2009 Atlantic hurricane season

On December 10, 2008, Klotzbach's team issued its first extended-range forecast for the 2009 season, predicting above-average activity (14 named storms, 7 hurricanes, 3 of Category 3 or higher and ACE Index of 125). On April 7, 2009, Klotzbach's team issued an updated forecast for the 2009 season, predicting near-average activity (12 named storms, 6 hurricanes, 2 of Category 3 or higher and ACE Index of 100), citing the possible cause as the high probability of a weak El Niño forming during the season.[11] On May 21, 2009, NOAA issued their forecast for the season, predicting near or slightly above average activity, (9 to 14 named storms, 4 to 7 hurricanes, and 1 to 3 of Category 3 or higher).[12]

On June 2, 2009, Klotzbach's team issued another updated forecast for the 2009 season, predicting slightly below average activity (11 named storms, 5 hurricanes, 2 of Category 3 or higher and ACE Index of 85). Also on June 2, 2009, the Florida State University Center for Ocean-Atmospheric Prediction Studies (FSU COAPS) issued its first ever Atlantic hurricane season forecast. The FSU COAPS forecast predicted 8 named storms, including 4 hurricanes, and an ACE Index of 65.[13] On June 18, 2009, the UK Met Office (UKMO) issued a forecast of 6 tropical storms in the July to November period with a 70% chance that the number would be in the range 3 to 9. They also predicted an ACE Index of 60 with a 70% chance that the index would be in the range 40 to 80.[14] On August 4, 2009, Klotzbach's team updated their forecast for the 2009 season, again predicting slightly below average activity (10 named storms, 4 hurricanes, and 2 major hurricanes). On August 6, 2009, the NOAA also updated their forecast for the 2009 season, predicting below average activity (7–11 named storms, 3–6 hurricanes, and 1–2 major hurricanes).[15]

Tropical depression (SSHWS)
Duration	May 28 – May 29
Peak intensity	35 mph (55 km/h) (1-min); 1006 mbar (hPa)

During late-May, a frontal boundary stalled near The Bahamas and slowly degenerated. On May 25, 2009, an area of low pressure developed along the tail-end of a decaying cold front near the northern Bahamas. Tracking northward, this low gradually developed as it moved within 85 mi (135 km) of North Carolina's Outer Banks. By May 28, deep convection developed across a small area over the low-pressure system, leading to the National Hurricane Center classifying the system as Tropical Depression One. It was the northernmost forming May tropical cyclone in Atlantic history, though subtropical cyclones formed equally far north in 1972 and 2007. It also marked the third consecutive year with pre-season tropical or subtropical cyclones in the basin. The depression moved over the warm waters of the Gulf Stream for the following 24 hours, allowing it to maintain its convection, before moving into a hostile environment characterized by strong wind shear and cooler waters. Late on May 29, the system degenerated into a remnant low. Several hours later, on May 30, about 345 mi (555 km) south-southeast of Halifax, Nova Scotia, Tropical Depression One was absorbed by a warm front.[4][22]

As a tropical cyclone, the depression had no impact on land. However, the precursor to the system brought scattered rainfall and increased winds to parts of the North Carolina coastline, but no damage.[4] Rainfall in Hatteras amounted to 0.1 in (2.5 mm) on May 27; sustained wind reached 15 mph (24 km/h) and gusts were measured up to 23 mph (37 km/h). The lowest sea level pressure recorded in relation to the system was 1009 mbar (hPa; 29.80 inHg).[23] Increased winds along coastal areas of the state was possible in relation to the outer edges of the depression.[24]

Tropical storm (SSHWS)
Duration	August 11 – August 16
Peak intensity	40 mph (65 km/h) (1-min); 1003 mbar (hPa)

