2011 Atlantic hurricane season

Seasonal summary

The Atlantic hurricane season officially began on June 1, 2011. It was an above average season in which twenty tropical cyclones formed. Nineteen of the twenty depressions attained tropical storm status, tied with 1887, 1995, 2010, and later the 2012 season for the fourth-highest number of named storms since record-keeping began in 1851. Seven of these tropical storms became hurricanes, while four of those hurricanes further intensified into major hurricanes. The season was more active than usual due to lower than average wind shear, warmer than average sea surface temperatures, and the presence of a La Niña. Collectively, the tropical cyclones of this season resulted in nearly $17.44 billion in damage and there were 118 deaths; a majority of it was caused by Hurricane Irene and Tropical Storm Lee. The season officially ended on November 30, 2011. Despite having 19 named storms, the season only generated an average cumulative ACE rating of 126.3.

Tropical cyclogenesis began in the month of June, with Tropical Storm Arlene forming on June 28. After Arlene dissipated on July 1, there was about a two-week lull in activity, before Bret, Cindy, and Don developed in the latter half of July. August was the most active month of the season, featuring eight tropical cyclones – Emily, Franklin, Gert, Harvey, Irene, Tropical Depression Ten, Jose, and Katia. The number of named storms in August was well above the 1944–2010 average of four, and just one short of the record of eight set in 2004 and later in 2012, but the number of hurricanes was below the mean. September was slightly above average, with 5 named storms, 2 hurricanes, and 1 major hurricane and featuring the unnamed tropical storm, Lee, Maria, Nate, Ophelia, and Philippe. Ophelia was the most intense tropical cyclone of the season, peaking as a Category 4 hurricane with winds of 140 mph (225 km/h) and a minimum pressure of 940 mbar (28 inHg). The next two months featured one system each, with Rina developing in October and Sean forming in November. Sean was the final storm of the season and became extratropical on November 11.

Systems

Tropical Storm Arlene

A tropical wave emerged into the eastern Atlantic on June 13. Tracking westward, the disturbance remained disorganized prior to reaching the western Caribbean. Cyclonic rotation became increasingly evident on satellite imagery, though organization was halted by the disturbance's passage over the Yucatán Peninsula on June 26. After emerging into the Bay of Campeche, favorable environmental conditions allowed for the development of Tropical Storm Arlene by 18:00 UTC on June 28. Moving generally westward due to the influence of high pressure to the cyclone's north, Arlene gradually intensified, reaching its peak intensity with maximum sustained winds of 65 mph (105 km/h) and a minimum barometric pressure of 993 mbar (29.3 inHg) at 12:00 UTC on June 30; the strong tropical storm moved ashore in Mexico near Cabo Rojo, Veracruz, about an hour later. Once inland, the center of circulation became increasingly diffuse, and the storm dissipated over the Sierra Madre Mountains early on July 1.

Numerous tropical cyclone watches and warnings were issued for the coastline of Mexico shortly after the formation of Arlene; once inland, all were discontinued. Despite its relatively weak strength, Arlene produced isolated rainfall totals in excess of 9 in (230 mm). High amounts of precipitation led to numerous mudslides and flooding, causing an estimated $223.4 million in damage. A total of 22 deaths were reported in association with Tropical Storm Arlene. Although the center of circulation remained over Mexico, the storm's far-reaching effects brought minimal relief to drought-stricken portions of southern Texas and Florida.

Tropical Storm Bret

An area of low pressure formed on the southern extent of a stalled cold front just off the East Coast of the United States on July 16. Tracking south-southeast, the low-pressure center was initially baroclinic in nature, but quickly transitioned into a warm-core low over the warm waters of the western Atlantic. Decreasing vertical wind shear allowed for the development of convection – shower and thunderstorm activity – atop the low-level circulation, and Dvorak satellite classifications were initiated early on July 17 given the organization on satellite imagery. Following an aircraft reconnaissance flight into the disturbance that afternoon, the National Hurricane Center (NHC) subsequently classified the system as Tropical Depression Two at 18:00 UTC on July 17 about 100 mi (160 km) northwest of Great Abaco Island in the Bahamas. After about six hours, the depression intensified into Tropical Storm Bret.

