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Pdf expert 50 free.2005 Atlantic hurricane season

 

Some weather models predicted relaxing shear and intensification of the system; [94] however, the hostile conditions ripped the system apart, causing the depression to degenerate into a remnant low, and the NHC discontinued advisories on August 14, when no organized deep convection remained.

The remnants of Tropical Depression Ten continued drifting northwestward, before degenerating further into a tropical wave north of the Leeward Islands , on August Soon afterward, the low-level and mid-level circulations split, with the mid-level circulation lagging behind to the east.

The remnant low-level circulation continued westward, before dissipating near Cuba on August Producing occasional bursts of convection, the mid-level remnant circulation eventually merged with another tropical wave approaching from the east, on August A tropical wave, plausibly the same that spawned Tropical Depression Ten nine days earlier, led to the formation of Tropical Depression Eleven over the Bay of Campeche on August The cyclone became more organized two hours before making landfall and was forming an eye, but its winds remained under hurricane strength.

Jose rapidly weakened and soon dissipated as it moved inland over Mexico. Jose was the earliest 10th named storm until surpassed by Tropical Storm Josephine in While drenching Mexico's Gulf coast, Jose forced some 25, residents from their homes in Veracruz state and damaged at least 16, homes in the state. A tropical depression developed on August 23 from the complex interaction of a tropical wave, the mid-level remnants of Tropical Depression Ten, and a nearby upper-level trough.

The depression became a tropical storm on August 24 and a hurricane on August 25, making landfall as a Category 1 hurricane in southeastern Florida. Katrina rapidly intensified to Category 5 status early on August 28, becoming the seventh most intense Atlantic hurricane. Turning northward, the hurricane weakened as it approached the northern Gulf Coast.

The cyclone quickly weakened after moving inland and became extratropical over Kentucky on August On August 27, the New Orleans National Weather Service issued an urgent weather bulletin describing potentially catastrophic impacts, comparing Katrina to Hurricane Camille of A day later, New Orleans mayor Ray Nagin issued the city's first-ever mandatory evacuation.

Portions of the city remained underwater for 43 days. About 2. Throughout the United States, Katrina killed 1, people, making it one of the deadliest hurricanes in the United States , [] [] [34] and the deadliest American hurricane since Within a year of the storm, most of the levees were largely repaired. A tropical wave moved off the coast of Africa on August Strong wind shear prevented much organization, and the depression degenerated into a low pressure area late on August The remnants moved to the north and northeast, steered by a larger non-tropical system to the north.

The convection increased on August 31; that day the system regenerated into a tropical depression, which strengthened further into Tropical Storm Lee. After 12 hours as a tropical storm, Lee weakened back to a tropical depression as it turned to the northwest, steered by the larger non-tropical storm. On September 2, the depression degenerated into a remnant low, which was absorbed by a cold front two days later.

A strong tropical wave entered the eastern Atlantic on August The broad disturbance was initially hindered by strong wind shear but eventually organized into a tropical depression about halfway between the Leeward Islands and Cabo Verde early on September 1. The tropical cyclone moved northwest and steadily organized as upper-level winds became more conducive.

It strengthened into Tropical Storm Maria on September 2 and eventually became the sixth hurricane of the season early on September 4. Around the time of its peak, Maria turned to the north and northeast, moving around the subtropical ridge as it gradually weakened. Maria fell to tropical storm intensity on September 9 and became extratropical a day later between Newfoundland and the Azores.

The former hurricane re-intensified over the northern Atlantic Ocean, only to weaken before passing near southern Iceland.

On September 14, the extratropical storm that was once Maria merged with another extratropical storm while approaching Norway. The remnants of Maria brought resulted in heavy rainfall to Norway, triggering a landslide in Bergen that killed three people and injured seven others. A tropical wave left Africa on August 30 and moved into the southwestern Atlantic, where subsequent interaction with an upper-level low led to the genesis of a tropical depression south-southwest of Bermuda on September 5.

This depression quickly intensified into Tropical Storm Nate, which moved slowly northeastward. On September 7, Nate intensified into the seventh hurricane of the season.

The same trough created unfavorable conditions, causing Nate to weaken quickly back to tropical storm status. On September 10, Nate transitioned into an extratropical storm which was absorbed by a larger extratropical storm near the Azores on September Canadian Navy ships headed to the U. Gulf Coast to help in the aftermath of Hurricane Katrina were slowed down trying to avoid Nate and Ophelia.

The interplay of a cold front and a trough led to the development of Tropical Depression Sixteen over the northern Bahamas on September 6. The depression strengthened into Tropical Storm Ophelia on September 7 and briefly into a hurricane on September 9 while stalled off the east coast of Florida. Ophelia fluctuated between hurricane and tropical storm intensity for the next week as it meandered off the southeastern United States.