Ana formed out of an area of low pressure associated with a tropical wave on August 11, Ana briefly attained tropical storm intensity on August 12 before weakening back to a depression. The following day, the system degenerated into a non-convective remnant low as it tracked westward. On August 14, the depression regenerated roughly 1,075 mi (1,735 km) east of the Leeward Islands. Around 06:00UTC on August 15, the storm re-attained tropical storm status, at which time it was named Ana. After reaching a peak intensity with winds of 40 mph (65 km/h) and a barometric pressure of 1003 mbar (hPa; 29.62 inHg), the storm began to weaken again due to increasing wind shear and the unusually fast movement of Ana. In post-storm analysis, it was discovered that Ana had degenerated into a tropical wave once more on August 16, before reaching any landmasses.[25]

Numerous tropical storm watches were issued for the Lesser Antilles, Puerto Rico and the Dominican Republic between August 15 and 17.[25] Several islands took minor precautions for the storm, including St. Croix which evacuated 40 residents from flood-prone areas ahead of the storm.[26] In the Dominican Republic, officials took preparations by setting up relief agencies and setting up shelters.[27] Impact from Ana was minimal, mainly consisting of light to moderate rainfall.[25] In Puerto Rico, up to 2.76 in (70 mm),[28] causing street flooding and forcing the evacuation of three schools. High winds associated with the storm also downed trees and power lines, leaving roughly 6,000 residents without power.[29]

Category 4 hurricane (SSHWS)
Duration	August 15 – August 24
Peak intensity	130 mph (215 km/h) (1-min); 943 mbar (hPa)

As Ana regenerated into a tropical depression,[25] a new tropical depression developed early on August 15 southwest of the Cape Verde Islands. Light wind shear and warm waters allowed the depression to steadily intensify, becoming Tropical Storm Bill later that day. By August 17, Bill attained hurricane-status about midway between the Cape Verde Islands and the Lesser Antilles. Eventually the hurricane attained its peak intensity as a Category 4 storm roughly 345 mi (555 km) east-northeast of the Leeward Islands. The storm attained maximum winds of 130 mph (210 km/h), the highest of any storm during the season, before weakening slightly as it turned north. The large storm passed roughly 175 mi (280 km) west of Bermuda as a Category 2 hurricane. Further weakening took place as Bill brushed the southern coast of Nova Scotia the following day. Shortly before making landfall in Newfoundland, Bill weakened to a tropical storm and accelerated. The storm eventually transitioned into an extratropical cyclone after moving over the north Atlantic before being absorbed by a larger non-tropical low on August 24.[6]

Two people were killed by the storm's large swells—one in Maine and another in Florida. The hurricane came close enough to warrant tropical cyclone watches and warnings in both the US and Canada. Bill was one of three tropical storms active on August 16.[6] Large, life-threatening swells produced by the storm impacted north-facing coastlines of Puerto Rico and Hispaniola as Hurricane Bill approached Bermuda.[30] Along the coasts of North Carolina, waves averaging 10 ft (3.0 m) in height impacted beaches. On Long Island, beach damage was severe; in some areas the damage was worse than Hurricane Gloria in 1985.[31] In New York, severe beach erosion caused by the storm resulted in over $35.5 million in losses.[32]

Tropical storm (SSHWS)
Duration	August 16 – August 18
Peak intensity	60 mph (95 km/h) (1-min); 1005 mbar (hPa)

Just one day after the formation of Hurricane Bill, the season's third named storm developed on August 16. Forming out of a tropical wave and an upper-level low-pressure system, Claudette quickly intensified into a tropical storm offshore south of Tallahassee, Florida. By the afternoon, the storm had attained winds of 60 mph (95 km/h) and steadily tracked towards the Florida Panhandle. Early on August 17, the center of Claudette made landfall on Santa Rosa Island. Several hours after landfall, the storm weakened to a tropical depression and the Hydrometeorological Prediction Center took over primary responsibility of the storm. The system quickly dissipated and was last noted over Alabama on August 18.[33]

The National Hurricane Center issued tropical storm warnings for the Florida coastline and residents in some counties were advised to evacuate storm-surge-prone areas.[33][34] Tropical Storm Claudette, produced moderate rainfall across portions of Florida, Georgia, and Alabama between August 16 and 18. Two people were killed offshore amidst rough seas from the storm.[35] An EF-0 tornado spawned by the storm in Cape Coral damaged 11 homes, leaving $103,000 in damages. Additional damages to coastal property and beaches amounted to $125,000 as a result of Claudette.[36]