As the system turned northeastward, the formation of an anticyclone atop Bret's center provided favorable conditions for intensification; accordingly, an eye-like feature and an eyewall – a ring of thunderstorms around the eye where typically the most intense convection associated with a tropical cyclone is located – were noted on microwave satellite imagery during the afternoon hours of July 18. At 18:00 UTC, the system attained its peak intensity with winds of 70 mph (115 km/h) and a minimum barometric pressure of 995 mbar (29.4 inHg). After moving over increasingly cool sea surface temperatures, the cyclone began to gradually weaken. Bret weakened to a tropical depression at around 00:00 UTC on July 22 and no longer met the criteria of a tropical cyclone by 12:00 UTC, while positioned approximately 375 mi (605 km) north of Bermuda. Bret left minimal impact in the Bahamas, with rainfall alleviating drought conditions. Precipitation was also generally beneficial on Bermuda, though minor flooding affected some local businesses in poor-drainage areas.

Tropical Storm Cindy

On July 17, an area of showers and thunderstorms, associated with the same frontal system that spawned Tropical Storm Bret, consolidated around a developing area of low pressure about 345 mi (555 km) west-southwest of Bermuda. Tracking east-northeastward, the system gradually organized and became better defined. The disturbance produced moderate rains while passing south of the territory, peaking at 1.16 in (29 mm); gusty winds were also observed. At 06:00 UTC on July 20, the low developed into a tropical depression east of Bermuda. Embedded within the mid-latitude westerlies, the depression moved northeast and maintained this general direction for the remainder of its existence.

Six hours after formation, the system strengthened into Tropical Storm Cindy. Convection steadily increased over the storm, and a ragged eye-like feature appeared on both visible and microwave satellite imagery. Corresponding with this, Cindy attained its peak intensity late on July 21, with winds of 70 mph (115 km/h) and a barometric pressure of 994 mbar (29.4 inHg). Shortly thereafter, the storm moved over waters cooler than 78.8 °F (26 °C). Throughout July 22, convection diminished and the system transitioned into an extratropical cyclone about 985 mi (1,585 km) southwest of Ireland. The remnants persisted for another 12 hours before degenerating into a trough over the North Atlantic on July 23.

Tropical Storm Don

A tropical wave emerged off the western coast of Africa on July 16. Tracking westward, the disturbance produced sporadic convection, but remained disorganized through its passage into the Caribbean on July 23. Once there, showers and thunderstorms began to develop within an environment marginally conducive for tropical cyclogenesis. A broad area of low pressure formed and consolidated over the northwestern Caribbean Sea, and the NHC subsequently designated Tropical Depression Four on July 27 about 60 mi (95 km) northeast of Cancún, Mexico. The depression quickly intensified into Tropical Storm Don as it moved into the Gulf of Mexico. Steered west-northwestward by a subtropical ridge across over the southeastern United States, Don strengthened initially under low wind shear, attaining a peak intensity with maximum sustained winds of 50 mph (80 km/h) and a minimum barometric pressure of 997 mbar (hPa; 29.44 inHg). Despite low shear, Don was met with a significantly more stable environment as it emerged into the Gulf of Mexico. As Don approached the Texas coast early on July 30, the thunderstorms rapidly diminished due to the combination of wind shear, drier air, and cooler sea surface temperatures just offshore. The winds decreased as the convection dissipated, and Don made landfall on Padre Island National Seashore as a tropical depression at 02:30 UTC on July 30. About three and a half hours later, Don degenerated into a remnant low, and the circulation dissipated six hours after that.

As a tropical cyclone, Don prompted tropical cyclone advisories for the southern Texas coastline. Due to its abrupt weakening prior to landfall, rainfall totals and wind observations along the warned areas were scarce; a maximum precipitation total of 2.56 in (65 mm) was documented near Bay City, Texas, and a peak wind gust of 41 mph (66 km/h) was recorded at Waldron Field. Cotton farmers benefited from what rains that did fall as they harvested their crop. The storm produced storm surge values lower than 2 ft (0.61 m) as well. In Don's final discussion, the National Hurricane Center famously stated that "the cyclone literally evaporated over Texas".

