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    2006 Pacific hurricane seasonFrom Wikipedia, the free encyclopedia

    The 2006 Pacific hurricane season was the most activesince 2000, which also produced 19tropical storms or

    hurricanes. [1] Eighteen developed within the National

    Hurricane Center (NHC) area of warning responsibility,which is east of 140W, and one storm formed between 140W and the International Date Line , which is under theurisdiction of the Central Pacific Hurricane Center (CPHC).

    Of the 19 total storms, eleven became hurricanes, of whichsix attained major hurricane status. Within the NHC portionof the basin, the season officially began on May 15, and inthe CPHC portion, it started on June 1; the season officiallyended on November 30. These dates conventionally delimitthe period of each year when most tropical cyclones form inthe eastern Pacific basin.

    The strongest storm of the season was Hurricane Ioke, which

    reached Category 5 status on the Saffir-Simpson scale in thecentral Pacific Ocean; Ioke passed near Johnston Atoll andlater Wake Island, where it caused heavy damage but nodeaths. The deadliest storm of the season was HurricaneJohn, which killed six people after striking the BajaCalifornia Peninsula, and the costliest storm was HurricaneLane, which caused $203 million in damage in southwesternMexico (2003USD, $221 million 2011 USD).

    Seasonal activity began on May 27 whenTropical StormAletta formed off the southwest coast of Mexico. No stormsformed in June, though the season became active in July

    when five named storms developed, including HurricaneDaniel which was the second strongest storm of the season.During August, Hurricanes Ioke and John formed, as well asfour other storms. September was a relatively quiet monthwith two storms, of which one was Hurricane Lane. Threestorms developed in October and two formed in November;this marked the first time on record when more than onetropical storm developed in the basin during the month ofNovember.

    2006 Pacific hurricane season

    Season summary map

    First storm formed: May 27, 2006

    Last storm

    dissipated:

    November 20, 2006

    Strongest storm: Ioke 915mbar (hPa)

    (27.03inHg), 160 mph (260

    km/h) (1-minute sustained)

    Total depressions: 25Total storms: 18 East

    1 Central

    Hurricanes: 10 East

    1 Central

    Major hurricanes

    (Cat. 3+):

    5 East

    1 Central

    Total fatalities: 14

    Total damage: $355 million (2006USD)

    $390 million (2011 USD)

    Pacific hurricane seasons

    2004, 2005, 2006, 2007, 2008

    Related articles:

    List of storms in the 2006 Pacific hurricane season

    Timeline of the 2006 Pacific hurricane season

    Contents

    1 Seasonal forecasts 2 Storms

    2.1 May and June 2.2 July 2.3 August 2.4 September 2.5 October

    2.5.1 Unclassified storm

    2.6 November

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    Seasonal forecasts

    On May 22, 2006, theNational Oceanic and AtmosphericAdministration (NOAA) released their forecasts for the2006 Atlantic, East Pacific, and Central Pacific hurricaneseasons. The Pacific season was expected to be hinderedby the decades-long cycle that began in 1995, whichgenerally increased wind shear across the basin. NOAApredicted a below-normal level of activity in the EasternPacific, with 1216 namedstorms, of which 68 wereexpected to become hurricanes, and 1 3 expected to

    become major hurricanes. [3] The Central Pacific basinwas also expected to be below average, with only two to three tropical cyclones expected to form or cross into the

    area.[4] They expected that neither El Nio nor La Nia would affect conditions significantly. [3]

    Storms

    Main article: Timeline of the 2006 Pacific hurricane season

    Main article: List of storms in the 2006 Pacific hurricane season

    May and June

    On May 15, the hurricane season began in the Eastern Pacific basin,

    which is the area of the northern Pacific Ocean east of 140W.[5]Twelvedays later, an area of disturbed weather developed into the first tropicaldepression of the season, about 190 mi (310 km) south ofAcapulco,Mexico. It quickly intensified into a tropical storm, and upon doing sowas named Aletta. The storm drifted northeastward toward the coast,bringing light rainfall before turning southward. Wind shear weakened thestorm, and on May 31 Aletta dissipated about 200 mi (320 km) west-

    northwest of where it formed.[6]

