane on the modern-day Saffir–Simpson hurricane wind scale struck the Texas coastline, with 3 deaths and $20.1 million in damage. The most powerful hurricane of the season, reaching Category 4 intensity, wrought severe damage throughout the Bahamas and East Coast of the United States, namely Florida, in mid-September; 26 people were killed and damage reached $60 million. A hurricane moved ashore the coastline of Belize in early October, causing one death, while the final cyclone of the year resulted in 5 deaths and $2 million in damage across Cuba and the Bahamas two weeks later. Overall, 36 people were killed and damage reached at least $82.85 million.
The 2005 Pacific hurricane season continued the trend of generally below-average activity that began a decade prior. The season officially began on May 15 in the eastern Pacific, and on June 1 in the central Pacific; it lasted until November 30 in both basins. These dates conventionally delimit the period during each year when most tropical cyclones form in the northeastern Pacific Ocean. Activity began with the formation of Hurricane Adrian, the fourth-earliest-forming tropical storm on record in the basin at the time. Adrian led to flash flooding and several landslides across Central America, resulting in five deaths and $12 million in damage. Tropical storms Calvin and Dora caused minor damage along the coastline, while Tropical Storm Eugene led to one death in Acapulco. In early October, Otis produced tropical storm-force winds and minor flooding across the Baja California peninsula. The remnants of Tropical Depression One-C in the central Pacific, meanwhile, caused minor impacts in Hawaii. The strongest storm of the season was Hurricane Kenneth, which attained peak winds of 130 mph (215 km/h) over the open Pacific. Cooler than average ocean temperatures throughout the year aided in below-average activity through the course of the season, which ended with 15 named storms, 7 hurricanes, 2 major hurricanes, and an Accumulated cyclone energy index of 75 units.
The 2008 Atlantic hurricane season was the most disastrous Atlantic hurricane season since 2005, causing over 1,000 deaths and nearly $50 billion in damage. The season ranked as the third costliest ever at the time, but has since fallen to sixth costliest. It was an above-average season, featuring sixteen named storms, eight of which became hurricanes, and five which further became major hurricanes. It officially started on June 1 and ended on November 30. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. However, the formation of Tropical Storm Arthur caused the season to start one day early. It was the only year on record in which a major hurricane existed in every month from July through November in the North Atlantic. Bertha became the longest-lived July tropical cyclone on record for the basin, the first of several long-lived systems during 2008.
The 2011 Atlantic hurricane season was the second consecutive season to feature the third highest count of tropical storms, but most of the storms were weak. The season was above-average, mostly due to a La Niña that persisted during the previous year. Therefore, the season was tied with 1887, 1995, 2010, and the following 2012 season for the third highest number of tropical storms since record-keeping began in 1851. Although the season featured 19 tropical storms, only 7 of them intensified into hurricanes and 4 of those became major hurricanes: Irene, Katia, Ophelia, and Rina. The season officially began on June 1 and ended on November 30, dates which conventionally delimit the period during each year in which most tropical cyclones develop in the Atlantic Ocean. However, the first tropical storm of the season, Arlene, did not develop until nearly a month later. The final system, Tropical Storm Sean, dissipated over the open Atlantic on November 11.
The 2010 Atlantic hurricane season was the first in a group of three very active Atlantic hurricane seasons. It is tied alongside 1887, 1995, 2011, and 2012 for the third-most active Atlantic hurricane season on record, with 19 tropical storms, only behind the 1933 and the 2005 seasons. The hyperactive season featured 12 hurricanes, tied with 1969 for the second highest total. Only the quintessential 2005 season saw more activity. 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, tying 2002 and 2007 for the record. October featured five hurricanes, just short of the record set in 1870. Finally, Hurricane Tomas became the latest hurricane on record to move through the Windward Islands in late October. 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 very active activity in 2010 was due to a very strong La Niña, which led to a very quiet Pacific hurricane season.