Tropical Storm Emily

A tropical wave emerged off the west coast of Africa on July 25. Tracking westward, the disturbance gradually consolidated as multiple centers of circulation eventually dissipated and a new one formed. A marginally favorable atmospheric environment allowed for convection to develop, and a reconnaissance aircraft flight into the system led to the classification of Tropical Storm Emily around 00:00 UTC on August 2 near Dominica. Turning west-northwestward along the southwest edge of a large subtropical ridge to its northeast, Emily remained relatively disorganized on satellite imagery due to strong westerly wind shear. Despite a large burst of convection south of Hispaniola on August 3, the center of circulation accelerated west-northwestward, with a mid-level center moving inland over the island. At 18:00 UTC the following day, Emily degenerated into a tropical wave.

The mid-level remnants of Emily continued northwestward, with a new area of low pressure developing over the Bahamas. The low regenerated into a tropical depression at 18:00 UTC on August 6; six hours later, it re-intensified into Tropical Storm Emily. However, strong wind shear exposed the center of circulation once again. At 12:00 UTC on August 7, Emily degenerated into a remnant area of low pressure northeast of the Bahamas. Heavy rainfall and landslides in Martinique damaged 29 homes. One indirect death was reported on the island. In Puerto Rico, flooding and mudslides damaged roads, homes, and crops. Additionally, around 18,500 people lost electricity after winds damaged an electrical grid. About $5 million in infrastructural damage occurred, with $55 million in capital losses over. In Dominican Republic, flooding and mudslides left 56 communities isolated and caused three people to drown. Flooding in Haiti damaged over 300 homes and destroyed several cholera treatment centers. One death occurred in the country. The storm brought up to 7.9 in (200 mm) of rainfall to the Bahamas.

Tropical Storm Franklin

A low-pressure area developed in association with a slow-moving frontal boundary over western Atlantic on August 10 and August 11. Tracking northeastward in response to deep southeasterly flow, the disturbance was initially slow to organize, but a marked organization of thunderstorm activity took place on August 12. Thus, Tropical Depression Six developed at 18:00 UTC while situated roughly 260 mi (420 km) north of Bermuda. The system brought unsettled weather to island, with rainfall reaching 0.07 in (1.8 mm) at L.F. Wade International Airport. Moving northeastward, the depression intensified into Tropical Storm Franklin at 06:00 UTC on August 13, following a large burst of convection over its center. Six hours later, Franklin peaked with winds of 45 mph (70 km/h), before encountering increasing wind shear and decreasing ocean temperatures. Rapid deterioration of the storm's structure took place as environmental conditions became increasingly hostile, with convection being sheared well away from the center. Franklin began acquiring extratropical characteristics and completed its transition into an extratropical cyclone late on August 13. The remnants degenerated into a trough of low pressure early on August 16.

Tropical Storm Gert

During the second week of August, a weak low-pressure area, located east of Bermuda, became associated with a synoptic-scale trough. Moving west-southwestward, it interacted with an upper low and eventually developed into a small low pressure by August 13. After the low become very well-defined with a tight circulation and deep convection, it was designated as a tropical depression at 18:00 UTC that day, about 360 mi (580 km) southeast of Bermuda. As the depression curved west-northwestward along the weakening subtropical ridge, it intensified into Tropical Storm Gert early on August 14. As Gert neared Bermuda, a small eye-like feature became apparent on radar imagery. Coinciding with this, Gert reached its peak intensity with winds of 60 mph (95 km/h). Passing roughly 90 mi (145 km) east of Bermuda, Gert brought light rain and winds up to 25 mph (40 km/h). By August 16, convection had mostly dissipated due to increasing wind shear and cooler water temperatures, degenerating into post-tropical cyclone about 500 mi (800 km) northeast of Bermuda. The remnant low dissipated well east of Newfoundland on August 17.

Tropical Storm Harvey

On August 10, a tropical wave emerged into the Atlantic from the west coast of Africa. After moving westward across the Atlantic and Caribbean for several days, the wave developed into a tropical depression about 100 mi (160 km) east-northeast of Cabo Gracias a Dios at the Honduras–Nicaragua border. Tracking over the warm waters of the northwestern Caribbean, the depression strengthened into Tropical Storm Harvey while just offshore Honduras. Additional intensification occurred, with Harvey attaining its peak intensity with winds of 65 mph (105 km/h) prior to landfall in Belize on August 20. Harvey weakened to a tropical depression on August 21, but re-intensified to a tropical storm after emerging into the Bay of Campeche. Early on August 22, it made landfall near Punta Roca Partida, Veracruz, then weakened and dissipated several hours later.