    On June 1, the season began in the Central Pacific basin, which is theregion between 140W and the International Dateline; however, no storms

    occurred in the basin until July. [7] In the Eastern Pacific, TropicalDepression Two-E formed on June 3 about 145 mi (245 km) southwest ofZihuatanejo, Mexico. It tracked eastward and brought heavy rainfall to thecoastline, with a report of about 11 inches (280 mm) in Acapulco. Land

    interaction weakened the depression, and it dissipated on June 5.[8] Notropical storms developed in June in the basin, which was unusual compared to the average of two stormsforming during the month. Since 1966, there have been only three other seasons in which a tropical storm did not

    form in June, these being 1969, 2004, and 2007.[9]

    3 Impact 4 Season effects 5 Storm names

    5.1 Retirement

    6 See also 7 Notes 8 References 9 External links

    Predictions of tropical activity in the 2006season

    for the Eastern North Pacific

    Source DateNamedstorms

    HurricanesMajor

    hurricanes

    NOAA Average[2] 15.3 8.8 4.2

    NOAA May 22, 2006 1216 68 13

    Actual activity 18 10 5

    Satellite image of Tropical Storm

    Aletta, the first storm of the season

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    July

    After about a month of no storms, the basin became active in July. The first storm of the month was HurricaneBud, which developed early on July 11 about 805 mi (1300 km) south ofCabo San Lucas. Moving west-northwestward, it encountered conditions for quick strengthening, and within 24 hours of forming it attainedhurricane status. Bud continued strengthening, reaching major hurricane status, or Category 3 status on theSaffir-Simpson scale, and peak winds of 125 mph (205 km/h) on July 13. Thereafter, cooler watersand stable air caused

    the hurricane to quickly weaken. On July 14, Bud weakened to tropical storm status, and two days later itdegenerated into a remnant low pressure area. The remnants of Bud dissipated on July 17 about 750 mi

    (1210 km) east-southeast of Hawaii.[10]

    One day after Bud formed, a tropical disturbance organized into a tropical depression about 290 mi (465 km) offthe coast of Mexico, which would later become Hurricane Carlotta. A large cyclone, its outer rainbands brushedthe coastline of Mexico, as it steadily intensified to reach tropical storm and later hurricane status within 30 hoursof forming. Outflow from Hurricane Bud prevented Carlotta from strengthening much further, though for aperiod of about 60 hours it fluctuated between strong tropical storm status and minimal hurricane status. Coolerwaters weakened the storm, and on July 16 Carlotta degenerated into a remnant low. Its low -level circulation

    persisted for three days before dissipating.[11]

    As the previous two storms were dissipating, a new tropical depressionformed off the southwest coast of Mexico on July 16, which would laterbecome Hurricane Daniel. It moved westward, gradually intensifyingunder favorable conditions. On July 22, it attained peak winds of 150 mph(240 km/h), a Category 4 on theSaffir-Simpson scale and making Danielthe strongest hurricane during the season in the NHC area ofresponsibility. Maintaining Category 4 status for about three days, the

    hurricane subsequently weakened quickly due to cooler waters. [12] Danielwas briefly forecast to move through the Hawaiian Islands as a tropical

    storm;[13] however, the storm continued to weaken, degenerating into aremnant low on July 27 about 800 mi (1290 km) east-southeast of Hilo,Hawaii. Its remnants brought moderate rainfall to the region, though no

    damage or deaths were reported. [14]

    Another tropical depression formed off the coast of Mexico on July 21. Ittracked northward toward the coast, strengthening into Tropical Storm

    Emilia and attaining peak winds of 65 mph (105 km/h). It briefly developed aneye, though weakened due toincreased wind shear as it turned away from the coast. Emilia later turned to the north, restrengthening to its peakintensity before weakening and paralleling the coastline of the Baja California peninsula. After droppingmoderate rainfall along the peninsula, it weakened further as it turned out to sea, and on July 27 degenerated into

    a remnant low.[15]

    The final storm of the month formed on July 31 from a tropical wave, well to the southwest of Mexico. Itmaintained a steady westward track throughout its duration, and quickly intensified into Tropical Storm Fabio.On August 1 it attained peak winds of 50 mph (85 km/h), butsubsequently began gradually weakening due to

    wind shear. Fabio degenerated into a remnant low on August 4, and a few days later brought locally heavyrainfall to Hawaii.[16]