Tropical storm (SSHWS)
Duration	August 26 – August 29
Peak intensity	60 mph (95 km/h) (1-min); 1006 mbar (hPa)

Around the same time the remnants of Hurricane Bill dissipated over the northern Atlantic,[6] a new tropical storm developed near the Bahamas on August 26. The system, immediately declared Tropical Storm Danny on its first advisory, erratically moved in a general northwestward direction. Danny attained peak winds of 60 mph (95 km/h) before succumbing to high wind shear. After turning northward, the storm weakened and was eventually absorbed by another low-pressure system off the east coast of the United States early on August 29.[37] High waves from Danny killed a boy in the Outer Banks.[38]

Tropical storm (SSHWS)
Duration	September 1 – September 3
Peak intensity	50 mph (85 km/h) (1-min); 1004 mbar (hPa)

On September 1, the season's fifth named storm, Tropical Storm Erika, formed east of the Lesser Antilles. Upon forming, the storm had attained its peak intensity with winds of 50 mph (80 km/h). Persistent wind shear prevented the system from intensifying and resulted in the storm's convection being completely displaced from the center of circulation by the time it passed over Guadeloupe on September 2. After entering the Caribbean Sea, Erika briefly regained strength before fully succumbing to strong shear. The system eventually dissipated on September 4, to the south of Puerto Rico.[39] Damages were minor, though one island received several inches of rain.

Category 3 hurricane (SSHWS)
Duration	September 7 – September 12
Peak intensity	120 mph (195 km/h) (1-min); 958 mbar (hPa)

Several days after Erika dissipated,[39] a new tropical depression formed southeast of the Cape Verde Islands on September 7. This depression rapidly intensified within an environment of low wind shear and high sea surface temperatures. Receiving the name Fred on September 8, the storm quickly developed an eye feature and was upgraded to a hurricane roughly 24 hours after being named. Within a 12‑hour span, the storm's winds increased by 40 mph (65 km/h) to its peak of 120 mph (195 km/h). Upon reaching this intensity, Fred became the strongest storm on record south of 30°N and east of 35°W in the Atlantic basin. Not long after the intensification ceased, it began to weaken as dry air became entrained within the system. By September 11, the storm nearly stalled northwest of the Cape Verde Islands and weakened to a tropical storm. The following day, Fred degenerated into a remnant low before taking a westward track across the Atlantic. The remnants of Fred persisted for nearly a week, nearly regenerating into a tropical depression several times. The low eventually dissipated on September 19, to the south of Bermuda.[17]

Tropical depression (SSHWS)
Duration	September 25 – September 26
Peak intensity	35 mph (55 km/h) (1-min); 1008 mbar (hPa)

In late September, a new, well-defined tropical wave moved off the west coast of Africa into the Atlantic Ocean. By September 25, the system had developed sufficient deep convection for the NHC to classify it as Tropical Depression Eight. At this time, the depression attained its peak intensity with winds of 35 mph (55 km/h) and a minimum pressure of 1008 mbar (hPa). Shortly thereafter, wind shear and decreasing sea surface temperatures caused the depression to weaken. The system degenerated into a remnant low on September 26 before degenerating into a trough of low pressure.[40]

Tropical storm (SSHWS)
Duration	October 4 – October 6
Peak intensity	65 mph (100 km/h) (1-min); 986 mbar (hPa)