The precursor disturbance produced squally weather and gusty winds throughout the Lesser Antilles. On Saint Croix in the United States Virgin Islands, gusty winds downed trees, which struck power lines, leaving minor electrical outages. Along its path, Harvey dropped heavy rainfall across much of Central America. Strong winds and heavy precipitation were reported in Belize, damaging or destroying homes in Crooked Tree. A tornado in northern Belize also caused wind damage in a few villages. Heavy rains in Mexico triggered numerous landslides, one of which killed three people. Two other fatalities occurred in the country. Landslides and overflowing rivers damaged 36 homes and 334 homes in the states of Chiapas and Veracruz, respectively.

Hurricane Irene

A tropical wave developed into Tropical Storm Irene about 190 mi (305 km) east of the Lesser Antilles early on August 21. The storm made landfall in Saint Croix as a strong tropical storm later that day. Early on August 21, the storm struck Puerto Rico. While crossing the island, Irene strengthened into a Category 1 hurricane. The storm moved parallel to the coast of Hispaniola, continuing to slowly intensify in the process. Shortly before making four landfalls in the Bahamas, Irene peaked as a 120 mph (195 km/h) Category 3 hurricane. Thereafter, the storm slowly weakened as it struck the Bahamas and then curved northward after passing east of Grand Bahama. Irene was downgraded to a Category 1 hurricane before making landfall near Cape Lookout, North Carolina, on August 27. Early on the following day, the storm re-emerged into the Atlantic from southeastern Virginia. Although the cyclone remained a hurricane over water, it weakened to a strong tropical storm while making landfall at Little Egg Inlet in New Jersey on August 28. A few hours later, Irene struck Brooklyn, New York City, while slightly weaker. Early on August 29, Irene became extratropical near the New Hampshire–Vermont state line, before being absorbed by a frontal system over Labrador on August 30.

In Puerto Rico, heavy rainfall caused several rivers burst their banks, damaging roads and crops, particularly in Maunabo and Yabucoa. One death occurred on the island. Strong winds toppled many trees and utility poles, leaving over 1 million people without electricity. Overall, damage in Puerto Rico totaled approximately $500 million. In Dominican Republic, flooding displaced more than 37,700 people and left at least 88 communities isolated. A total of 2,292 homes were damaged, 16 of which were rendered beyond repair. Throughout the country, there were five deaths and about $30 million in damage. In Haiti, brisk winds in the Port-au-Prince area blew down many refuge tents home to victims from the major 2010 earthquake. Two people were killed after being caught in rain-swollen rivers. In the Bahamas, strong winds damaged at least 40 homes on Mayaguana, while dozens of homes on Acklins were destroyed. On Cat Island, the storm caused "millions of dollars" in structural damage and left many people homeless. Damage throughout the Bahamas reached about $40 million.

Irene impacted the East Coast of the United States from Florida to Maine. Rough seas along the coast of Florida resulted in minor beach erosion and the deaths of two people. Overall, damage in Florida, Georgia, and South Carolina was minimal. Eastern North Carolina was lashed with heavy rainfall, strong winds, and abnormally high tides. In all, over 1,100 homes were destroyed and thousands of others were damaged in North Carolina. Damage in the state reached about $1.2 billion. New Jersey was also hit hard by flooding, strong winds, and storm surge. A number of rivers and creeks reached record or near record levels. Winds left approximately 1.6 million people without electricity. About 200,000 buildings and homes across the state suffered some degree of damage. The cost of damage throughout the state was approximately $1 billion.

In New York, winds left almost 350,000 homes and businesses without power in Nassau and Suffolk counties alone, but the state received only minor wind damage overall. Storm surge left hundreds of millions in damage in New York City and on Long Island. Severe flooding occurred in the Catskill Mountains region, with three towns rendered completely uninhabitable. Damage in the state of New York was estimated at over $1.3billion. In Vermont, rainfall totals of 4–7 in (100–180 mm) were common. Approximately 800 homes were damaged or destroyed. Additionally, nearly 2,400 roads and 300 bridges were damaged or washed away, several of which were covered bridges built more than 100 years prior to the storm. Flooding in Vermont was considered the worst since the flood of November 1927, with uninsured losses alone reaching about $733 million. The other states in New England experienced extensive flooding, but to a less degree. The storm left at least 48 deaths and about $14.2 billion in damage in the United States. The remnants of Irene also brought flooding to Canada, especially Quebec. One death and about $130 million in insured damage were reported.