    August

    Within the basin, more tropical cyclones developed in August than in any

    other month.[1] The first storm of the month was Tropical Storm Gilma,which in terms of winds was tied with Rosa for the weakest named storm of the season. Gilma developed onAugust 1 off the southwest coast of Mexico, attaining peak winds of 40 mph (65 km/h). The storm wasdisorganized due to persistent wind shear, which prevented further strengthening. On August 5 the cyclone

    Hurricane Daniel near peak intensity

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    dissipated without ever having affected land.[17]

    After a period of inactivity lasting a week and a half, a tropical depressionformed southwest of Mexico on August 15. It tracked generally west-northwestward for its entire duration, eventually becoming HurricaneHector. On August 18, it attained peak winds of 110 mph (175 km/h),before gradually weakening due to cooler waters. Weakening to a tropical

    storm on August 20, it later turned sharply to the west, degenerating into aremnant low on August 23 and dissipating the next day without affecting

    land.[18]

    The strongest hurricane of the season was Hurricane Ioke,[1] which

    formed on August 20 far to the south of Hawaii.[14] It was the first central

    Pacific named storm since Hurricane Huko in 2002.[1] Encounteringwarm waters and little wind shear, and maintaining well -defined outflow,Ioke intensified from a tropical depression to Category 4 status on theSaffir-Simpson scale within 48 hours. Late on August 22 it rapidly weakened to Category 2status before crossingover Johnston Atoll, where 12 people rode out the storm in a hurricane-proof bunker. Two days later, favorableconditions again allowed for rapid strengthening, and Ioke attained Category 5 status on August 25 before

    crossing the International Date Line.[14] As it continued westward its intensity fluctuated, and on August 31 itpassed near Wake Island with winds of 155 mph (249 km/h). Ioke gradually weakened as it turned northwestwardand northward, and by September 6 transitioned into an extratropical cyclone. The remnants of Ioke accelerated

    northeastward and ultimately crossed into Alaska.[14]

    On August 21 shortly after the previous storm formed, Hurricane Ileana developed off the southwest coast ofMexico. It generally paralleled the coastline throughout its duration, ultimately reaching peak winds of 120 mph(195 km/h) before weakening. Around the time of peak intensity, the hurricane passed near Socorro Island, whereit produced hurricane-force wind gusts. On August 27, Ileana degenerated into a remnant low, and two days later

    dissipated well offshore. [19]

    The next tropical depression, which would eventually become Hurricane

    John, formed on August 28 about 250 mi (400 km) off the coast ofMexico.[20] With favorable environmental conditions, [21] the systemquickly organized, becoming a hurricane within 36 hours of forming.Hurricane John continued rapid intensification and reached peak winds of135 mph (215 km/h) on August 30 while just off the Mexican coast.Landinteraction weakened the hurricane, and still tracking northwestward itstruck the eastern portion of the Baja California peninsula on September 2as a Category 2 hurricane.John dissipated on September 4, though its

    remnants brought rainfall to the southwest United States.[20]

    The last storm to develop in August was Hurricane Kristy, which formedon August 30 about 935 mi (1505 km)west-northwest of Hurricane John.

    It initially tracked northwestward, reaching peak winds of 80 mph(130 km/h) within 36 hours of forming.Outflow from Hurricane Johncaused Kristy to weaken, and at the same time, the storm's motion became

    nearly stationary as steering currents collapsed. On September 2 it turned to a southeast drift, and degeneratedinto a tropical depression around the same time. Kristy later turned to the west, oscillating between tropical

    depression and tropical storm status until dissipating on September 9.[22]

    September

    Hurricane Lane developed from a tropical wave on September 13 to the

    Typhoon Ioke after brushing Wake

    Island

    Hurricane John on August 31

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    south of Mexico. It moved northwestward parallel to the coast of Mexico,and steadily intensified in a favorable environment. After turning to thenortheast Lane attained peak winds of 125 mph (205 km/h), and madelandfall in the Mexican state of Sinaloa at peak strength. It rapidlyweakened and dissipated on September 17, and later brought precipitation

    to southern Texas.[23]

    An area of disturbed weather associated with the IntertropicalConvergence Zone spawned a tropical depression on September 16 off thecoast of Mexico. Despite being disorganized, it quickly strengthened intoTropical Storm Miriam. The storm was sheared throughout its duration,and after encountering cooler waters Miriam dissipated on September 18

    near the Baja California peninsula.[24]