The 2012 Atlantic hurricane season was the final year in a consecutive string of three very active seasons, although many of the storms were weak and short-lived. It is tied with 1887, 1995, 2010, and 2011 for having the third-most named storms on record. It was also the third-costliest season, behind 2005 and 2017. The season officially began on June 1 and ended on November 30, dates that conventionally delimit the period during each year in which most tropical cyclones form in the Atlantic Ocean. However, Alberto, the first system of the year, developed on May 19 – the earliest date of formation since Tropical Storm Ana in 2003. A second tropical cyclone, Beryl, developed later that month. This was the first occurrence of two pre-season named storms in the Atlantic basin since 1951. It moved ashore in North Florida on May 29 with winds of 65 mph (100 km/h), making it the strongest pre-season storm to make landfall in the Atlantic basin. This season marked the first time since 2009 where no tropical cyclones formed in July. Another record was set by Hurricane Nadine later in the season; the system became the fourth-longest-lived tropical cyclone ever recorded in the Atlantic, with a total duration of 22.25 days. The final storm to form, Tony, dissipated on October 25 – however, Hurricane Sandy, which formed before Tony, became extratropical on October 29.
The 2015 Atlantic hurricane season was the last of three consecutive below average Atlantic hurricane seasons. It produced twelve tropical cyclones, eleven named storms, four hurricanes, and two major hurricanes. The Accumulated Cyclone Energy (ACE) for the season was 68% of the long-term median value. The hurricane season officially began on June 1, 2015, and ended on November 30, 2015. These dates historically describe the period each year when most tropical cyclones form in the North Atlantic basin. However, the first named storm, Ana, developed on May 8, nearly a month before the official start of the season, the first pre-season cyclone since Beryl in 2012 and the earliest since Ana in 2003. The season concluded with Kate transitioning into an extratropical cyclone on November 11, almost three weeks before the official end.
The 2013 Atlantic hurricane season was a well below average Atlantic hurricane season and the first since 1994 with no major hurricanes. It was a well below average season for both hurricanes and major hurricanes but it was a slightly above average season for named storms. It was also the first season since 1968 with no storms of at least Category 2 intensity on the Saffir–Simpson hurricane wind scale. The first tropical cyclone of this hurricane season, Andrea, developed on June 5, while the final cyclone, an unnamed subtropical storm, dissipated on December 7. Throughout the year, only two storms—Humberto and Ingrid—reached hurricane intensity; this was the lowest seasonal total since 1982.
The 2014 Atlantic hurricane season was a well below average season in terms of named storms, and an average season in terms of both hurricanes and major hurricanes. It produced nine tropical cyclones, eight named storms, the fewest since the 1997 Atlantic hurricane season, six hurricanes and two major hurricanes. It officially began on June 1, 2014, and ended on November 30, 2014. These dates historically describe the period each year when most tropical cyclones form in the Atlantic basin. The first storm of the season, Arthur, developed on July 1, while the final storm, Hanna, dissipated on October 28, about a month prior to the end of the season.
The 2016 Atlantic hurricane season was the first above-average hurricane season since 2012, producing 15 named storms, 7 hurricanes and 4 major hurricanes. The season officially started on June 1 and ended on November 30, though the first storm, Hurricane Alex which formed in the Northeastern Atlantic, developed on January 12, being the first hurricane to develop in January since 1938. The final storm, Otto, crossed into the Eastern Pacific on November 25, a few days before the official end. Following Alex, Tropical Storm Bonnie brought flooding to South Carolina and portions of North Carolina. Tropical Storm Colin in early June brought minor flooding and wind damage to parts of the Southeastern United States, especially Florida. Hurricane Earl left 94 fatalities in the Dominican Republic and Mexico, 81 of which occurred in the latter. In early September, Hurricane Hermine, the first hurricane to make landfall in Florida since Hurricane Wilma in 2005, brought extensive coastal flooding damage especially to the Forgotten and Nature coasts of Florida. Hermine was responsible for five fatalities and about $550 million (2016 USD) in damage.