Tropical Depression Ten

A well-organized tropical wave moved into the eastern Atlantic on August 22. Tracking westward at a fast pace, the wave gradually developed shower and thunderstorm activity and a closed center of low pressure. Curved bands extended from the center by 00:00 UTC on August 25, indicating the development of a tropical depression; at this time, the system was centered about 405 mi (650 km) west-southwest of the southernmost Cape Verde Islands. Unfavorable northeasterly shear prevented intensification, with the depression peaking with winds of 35 mph (55 km/h) and a minimum pressure of 1006 mbar (hPa; 29.71 inHg) at the time of formation. As a mid-level ridge to the north of the cyclone weakened, it turned west-northwest while gradually weakening. By late on August 26, little convection existed over the center of circulation. At 00:00UTC on August 27, the depression degenerated into a remnant area of low pressure and dissipated a few hours later after the center deteriorated into a trough.

Tropical Storm Jose

A mesoscale convective system developed north of an upper-level low east-southeast of Bermuda on August 25. A small mid-level area of low pressure formed on the western side of the convective complex later that same day, gradually developing into the lower levels of the atmosphere. As convection near the center of circulation increased in coverage and intensity, the system developed into a tropical depression at 06:00 UTC on August 27. Six hours later, the depression intensified into Tropical Storm Jose. After formation, strong wind shear from nearby Hurricane Irene slowed, and eventually halted, development trends. Jose attained its peak intensity with winds of 45 mph (70 km/h) and a minimum barometric pressure of 1006 mbar (hPa; 29.71 inHg) but slowly weakened thereafter.

Accelerating to the north and northeast, shower and thunderstorm activity gradually diminished, the low-level circulation became exposed, and the NHC determined Jose degenerated into a remnant area of low pressure near 00:00 UTC on August 29, roughly 135 mi (215 km) north-northwest of Bermuda. As a tropical cyclone, Jose produced tropical storm-force wind gusts on the island and several nearby buoys.

Hurricane Katia

A tropical wave developed into a tropical depression about 430 mi (690 km) southwest of the southernmost Cape Verde Islands early on August 29. It intensified into a tropical storm the following day and further developed into a hurricane by September 1, although unfavorable atmospheric conditions hindered strengthening thereafter. As the storm began to recurve over the western Atlantic, favorable conditions allowed Katia to become a major hurricane by September 5 and peak as a Category 4 hurricane with winds of 140 mph (225 km/h). However, internal core processes, increased wind shear, an impinging cold front, and increasingly cool ocean temperatures caused the cyclone to weaken almost immediately. Katia ultimately transitioned into an extratropical cyclone on September 10 about 290 mi (465 km) south-southeast of Newfoundland. At 00:00 UTC on September 13, Katia's remnant merged with a larger extratropical system, over the North Sea.

Although Katia passed well north of the Lesser Antilles, a yellow alert was hoisted for Guadeloupe to notify residents of dangerous seas. Strong rip currents along the East Coast of the United States led to the deaths of two swimmers. After losing its tropical characteristics, Katia prompted the issuance of numerous warnings across Europe. Hurricane-force winds impacted numerous locations, downing trees and power poles, leaving thousands of people without electricity. The storm was responsible for two deaths in the United Kingdom, with one from when a tree fell on a vehicle in County Durham and another during a multi-car accident on the M54 motorway resulting from adverse weather conditions. The post-tropical cyclone caused approximately £100m ($157 million) in damage in the United Kingdom alone.

Unnamed tropical storm

As part of their routine post-season analysis, the NHC identified an additional tropical storm. In late August, an area of convection that formed to the southwest of Bermuda organized into a distinct low-pressure area. At around 00:00 UTC on September 1, a tropical depression formed about 335 mi (540 km) north of Bermuda. It initially drifted erratically northeastward due to its position within a stationary front. Despite moderate southwesterly wind shear, the depression intensified into a tropical storm after about 12 hours, based on an increase of convection over the center. At that time, the storm attained maximum sustained winds of 45 mph (70 km/h) and a minimum barometric pressure of 1,002 mbar (29.6 inHg).