    On September 18, an area of disturbed weather in the central Pacificbecame sufficiently organized and was designated Tropical DepressionTwo-C. Vertical wind shear caused the depression to weaken into aremnant low on September 20, it never having attained tropical storm status. The depression was initially thought

    to be a regeneration of earlier Hurricane Kristy.[14]

    On September 26, another area of disturbed weather in the Central Pacific near the International Date Linebecame organized and was designated Tropical Depression Three -C. However, wind shear and the presence ofdry air to the west inhibited further development, and the system dissipated 12 hours later; at around the same

    time, the system crossed into the Western Pacific. [14]

    October

    The first cyclone to develop in the month of October was Tropical StormNorman, which formed well off the coast of Mexico on October 9. Itquickly reached peak winds of 50 mph (85 km/h), though almost asquickly the cyclone degenerated into a remnant low due to wind shear. Itsremnants turned to the east, and on October 15 regenerated into a tropical

    cyclone just off the coast of Mexico after merging with anotherdisturbance. Norman quickly dissipated as unfavorable conditions

    returned, although it brought heavy rainfall to the Mexican coastline. [25]

    Tropical Storm Olivia formed on October 9 about 700 mi (1120 km) westof Norman. Tracking northeastward and attaining tropical storm status, itfailed to strengthen significantly due to wind shear. Olivia weakened totropical depression status on October 11, and turning to the east-southeastdegenerated into a remnant low two days later. Its remnants were laterabsorbed by a larger disturbance that included the remnants of Norman.[26]

    The final cyclone to develop within the CPHC area of responsibility was Tropical Depression Four-C, whichformed on October 13 to the southwest of Hawaii. Within 24 hours of forming, it degenerated into a remnantdisturbance due to unfavorable wind shear. Moisture from the depression contributed to heavy rainfall in Hawaii.[14]

    The strongest hurricane during the month was Hurricane Paul. Forming on October 21, it did not strengthen muchinitially due to the presence of wind shear. However, a decrease in shear allowed Paul to strengthen rapidly, andin a 24-hour period it developed from a moderate tropical storm to a 105 mph (170 km/h) hurricane, its peakintensity. By that time, it had turned northeastward and entered an unfavorable environment, which caused Paulto steadily weaken to tropical storm status. After passing south ofthe Baja California peninsula it deteriorated to

    Tropical Storm Miriam, one of two

    storms to form in September

    TRMM satellite image of the rainfall

    from Hurricane Paul

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    tropical depression status and moved ashore in northwestern Sinaloa.[27]

    On October 26 shortly after Paul dissipated, another tropical depression formed off the southwest coast ofMexico. Moving southwestward, it encountered unfavorable wind shear, which prevented strengthening. On

    October 28 it degenerated into a remnant low, and the next day dissipated without affecting land. [26]

    Unclassified storm

    Main article: 2006 Central Pacific cyclone

    An extratropical storm persisted in the extreme northern central Pacific Ocean in late October. It drifted overunusually warm waters up to 3.6F (2C) above normal, and gradually developed convection near the center. ByNovember 2,QuikSCAT satellite suggested the system attained winds of up to 60 mph (95 km/h) about 900 mi(1450 km) west ofOregon. The system also developed an eye and an eyewall. The cyclone tracked northeastwardas it gradually weakened, and dissipated on November 4.NASA considered the cyclone to be a subtropical storm.However, as it formed outside of the territory of any monitoring organization, it was not named. Operationally,

    the United States Navy treated the system as a tropical disturbance, numbered 91C. [28]

    November

    Tropical activity within the basin in November 2006 was the most activeon record, based on the Accumulated Cyclone Energy (ACE) Index.Three tropical cyclones formed, of which two became tropical storms;only one other season on record, 1961, produced two tropical storms inthe month of November. The first storm of the month was Tropical StormRosa, which formed on November 8 as a tropical depression off thesouthwest coast of Mexico. Immediate development was hampered bywind shear, although an increase in thunderstorms on November 9brought the depression to tropical storm status. Continued shear prevented

    intensification, and Rosa dissipated on November 10.[26] Rosa was thefirst Eastern Pacific tropical storm in November since another storm

    named Rosa in the 2000 season.[1]