After moving away from the state, Ophelia weakened to tropical storm status for a fourth and final time due to stronger wind shear and dry air. The storm accelerated northeastward and passed southeast of Cape Cod. Ophelia transitioned into an extratropical storm on September 18 and subsequently crossed Nova Scotia and Newfoundland, eventually dissipating on September 23 north of the Scandinavian Peninsula.

Ophelia caused significant coastal erosion from the churning waves. The hurricane caused extensive damage in the Outer Banks and around Cape Fear. The storm's remnants produced strong winds and heavy rain over Atlantic Canada. Ophelia killed three people — a drowning in Florida from high surf, a traffic fatality in North Carolina, and a death from a fall in Nova Scotia.

On September 17, Tropical Depression Seventeen formed from a tropical wave about miles km east of Barbados. It quickly intensified into Tropical Storm Philippe while taking a track to the north-northwest. Wind shear from an upper-level low caused the hurricane to weaken back to a tropical storm, exposing the center from the convection. On September 21, Philippe accelerated to the north and began moving around the upper-level low, which had extended to the surface and developed into a non-tropical cyclone.

The storm briefly threatened Bermuda as it turned to the northwest and began a counterclockwise loop. On September 23, Philippe weakened to a tropical depression and later a remnant low; it was absorbed by the larger non-tropical cyclone a day later.

Philippe brought gusty winds and moisture to Bermuda, with 0. The circulation that absorbed Philippe dropped light rainfall on the island, and was responsible for the lowest barometric pressure during the month.

In mid-September, the southern extent of a stationary front devolved into a trough north of the Leeward Islands. A tropical wave interacted with this feature to form a tropical depression near the Turks and Caicos Islands on September It organized into Tropical Storm Rita later that day. Moving to the west-northwest, the storm's intensification attenuated over the Bahamas before resuming thereafter, becoming a hurricane on September 20 between Cuba and Florida.

Rapid intensification ensued as Rita moved into the Gulf of Mexico. It rapidly weakened over land as it turned to the north and northeast, and was later absorbed by an approaching cold front on September 26 over Illinois.

Gulf Coast prompted one of the largest mass evacuations in the country's history, with an estimated 3. Storm surge also damaged homes in adjoining Jefferson County in Texas. In New Orleans, Rita produced additional flooding and overtopped levees that had been repaired after Hurricane Katrina a month earlier.

Impacts from heavy rainfall, gusty winds, and tornadoes associated with Rita affected much of the lower Mississippi River Valley, and over a million electricity customers lost power. A third of Cameron Parish's population left the parish following the devastation wrought by Rita. The newly formed cyclone exhibited deep convection in the southern semicircle, [] but its cloud pattern quickly deteriorated under the influence of strong wind shear.

A tropical wave emerged from Africa on September 17 and moved across the central Atlantic, hampered by north-northeasterly wind shear. The disturbance eventually traveled into the western Caribbean Sea, where it organized into a tropical depression southeast of Cozumel around UTC on October 1.

High pressure directed the cyclone toward the west-northwest, and the depression intensified into Tropical Storm Stan shortly before making landfall along the eastern coast of the Yucatan Peninsula.

Stan briefly weakened to a tropical depression as it crossed over land, but it regained tropical storm strength over the Bay of Campeche on October 3, when ridging further intensified and forced the storm west-southwest.

Rapid intensification ensued, allowing Stan to become a Category 1 hurricane before its second landfall east-southeast of Veracruz early on October 4. Once inland, the system rapidly unraveled over the mountainous terrain of Mexico, dissipating in the state of Oaxaca just after UTC on October 5. In the post-season analysis, the National Hurricane Center identified an additional subtropical storm that had gone unclassified during the course of the season.

In late September, an upper-level low formed west of the Canary Islands and moved westward, organizing into a subtropical depression early on October 4. It quickly intensified into a subtropical storm while curving northeast ahead of an approaching cold front.

Early on October 5, the storm merged with the cold front; later that day, its remains were absorbed by a non-tropical low. The low that absorbed the storm would eventually become Hurricane Vince. On October 5, Tropical Storm Tammy developed east of Florida following the interaction of a tropical wave and an upper-level trough.

Tammy weakened as it moved inland, crossing southern Georgia and Alabama. It was absorbed by a larger extratropical storm on October 6. Tammy dropped locally heavy rainfall along its path, causing minor damage. Subtropical Depression Twenty-Two formed from a non-tropical low miles km southeast of Bermuda on October 8. The system encountered unfavorable conditions as it turned westward and degenerated into a remnant low on October 10, before becoming extratropical on the following day.