Originating from an extratropical cyclone east of Newfoundland on September 27, the precursor to Tropical Storm Grace tracked southeastward towards the Azores, gaining subtropical characteristics. After executing a counterclockwise loop between October 1 and 3, deep convection wrapped around a small circulation center that had developed within the larger cyclone. On October 4, this smaller low developed into a tropical storm while situated near the Azores Islands, becoming the northeasternmost forming Atlantic tropical cyclone on record. The storm quickly turned northeastward and intensified, developing an eye-like feature as it attained peak winds of 65 mph (105 km/h) and a minimum pressure of 986 mbar (hPa; 29.12 inHg). It weakened over increasingly colder waters and began merging with an approaching frontal boundary. Early on October 6, Grace transitioned into an extratropical cyclone before dissipating later that day near Wales.[18]

Although Grace passed through the Azores Islands, the storm had little known effects there.[18] In Europe, the system and its remnants brought rain to several countries, including Portugal,[41] the United Kingdom[42] and Belgium.[43] No fatalities were linked to Grace and overall damage was minimal.[18]

Tropical storm (SSHWS)
Duration	October 6 – October 8
Peak intensity	50 mph (85 km/h) (1-min); 1005 mbar (hPa)

A tropical wave left the coast of Africa on October 1, moving westward with intermittent showers and thunderstorms.[44] On October 5, the system became better organized,[45] and a low-pressure area formed.[46] Although the thunderstorms were displaced east of the center of circulation and the probability for development was never high, the disturbance became a tropical depression around 0000 UTC on October 6 about 775 mi (1,245 km) east of the Lesser Antilles.[44] Operationally, the storm was not designated a tropical cyclone until later on October 6, when it was immediately declared a tropical storm.[47]

Affected by strong wind shear, Henri remained disorganized with its center located on the western edge of the convection. Moving northwestward, Henri intensified slightly to peak winds of 50 mph (80 km/h) on October 7 after the convection increased. Shortly thereafter, the wind shear grew stronger, and on October 8 the storm weakened to a tropical depression.[44] The structure became further disorganized with several low-level vortices.[48] Just twelve hours after weakening into a depression, Henri degenerated into a remnant area of low pressure. The remnants continued northwestward before turning to the west-southwest due to a ridge. On October 11, the storm's circulation dissipated near Hispaniola, having never impacted land.[44]

Category 2 hurricane (SSHWS)
Duration	November 4 – November 10
Peak intensity	105 mph (165 km/h) (1-min); 975 mbar (hPa)

The final storm of the 2009 season formed over the southern Caribbean Sea on November 4. The slow moving system quickly developed into Tropical Storm Ida within a favorable environment as it neared the coastline of Nicaragua. Several hours before moving over land, Ida attained hurricane-status, with winds reaching 80 mph (130 km/h). Hours after moving inland, Ida weakened to a tropical storm and further to a tropical depression as it turned northward. On November 7, the depression re-entered the Caribbean Sea and quickly intensified. Early on November 8, the system re-attained hurricane intensity as it rapidly intensified over warm waters. Ida attained its peak intensity as a Category 2 hurricane early the next day with winds of 105 mph (170 km/h) as it moved over the Yucatán Channel. Not long after reaching this intensity, Ida quickly weakened to a tropical storm as it entered the Gulf of Mexico. Despite strong wind shear, the storm briefly re-attained hurricane status for a third time near the southeastern Louisiana coastline before quickly weakening to a tropical storm. Shortly before moving inland over the southern United States, Ida transitioned into an extratropical cyclone. The remnants of Ida persisted until November 11, at which time the low dissipated. Remnant energy from Ida provided energy for another system which became a powerful nor'easter, causing significant damage in the Mid-Atlantic States. The resulting storm came to be known as Nor'Ida.[5]

In the southern Caribbean, Hurricane Ida caused roughly $2.1 million in damage in Nicaragua after destroying numerous homes and leaving an estimated 40,000 people homeless.[49][50] Ida also produced significant rainfall across portions of western Cuba, with some areas recording up to 12.5 in (320 mm) of rain during the storm's passage.[5] In the United States, the hurricane and the subsequent nor'easter caused substantial damage, mainly in the Mid-Atlantic States.[5] One person was killed by Ida after drowning in rough seas while six others were killed in various incidents related to the nor'easter. Overall, the two systems caused nearly $300 million in damage throughout the country.[36]