    On November 11, another tropical depression formed off the coast ofMexico, about 450 mi (720 km)west-southwest of where Rosa dissipated

    the previous day.[1][29] Similar to Rosa, it developed within anenvironment with unfavorable wind shear, but failed to intensify beyondtropical depression status. About 18 hours after it formed the depression

    degenerated into a trough. [29]

    The final storm of the season was Hurricane Sergio, which was both thestrongest and longest-lived November Pacific hurricane on record. It formed on November 13 about 460 mi(740 km) south ofManzanillo, Colima, and steadily intensified while tracking southeastward. It reached peakwinds of 110 mph (175 km/h) on November 15, and subsequentlybegan to weaken due to increased wind shearas it turned to the north. Sergio later turned to the west, remaining well off the coast of Mexico, and dissipated on

    November 20 about 320 mi (515 km) west-northwest of it originally formed.[30] The storm brought light rainfall

    to the Mexican coastline, though no major effects were reported.[31]

    Impact

    During the season, tropical cyclones collectively caused 14 fatalities and

    $355 million in damage (2006USD, $387 million 2011 USD).).[nb 1]

    QuikSCAT image of Sergio on

    November 16

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    With its long coastline, the country of Mexico was affected by ten of thecyclones during the season, including four that made landfall. Ofthe sixstorms that affected Mexico but did not strike the country, the first was

    Tropical Storm Aletta, the first storm of the season,[1] which brought light

    rainfall and caused minor damage. [32][33] The next tropical depression ofthe season produced heavy rainfall in the Acapulco area while remaining

    offshore; mudslides and flooding were reported, and 72 people wereforced to leave their homes. [34] In July, Hurricane Carlotta brushed the

    coastline with light rainfall. [11] When Tropical Storm Emilia passed justoff the coast of Baja California, it brought moderate precipitation which

    caused minor flooding and damage around Cabo San Lucas.[15] Heavy

    surf from Hurricane Ileana killed a man near Cabo San Lucas.[35] The laststorm of the season, Hurricane Sergio, produced light rainfall along the

    coast while remaining well offshore. [31]

    Mexico was struck by four tropical cyclones in 2006, none on the Atlantic coast and all along the Pacific coast.[36] The first was Hurricane John, which made landfall near the southern tip of the Baja California peninsula onSeptember 1. Earlier, it produced flooding and high surf near Acapulco while paralleling the coastline, and later

    the hurricane damaged or destroyed at least 450 homes in the Baja California peninsula.[20] Hurricane John was

    the wettest tropical cyclone of the year in Mexico, dropping 17.7 in (449 mm) of rainfall.[36] Five people were

    killed, and damage in Mexico amounted to $663 million (2006MXN, $60.8 million 2006 USD).[20][37]

    Hurricane Lane moved ashore in the state of Sinaloa as a Category 3 hurricane on the Saffir-Simpson scale,which was the strongest landfall during the season. Paralleling the coastline a short distance offshore, the

    hurricane dropped heavy rainfall, causing flooding and mudslides which resulted in four fatalities. [22] HurricaneLane affected 4,320 houses, and a total of 19,200 mi (30,000 km)of roads and highways were damaged to somedegree. Monetary damage amounted to about $2.2 billion (2006 MXN, $203 million 2006 USD) indamage in the

    country.[38] In early October, former Tropical Storm Norman passed near or over southwestern Mexico, [26]

    destroying 20 houses and leaving 20 villages without power.[39] Later, former Hurricane Paul caused four deaths,

    two of which from rough seas and two from drowning in a flooded river.[40][41] The storm damaged

    5,000 houses,[42] and monetary damage totaled more than $35 million (2006MXN, $3.2 million 2006USD).[43]

    Three of the cyclones that affected Mexico also impacted the southwestern United States. Moisture from Tropical

    Storm Emilia produced thunderstorms in Arizona which caused flooding,[44] and in southern California its

    rainfall assisted firefighters in combating a wildfire. [45] The remnants of Hurricane John produced moisture

    across much of the southwestern United States, causing mudslides in California, [46] light rainfall in Arizona, [47]

    flooded waterways in New Mexico,[48] and up to 8 in (200 mm) of rainfall in Texas.[49] In western Texas, the

    precipitation was beneficial in some areas [47] but damaging in others, [50] causing flooded roads and washouts. [49]

    The remnants of Hurricane Lane also produced rainfall in Texas. [51]