The thunderstorms continued to pulsate, resulting in the winds fluctuating slightly. Additionally, the intermittent nature of the convection, as well as uncertainty on whether it was associated with a cold front, prevented the storm from being classified as a tropical cyclone in real time. On September 2, a Tropical Weather Outlook (TWO) by the NHC stated that "only a slight increase in organization [would] result in the formation of a tropical storm." That day, an approaching trough caused the storm to accelerate northeastward. Cooler waters and increased wind shear stripped away the convection, resulting in the storm becoming extratropical early on September 3. The remnants continued northeastward, with the circulation dissipating by September 4.

Tropical Storm Lee

A tropical wave developed into the season's thirteen tropical depression in the Gulf of Mexico about 255 mi (410 km) southwest of the mouth of the Mississippi River at 00:00 UTC on September 2. About 12 hours later, the depression intensified into Tropical Storm Lee. The cyclone moved slowly north-northwestward and continued to strengthen. However, Lee transitioned into a subtropical storm at 12:00 UTC on September 3 due to a significantly expanded wind field, further interaction with an upper-level low pressure, and weak convection near the center. Around that time, the cyclone peaked with maximum sustained winds of 60 mph (95 km/h) and a minimum barometric pressure of 986 mbar (29.1 inHg). Lee weakened slightly before making landfall near Intracoastal City, Louisiana, at 10:30 UTC on September 4. After moving inland, the storm moved northeastward and merged with a cold front over eastern Louisiana early on September 5. The remnant low dissipated over Georgia by late on the following day.

In Louisiana, storm surge from Lake Pontchartrain flooded more than 150 homes in Jefferson and St. Tammany parishes. Freshwater flooding also occurred in low-lying areas of southeastern Louisiana and southern and central Mississippi due to 10–15 in (250–380 mm) of rainfall across the area. Several roads were inundated, while 35 roads were damaged, 5 of which were washed out, in Neshoba County, Mississippi. The storm spawned 46 tornadoes, one of which damaged about 400 homes in Cherokee County, Georgia. In the Mid-Atlantic, the remnants of Lee produced over 10 in (250 mm) of rainfall in a wide area, causing worse flooding than in June and July 2006 and Hurricane Agnes in 1972. About 100,000 people in Pennsylvania evacuated, including the governor's residence. In Dauphin and Lebanon counties alone, nearly 5,000 dwellings were damaged or demolished. Extensive flooding also occurred in western New York, particularly in Binghamton, Endicott, Johnson City, Owego, Vestal, and Waverly. Overall, Lee resulted in 18 deaths and about $2.8 billion in damage.

Hurricane Maria

A tropical wave developed into a tropical depression about 700 mi (1,100 km) west-southwest of the southern Cape Verde Islands on late September 6. Early the following day, the depression strengthened into Tropical Storm Maria. The system reached winds of 50 mph (80 km/h) on September 8, before encountering stronger wind shear and cooler water temperatures near the Leeward Islands, degenerating into a low-pressure area on September 9. It slowly curved toward the north and northeast around the western periphery of the subtropical ridge, and regained tropical storm status on September 10. Maria further strengthened to attain hurricane status while making its closest approach to Bermuda. The cyclone peaked with winds of 80 mph (130 km/h) on September 16, but soon weakened due to an increase in wind shear and cooler ocean temperatures. Maria made landfall near Cape St. Mary's, Newfoundland, on September 16, before being absorbed by a frontal system later that day.

Despite its poor organization, Maria brought heavy rainfall to portions of the eastern Caribbean, especially Puerto Rico. Numerous roadways and homes were flooded, with 150 dwellings in the Yabucoa area receiving water damage. Many people were forced to evacuate after water and mud began entering their homes. Nearly 16,000 people were without electricity in Puerto Rico. Maria left approximately $1.36 million in damage on the island. In addition, tropical storm-force winds were observed on many of the U. S. Virgin Islands. As the system passed west of Bermuda, brief tropical storm-force sustained winds were recorded, along with higher gusts; rainfall on the island, however, was minimal. In Newfoundland, fairly strong winds were recorded, but rainfall totals were generally minimal.