The 2017 Atlantic hurricane season was the costliest tropical cyclone season on record, with a damage total of at least $294.92 billion (USD). It was also a hyperactive Atlantic hurricane season, featuring 17 named storms, 10 hurricanes, and 6 major hurricanes, 2017 was the fifth-most active Atlantic hurricane season on record, tied with 1936. Most of the season's damage was due to hurricanes Harvey, Irma, and Maria. Another notable hurricane, Nate, was the worst natural disaster in Costa Rican history. The names Harvey, Irma, Maria, and Nate were retired following the season due to the number of deaths and amount of damage they caused. Collectively, the tropical cyclones were responsible for at least 3,364 deaths—the most fatalities in a single season since 2005. The season also had the highest accumulated cyclone energy (ACE) since 2005, with a record three hurricanes each generating an ACE of over 40: Irma, Jose, and Maria.
The 2018 Atlantic hurricane season was the third in a consecutive series of above-average and damaging Atlantic hurricane seasons, featuring 15 named storms, 8 hurricanes, and 2 major hurricanes, which caused a total of over $50 billion in damages and least 172 deaths. The season officially began on June 1, 2018, and ended on November 30, 2018. These dates historically describe the period each year when most tropical cyclones form in the Atlantic basin and are adopted by convention. However, the formation of Tropical Storm Alberto on May 25 marked the fourth consecutive year in which a storm developed before the official start of the season. The season concluded with Oscar transitioning into an extratropical cyclone on October 31, almost a month before the official end.
The 2013 Atlantic hurricane season was a below-average season, featuring the fewest hurricanes since 1982. Although Tropical Storm Andrea formed on June 5, the season officially began on June 1 and ended on November 30, dates that conventionally delimit the period of each year when most tropical cyclones develop in the Atlantic basin. The season's final storm, an unnamed subtropical storm, dissipated on December 7.
The 2014 Atlantic hurricane season was a below-average Atlantic hurricane season, featuring the fewest named storms since 1997. The season officially began on June 1 and ended on November 30, dates that conventionally delimit the period of each year when most tropical cyclones develop in the Atlantic basin. The season's first storm, Hurricane Arthur, developed on July 1; the season's final storm, Tropical Storm Hanna, degenerated on October 28.
The 2019 Pacific hurricane season was a near average season which produced nineteen named storms, though most were rather weak and short-lived. Only seven hurricanes formed, the fewest since 2010. The season officially began on May 15 in the East Pacific Ocean, and on June 1 in the Central Pacific; they ended on November 30. These dates conventionally delimit the period of each year when most tropical cyclones form in the Pacific basin. However, the formation of tropical cyclones is possible at any time of the year.
Hurricane Dorian was the strongest hurricane to affect the Bahamas on record, causing catastrophic damage in the Abaco Islands and Grand Bahama in early September 2019. The fifth tropical cyclone, fourth named storm, second hurricane, and first major hurricane of the annual hurricane season, Dorian originated from a westward-traveling tropical wave over a thousand miles east of the Windward Islands on August 24. The newly formed Dorian strengthened only gradually over the next few days because of dry air and vertical wind shear. On August 27, Dorian made landfalls on Barbados and St. Lucia before entering the Caribbean Sea. The mountains of St. Lucia seriously disrupted Dorian's structure and caused the system's center to reform north of its previous location. Moving farther north and east than anticipated, Dorian passed east of Puerto Rico on August 28. Simultaneously, relaxing shear and warm sea surface temperatures allowed Dorian to become a Category 1 hurricane as it moved over the United States Virgin Islands. Intensification temporarily stagnated on August 29 before a spurt of rapid deepening began on August 30. During this time, the hurricane turned west-northwestward then westward as a ridge built in the subtropics to the north. Dorian achieved Category 5 intensity – the highest classification on the Saffir–Simpson scale – on September 1. The system reached peak intensity later that day with winds of 185 mph (295 km/h) and a central pressure of 910 mbar while making landfall at Elbow Cay in the Bahamas.
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