    Four tropical cyclones affected the U.S. state of Hawaii, all of which were

    the remnants of former tropical cyclones. Moisture from Hurricane Bud

    produced light rainfall in east -facing slopes of the island chain. [52] FormerHurricane Daniel produced up to 5 in (125 mm) of rainfall in the state,

    though no significant impact was reported. [14] The remnants of TropicalStorm Fabio contributed to heavy rainfall, peaking at 15.08 in (383 mm)

    on Mount Waialeale on the island of Kauai;[53] the rainfall caused river

    and roadway flooding, but little damage. [16] Moisture from TropicalDepression Four-C in October contributed to heavy rainfall on the island

    of Hawaii.[14]

    Satellite image of Hurricane Lane

    near landfall; Lane was the costliest

    hurricane of the season.

    Damage on Wake Island caused by

    Typhoon Ioke

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    The strongest hurricane of the season was Hurricane Ioke, which reached Category 5 status in the central PacificOcean. It first affected the uninhabited Johnston Atoll, although when Ioke struck there was a crew of 12 peopletaking shelter on the island. Hurricane force winds affected the landmass, powerful enough to knock down trees.[14] In the western Pacific Ocean after being re-classified as a typhoon, Ioke passed near Wake Island, forcing the

    first full-scale evacuation of the island since a typhoon in 1967. [54] The combination of strong winds and a

    powerful storm surge damaged 70% of the buildings on the island, many with moderate roof damage.[55]

    Destruction on the island was estimated at $88 million (2006 USD, $95.9 million2011 USD).).[56] Later, thestorm passed near the Japanese island of Minami Torishima, which was also fully evacuated;[57] facilities on the

    island were damaged, although it was repaired and fully operational within three weeks after the storm.[58] The

    remnants of Ioke later brought hurricane force wind gusts to southwestern Alaska. [59]

    Season effects

    This is a table of the storms in 2006 and their landfall(s), if any; the table does not include storms that did notmake landfall, which is defined as the center of the storm moving over a landmass. Deaths in parentheses areadditional and indirect (an example of an indirect death would be a traffic accident), but are still storm-related.Damage and deaths include totals while the storm was extratropical or a wave or low.

    SaffirSimpson Hurricane Scale

    TD SS TS C1 C2 C3 C4 C5

    2006 Pacific hurricane statistics

    StormName

    Dates active

    Stormcategory

    at peakintensity

    MaxWind

    (mph)

    Min.Press.(mbar)

    Landfall(s)Damage(millions

    USD)Deaths

    Where WhenWind

    (mph)

    AlettaMay 27May 30

    TropicalStorm

    45 1002 none Minimal 0

    Two-E June 3June 5

    TropicalDepression

    35 1005 none Unknown 0

    BudJuly 11July 16

    Category 3Hurricane

    125 953 none none 0

    CarlottaJuly 12July 16

    Category 1Hurricane

    85 981 none none 0

    DanielJuly 16July 26

    Category 4Hurricane

    150 933 none none 0

    EmiliaJuly 21July 28

    TropicalStorm

    65 990 none Unknown 0

    FabioJuly 31August 3

    TropicalStorm 50 1000 none none 0

    GilmaAugust 1August 3

    TropicalStorm

    40 1004 none none 0

    HectorAugust 15August 23

    Category 2Hurricane

    110 966 none none 0

    IokeAugust 20August 27

    Category 5Hurricane

    160 915WakeIsland(Direct hit,

    August 30 155 88 0

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    [nb 2] no landfall)[nb 3]

    IleanaAugust 21August 27

    Category 3Hurricane

    120 955 none Minimal 1

    John

    August 28

    September 4

    Category 4

    Hurricane 135 948

    Cabo del

    Este,Mexico September 1 110 60.9 5

    KristyAugust 30September 8

    Category 1Hurricane

    80 985 none none 0

    LaneSeptember 13

    September 17

    Category 3Hurricane

    125 952

    Islas Maras September 15 105

    203 4El Dorado,Mexico

    September 16 125

    MiriamSeptember 16

    September 18

    TropicalStorm

    45 999 none none 0

    Two-C

    September 18

    September 20

    TropicalDepression 35 1007 none none 0

    Three-CSeptember 26

    September 27

    TropicalDepression

    35 1007 none none 0

    NormanOctober 9October 15

    TropicalStorm

    50 1000

    Manzanillo,Mexico[nb 4]