Hurricane Nate

On September 5 and September 6, a frontal trough stalled in the Bay of Campeche. A low developed and organized sufficiently to be designated as Tropical Storm Nate at 18:00 UTC on September 7. Moving in an erratic motion at a very slow pace, Nate continued to strengthen. Late on September 8, the cyclone intensified into a Category 1 hurricane, peaking with maximum sustained winds of 75 mph (120 km/h) and a minimum barometric pressure of 994 mbar (29.4 inHg). Due to the storm's slow movement, Nate began to upwell cooler waters in its wake, while very dry air began entering into the storm, resulting in weakening. Around 16:00 UTC on September 11, Nate made landfall in Mexico near Tecolutla, Veracruz, with winds of 45 mph (70 km/h). Shortly after making landfall, much of Nate's showers and thunderstorms diminished, with the system generating into a remnant low by 00:00 UTC on September 12, which dissipated about six hours later.

In the Bay of Campeche, 10 oil rig workers evacuated the Trinity II rig, but were forced to abandon their lifeboat. Seven of the ten were rescued, though the other four perished. The storm brought up to 9.84 in (250 mm) of precipitation to southern Veracruz, causing flooding that damaged 839 homes. One person died in the state after being struck by lightning.

Hurricane Ophelia

On September 19, a tropical wave developed into a tropical depression about 1,300 mi (2,100 km) east of the Lesser Antilles. Moving west-northwestward, the depression became Tropical Storm Ophelia on September 21, and strengthened further to reach an initial peak wind speed of 65 mph (105 km/h) on September 22. As the storm entered a region of higher wind shear it began to weaken, and was subsequently downgraded to a remnant low on September 25. The following day, however, the remnants of the system began to reorganize as wind shear lessened, and on September 27, the system became a tropical depression again. Moving northward, Ophelia regained tropical storm status early on September 28, and significantly deepened to attain its peak intensity with maximum sustained winds of 140 mph (225 km/h) on October 2. This peak was short-lived however as the system passed over cooler water temperatures and into an area of high wind shear, causing it to quickly weaken and undergo transition to an extratropical cyclone. Ophelia weakened to a tropical storm early on October 3, and became fully extratropical shortly after. The extratropical low was absorbed by a larger weather system on the following day.

As the system made its closest approach to the Leeward Islands, Ophelia produced over 10 in (250 mm) of rainfall on some islands, leading to mudslides and several road rescues. Light precipitation totals and gusty winds below tropical storm force were observed on Bermuda, while storm surge and dangerous rip currents along the coast caused minimal damage. In Newfoundland, heavy rainfall contributed to floods that destroyed roads and exposed the inadequacy of some repair work in the aftermath of Hurricane Igor, which struck the previous year. Following Ophelia's transition into an extratropical cyclone, residents in the British Isles were urged to prepare for strong winds in excess of 75 mph (120 km/h) and precipitation accumulations up to 4 in (100 mm). In the northern regions of Ireland, a combination of moisture and significantly cooler weather produced several inches of snow, leaving hundreds without electricity.

Hurricane Philippe

On September 23, a well-defined tropical wave emerged off the coast of Africa, associated with plentiful shower and thunderstorm activity. Moving westward and embedded within a favorable environment for development, the wave quickly became organized. On September 24, a tropical depression developed about 290 mi (465 km) south of the southernmost Cape Verde Islands. Later that day, the depression intensified into Tropical Storm Philippe. Strong wind shear from upper-level winds and later on from Ophelia's outflow, as well as periodic entrainment of dry air, kept the cyclone both small and disorganized. Additionally, the low-level circulation was often exposed. Because of this hostile environment, Philippe remained near the minimum for a tropical storm and briefly weakened to a tropical depression on September 28.

The storm began to strengthen significantly by October 1, with an Advanced Scatterometer (ASCAT) pass on the following day confirming that Philippe was a strong tropical storm, contrary to satellite estimates. Despite high wind shear, it briefly strengthened to a hurricane on October 4 when it developed an eye feature, before weakening back to a tropical storm several hours later. Philippe re-acquired hurricane intensity on October 6 and peaked with maximum sustained winds of 90 mph (145 km/h) later that day. However, Philippe weakened to a tropical storm on October 8, before transitioning into an extratropical cyclone later that day. Early on October 9, the remnants extratropical storm was absorbed by larger low-pressure area to the west of the Azores.