The extratropical system transported tropical moisture northward, [] and was, along with Tropical Storm Tammy, a partial cause of severe flooding in New York, New Jersey and New England during early-to-mid-October. Subtropical Storm Vince formed in the eastern Atlantic near Madeira on October 8 from the same non-tropical low that absorbed the unnamed subtropical storm. Although Vince was a very small and short-lived storm that only briefly reached hurricane strength, it was notable for developing in the northeastern Atlantic, well away from where hurricanes usually form.

Vince made landfall on the Iberian Peninsula near Huelva , Spain, on October 11 just after weakening to a tropical depression. Vince was the first tropical cyclone on record to make landfall in Spain. An upper-level low over the southwestern Atlantic helped facilitate the formation of a large, monsoon -like gyre over the Caribbean Sea in middle October. A series of tropical waves moved into this area of disturbed weather and helped form a low-pressure system that developed into Tropical Depression Twenty-Four southwest of Jamaica on October It intensified into Tropical Storm Wilma two days later.

Wilma moved slowly through the warm waters of the western Caribbean Sea and began a period of rapid deepening on October 18 that lasted into the following day.

Wilma weakened to Category 4 intensity by the time it made landfall on Cozumel on October The hurricane quickly crossed the state and continued across the western Atlantic Ocean. Wilma transitioned into an extratropical cyclone on October 26, which was absorbed by a larger extratropical storm a day later over Atlantic Canada. In its formative stages, Wilma's large circulation spread across much of the western Caribbean Sea, killing 12 people in Haiti and one in Jamaica. Bush approved a disaster declaration for 13 Florida counties.

Later that day, the depression strengthened into Tropical Storm Alpha as it moved west-northwestward. Alpha weakened to a tropical depression over Hispaniola's steep mountains. Alpha was the 22nd named system in the Atlantic hurricane season, breaking the season's record, and became the first tropical storm to be named using the Greek Alphabet.

The storm claimed 26 lives, with more than half of them in Haiti. Early the next day, it was upgraded to Tropical Storm Beta. That brought the total number of major hurricanes in the season to seven, a record breaking achievement. However, Beta weakened to a Category 2 prior to landfall in Nicaragua.

The storm rapidly weakened inland and dissipated on October The Colombian island of Providencia was subjected to hurricane-force winds for several hours as the center of the storm moved very slowly by the island. Reports indicate extensive damage to homes and a loss of communications with the islanders. Late on November 13, Tropical Depression Twenty-Seven formed from a tropical wave about mi km west-southwest of St.

The remnants of the depression continued westward and moved along the northern shore of Honduras, merging with parts of a larger low pressure system.

It is uncertain whether the remnants of Gamma absorbed the low pressure system or vice versa. The storm strengthened and a closed circulation formed on November 18, making Gamma a tropical storm for the second time. After regeneration, and after making landfall over northern Honduras, floods from Gamma killed 34 people in Honduras. Three people died in Belize related to the storm. Gamma meandered in the Caribbean Sea for a short time, until slowly weakening and eventually disintegrating into a remnant low late on November Delta originated from a broad and non-tropical low-pressure area that arose 1, miles 2, km southwest of the Azores on November 19, initially moving northeast along the trailing fringes of a passing cold front.

Convection developed atop the center of the nascent disturbance two days later, and satellite data suggested that it was acquiring thermodynamic characteristics exhibited by tropical cyclones. On November 22, the NHC classified the low-pressure system as a subtropical storm with the name Delta.

Delta took a south-southwestward course and further coalesced its associated showers, leading to its re-designation as a tropical storm on November Delta moved erratically over the next two days and weakened to a low-end tropical storm in response to increasing wind shear.

A strengthening trough over western Europe accelerated Delta towards the east-northeast on November 27, concurrent with the brief emergence of an eye and a period of intensification. Delta's tropical characteristics later succumbed to wind shear and cold air, resulting in its extratropical transition on November 28 while miles mi west-northwest of the western Canary Islands; as an extratropical system, Delta tracked east, passing north of the Canary Islands before moving into Morocco and Algeria on November 29, where it dissipated.

Delta caused severe damage in the Canary Islands and claimed at least seven lives, including six who drowned after boats overturned; there were 12 people missing from the overturned boat. A surface low attached to a stationary front formed underneath an upper-level low east of Bermuda on November The surface low detached from the frontal zone and acquired tropical characteristics as deep convection wrapped around its center, leading to the development of Tropical Storm Epsilon early on November The NHC consistently forecast that the storm would weaken; however, Epsilon gradually intensified as it moved westward and later looped to the northeast.