    October 15 35 none 0

    OliviaOctober 9October 12

    TropicalStorm

    45 1000 none none 0

    Four-COctober 13October 14

    TropicalDepression 35 1007 none none 0

    PaulOctober 21October 26

    Category 2Hurricane

    105 970IslaAltamura,Mexico

    October 26 30 3.2 4

    Eighteen-E

    October 26October 27

    TropicalDepression

    35 1007 none none 0

    UnnamedOctober 30November 4

    SubtropicalStorm

    60 989 none none 0

    RosaNovember 8November 10

    TropicalStorm

    40 1002 none none 0

    Twenty-E

    November 11

    November 11

    TropicalDepression

    35 1007 none none 0

    SergioNovember 13

    November 20

    Category 2Hurricane

    110 965 none none 0

    Season Aggregates

    22cyclones

    May 27November 20

    160 915 5 landfalls 355 14

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    Storm names

    The following names were used for named storms that formed in the northeast Pacific in 2006.[60] This is thesame list that was used in the 2000 season. There were no names retired from the northeast Pacific list. Therefore,the same list will be reused in the 2012 season.

    Storms that formed in the central Pacific are given names from a sequential list; in 2006, the name Ioke was usedfrom this list, the first time a name from the Central Pacific list had been used since the 2002 season.

    Retirement

    The name Ioke was retired from the north-central Pacific list by the WMO in the spring of 2007 and replaced

    with Iopa.[61] During the 61st Interdepartmental Hurricane Conference, the Hawaii State Civil Defense requested

    the retirement of the name Daniel, citing that the storm had become memorable due to threat of damage. [62]

    However, the request was denied, as the name remains on the tropical cyclone naming list. [60]

    See also

    List of Pacific hurricanes List of Pacific hurricane seasons 2006 Atlantic hurricane season

    2006 Pacific typhoon season 2006 North Indian Ocean cyclone season South-West Indian Ocean cyclone seasons: 200506, 200607 Australian region cyclone seasons: 200506, 200607 South Pacific cyclone seasons: 200506, 200607

    Notes

    1. ^ The cumulative damage and fatality figures were obtained by summing the figures from the impact section.2. ^ Ioke did not dissipate on August 27, but crossed the Internationa l Date Line and became Typhoon Ioke.3. ^ Though Hurricane Ioke did not make landfall, its strike on Wake Island is included in the table, due to the severe

    damage on the island.

    4. ^ In its report on Tropical Storm Norman, the National Hurricane Center did not specify whether the storm movedashore or not. However, in its report to the World Meteorological Organization, officials from Mexico includedNorman in the storms that moved ashore along the country.

    References

    1. ^ a b c d e f g Hurricane Research Division (2008 -03-21). "Hurricane Data for Pacific Hurricanes 1949 -2007" (TXT).National Oceanic and Atmospheric Administration. Archived from the original on August 22, 2008.http://web.archive.org/web/20080822035410/http://www.nhc.noaa .gov/tracks1949to2007_epa.txt . Retrieved 2008-11-21.

    2. ^ Climate Prediction Center, NOAA (2006-05-22). "Background Information: East Pacific Hurricane Season" .

    Aletta Bud Carlotta Daniel Emilia Fabio Gilma Hector

    Ileana John Kristy Lane Miriam Norman Olivia Paul

    Rosa Sergio Tara(unused) Vicente(unused) Willa(unused) Xavier(unused) Yolanda(unused) Zeke(unused)

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    External links National Hurricane Center's Eastern Pacific Tropical Weather Outlook - updated four times daily National Hurricane Center National Hurricane Center's 2006 Advisory Archive Central Pacific Hurricane Center

    Retrieved from "http://en.wikipedia.org/wiki/2006_Pacific_hurricane_season "Categories: Pacific hurricane seasons | 2006 Pacific hurricane season

    This page was last modified on 9 March 2011 at 06:58. Text is available under the Creative Commons Attribution-ShareAlike License; additional terms may

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    Tropical cyclones of the 2006 Pacific hurricane season

    A 2E B C D E F G H I* I J K

    L M 2C* 3C* N O 4C* P 18E R 20E S * Central Pacific system

    SaffirSimpson Hurricane Scale

    TD SS TS C1 C2 C3 C4 C5

    Related articles

    Timeline

    List of storms

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