Hurricane Rina

A tropical wave emerged into the Atlantic from the west coast of Africa on October 9. After reaching the southwestern Caribbean, convection intensified near the center and organized into a broad low on October 21, possibly due to a cold front that moved into the region. After a marked increase in convection near and west of the center, a tropical depression developed early on October 23 about 60 mi (97 km) north of Isla de Providencia. The depression moved northward into a weakness in a ridge near Florida, caused by a broad mid-level trough over the Southeastern United States. Initially, the depression intensified gradually, becoming Tropical Storm Rina early on October 24. After a decrease in easterly wind shear, however, Rina rapidly deepened while crossing warm waters, reaching hurricane status at 18:00 UTC on October 24 and becoming a major hurricane about 24 hours later. Early on October 26, the storm peaked with winds of 115 mph (185 km/h).

After the storm reaching peak intensity, upper-level winds and wind shear quickly became unfavorable, weakening Rina to a Category 2 later on October 26. While moving west-northwest and northward along the western periphery of the ridge, the cyclone weakened to a tropical storm on October 27. Later that day, Rina curved northward. Around 02:00 UTC on October 28, Rina struck Quintana Roo about 12 mi (19 km) southwest of Playa del Carmen with winds of 60 mph (95 km/h). The storm left little impact in the Yucatán Peninsula due to its weakened state. Rina degenerated into a remnant low late on October 28, upon emerging into the Yucatán Channel. The remnant low dissipated near the western tip of Cuba on October 29. A cold front, combined with moisture from Rina, resulted in 5–7 in (130–180 mm) of rainfall across parts of South Florida in less than six hours, causing street flooding and leaving water damage in at least 160 homes and buildings in Broward County alone. Farther north, two tornadoes touched down in the vicinity of Hobe Sound, one of which damaged 42 mobile homes, 2 vehicles, and a number of trees.

Tropical Storm Sean

A low-pressure area of non-tropical origins developed into Subtropical Storm Sean at 06:00 UTC on November 8 about 445 mi (716 km) southwest of Bermuda. While convection and the wind field had become more symmetric, the system remained a subtropical cyclone due to the associated upper-level low. Within 12 hours, Sean separated from the low and transitioned into a tropical cyclone, after developing a warm core. It developed outflow and intensified due to light wind shear, combined with sufficiently warm water temperatures of at least 78.8 °F (26.0 °C). With a ridge to the northeast, the storm moved slowly to the west. On November 9, an eye feature developed in association with Sean, which later morphed into a ring of convection. The storm peaked with winds of 65 mph (105 km/h) on November 10 as reported by the hurricane hunters. An approaching cold front subsequently induced higher wind shear on the cyclone as it tracked northeastward into cooler waters; this led to weakening. Sean transitioned into an extratropical cyclone on November 11. Early on the next day, it was absorbed by the cold front.

Sean and its precursor produced light rainfall for several days in Bermuda. Shortly after development, the Bermuda Weather Service issued a tropical storm watch, which was later upgraded to a tropical storm warning. When Sean passed near the island on November 11, it produced sustained winds of 43 mph (69 km/h), with gusts to 62 mph (100 km/h). The storm produced rough seas to the east coast of Florida, which drowned one swimmer in Jensen Beach. Rip currents were also observed in North Carolina.

Storm names

The following list of names was used for named storms that formed in the North Atlantic in 2011. This was the same list used in the 2005 season with the exceptions of Don, Katia, Rina, Sean, and Whitney, which replaced Dennis, Katrina, Rita, Stan, and Wilma, respectively. Storms were named Don, Katia, Rina, and Sean for the first time in 2011.

Retirement

On April 13, 2012, at the 34th Session of the RA IV hurricane committee, the World Meteorological Organization retired the name Irene from the Atlantic hurricane name lists due to its significant impacts in the Caribbean and the United States, and it will never be used again for another Atlantic hurricane. It was replaced with Irma for the 2017 season.

Season effects

This is a table of all of the storms that formed in the 2011 Atlantic hurricane season. It includes their name, duration, peak classification and intensities, areas affected, damage, and death totals. Damage and deaths include totals while the storm was extratropical, a wave, or a low, and all of the damage figures are in 2011 USD.