The storm attained hurricane status on December 2 as the track shifted to the east. A ridge turned Epsilon to the southwest on December 6. Epsilon lasted as a hurricane until December 7, the most for any Atlantic tropical cyclone in December.

Epsilon degenerated into a remnant low on December 8; the circulation dissipated two days later. Towards the end of December, an upper-level low interacted with a cold front, which produced an area of low-pressure by December 28, about mi 1, km to the west-northwest of Cabo Verde.

Zeta weakened again as it turned westward, degenerating into a remnant low on January 6; the circulation dissipated on the next day to the southeast of Bermuda. The list below highlights the names used in the Atlantic hurricane season. This was the same list used for the season , with the exceptions of Franklin and Lee , which replaced Floyd and Lenny.

The season was the first Atlantic hurricane season to have storm names beginning with 'V' and 'W'. Also, when the list of 21 storm names pre-approved for the season by the World Meteorological Organization WMO was exhausted, became the first to move into the auxiliary list of names. There was considerable discussion on the usage of the Greek alphabet.

The committee agreed that the usage of the Greek alphabet had a "major important political, economic and social impact globally, which might not have happened if a secondary or circular list of names had been used", [46] and that the Greek alphabet would be used again if the traditional naming list was exhausted.

It was also decided that it was not practical to retire a Greek letter. Storms named with Greek letters that would otherwise be eligible for retirement would appear in the retired name list, but have a notation affixed with the circumstances.

A table of the storms that formed during the Atlantic hurricane season is given below: it includes storm name, duration, peak strength, areas affected, damage, and death total. Damage and deaths include amounts while the storm was extratropical, a wave, or a low. The death toll includes all indirect deaths, such as traffic accidents or electrocutions. Damage figures are in USD. From Wikipedia, the free encyclopedia. Hurricane season in the Atlantic Ocean. Timeline of the Atlantic hurricane season Pacific hurricane season Pacific typhoon season North Indian Ocean cyclone season.

For a chronological guide, see Timeline of the Atlantic hurricane season. Main article: Tropical Storm Arlene Main article: Tropical Storm Bret Main article: Hurricane Cindy Main article: Hurricane Dennis. Main article: Hurricane Emily Main article: Tropical Storm Gert Main article: Hurricane Irene Main article: Tropical Storm Jose Main article: Hurricane Katrina.

Main article: Hurricane Maria Main article: Hurricane Nate Main article: Hurricane Ophelia Main article: Hurricane Rita. Main article: Hurricane Stan. Main article: Azores subtropical storm. Main article: Tropical Storm Tammy. Main article: Hurricane Vince. Main article: Hurricane Wilma. Main article: Tropical Storm Alpha Main article: Hurricane Beta. Main article: Tropical Storm Gamma Main article: Tropical Storm Delta Main article: Hurricane Epsilon Main article: Tropical Storm Zeta See also: Tropical cyclone naming , History of tropical cyclone naming , List of historical tropical cyclone names , and List of retired Atlantic hurricane names.

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Brown March 10, August Archived PDF from the original on February 14, Retrieved February 10, October 10, Archived from the original on February 22, Retrieved February 21, Pasch; David P. Roberts February 14, Global Facility for Disaster Reduction and Recovery. Archived PDF from the original on February 22, Retrieved March 3, Archived PDF from the original on March 3, Retrieved February 6, Pasch; Eric S. Blake; Hugh D. Roberts September 9, United Nations Publications.

ISBN August 9, Archived PDF from the original on March 4, Retrieved November 21, World Food Programme Emergency Report United Nations World Food Programme. July 22, Archived PDF from the original on February 6, Pan American Health Organization. November Avila January 4, Nicaragua News Service. Archived from the original on September 21, Retrieved December 28, El Nuevo Diario in Spanish.

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Archived from the original on July 11, Retrieved March 5, El Siglo De Durango in Spanish. October 29, Archived from the original on July 22, Retrieved July 15, Government of Colombia Report in Spanish.

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November 14, Archived from the original on November 26, Stewart November 24, Blake February 8, European Observation Network. Archived from the original PDF on March 7, Beven; Eric S. Blake April 10, Franklin February 22, Beven February 14, Avila; Daniel P. Brown July 20, October 18, Tropical Cyclone Rainfall Data.

United States Weather Prediction Center. Retrieved November 26, Storm Data. ISSN Pasch January 23, Retrieved February 3, Archived from the original PDF on June 25, El Universal in Spanish.

Stewart February 14, Retrieved July 29, National Climatic Data Center. Retrieved May 12, Architect for simplicity Build a converged, automated and scalable network to future-proof your infrastructure. Build with trust Accelerate your digital journey with a partner dedicated to trust and security. Explore products and solutions.

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