| Basin: | SPac |
| Year: | 2005 |
| Track: | 2004-2005 South Pacific cyclone season summary.png |
| First Storm Formed: | October 28, 2004 |
| Last Storm Dissipated: | May 1, 2005 |
| Strongest Storm Name: | Percy |
| Strongest Storm Pressure: | 900 |
| Strongest Storm Winds: | 125 |
| Average Wind Speed: | 10 |
| Total Disturbances: | 18 |
| Total Depressions: | 17 |
| Total Hurricanes: | 9 |
| Total Intense: | 5 |
| Fatalities: | None |
| Damages: | 55 |
| Five Seasons: | 2002–03, 2003–04, 2004–05, 2005–06, 2006–07 |
| South Indian Season: | 2004–05 South-West Indian Ocean cyclone season |
| South Pacific Season: | 2004–05 Australian region cyclone season |
The 2004–05 South Pacific cyclone season was an above-average season in which tropical cyclones formed within the South Pacific Ocean to the east of 160°E. The season officially ran from November 1, 2004 to April 30, 2005, however a tropical cyclone could form at any time between July 1, 2004 and June 30, 2005 and would count towards the season total. The season got off to an early start, when Tropical Depression 01F developed near the Solomon Islands on October 28, three days before the official start of the season. The final disturbance of the season dissipated as the season was drawing to a close on May 1. The season was above-average in terms of activity, with 9 tropical cyclones and 5 severe tropical cyclones forming during the season. The season featured Cyclone Percy, the most intense of the season in terms of pressure.
During the season, tropical cyclones are officially monitored by the Fiji Meteorological Service (FMS), Australian Bureau of Meteorology (BOM) and New Zealand's MetService. The United States Armed Forces through the Joint Typhoon Warning Center (JTWC) also monitors the basin and issue unofficial warnings for American interests. The FMS attaches a number and an F suffix to tropical disturbances that form in or move into the basin while the JTWC designates significant tropical cyclones with a number and a P suffix. The FMS, BoM and MetService all use the Australian Tropical Cyclone Intensity Scale and estimate wind speeds over a period of ten minutes, while the JTWC estimated sustained winds over a 1-minute period, which are subsequently compared to the Saffir–Simpson hurricane wind scale (SSHWS).
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PlotData= barset:Hurricane width:10 align:left fontsize:S shift:(4,-4) anchor:till from:28/10/2004 till:30/10/2004 color:TD text:"01F (TD)" from:03/12/2004 till:14/12/2004 color:TD text:"02F (TD)" from:05/12/2004 till:10/12/2004 color:TD text:"03F (TD)" from:21/12/2004 till:27/12/2004 color:C1 text:"Judy (C1)" from:05/01/2005 till:14/01/2005 color:C3 text:"Kerry (C3)" from:27/01/2005 till:02/02/2005 color:C1 text:"Lola (C1)" from:01/02/2005 till:08/02/2005 color:C5 text:"Meena (C5)" barset:break from:10/02/2005 till:20/02/2005 color:C5 text:"Olaf (C5)" from:10/02/2005 till:17/02/2005 color:C4 text:"Nancy (C4)" from:24/02/2005 till:05/03/2005 color:C5 text:"Percy (C5)" from:26/02/2005 till:02/03/2005 color:TD text:"11F (TD)" from:27/02/2005 till:08/03/2005 color:C1 text:"Rae (C1)" from:27/02/2005 till:04/03/2005 color:TD text:"13F (TD)" from:14/04/2005 till:02/05/2005 color:TD text:"14F (TD)" barset:break from:16/04/2005 till:23/04/2005 color:C1 text:"Sheila (C1)" from:20/04/2005 till:22/04/2005 color:TDi text:"16F (TDi)" from:26/04/2005 till:02/05/2005 color:TD text:"17F (TD)" from:29/04/2005 till:02/05/2005 color:TD text:"18F (TD)"
bar:Month width:5 align:center fontsize:S shift:(0,-20) anchor:middle color:canvas from:01/10/2004 till:01/11/2004 text:October from:01/11/2004 till:01/12/2004 text:November from:01/12/2004 till:01/01/2005 text:December from:01/01/2005 till:01/02/2005 text:January from:01/02/2005 till:28/02/2005 text:February from:01/03/2005 till:01/04/2005 text:March from:01/04/2005 till:01/05/2005 text:April from:01/05/2005 till:01/06/2005 text:MayTextData = pos:(569,23) text:"(For further details, please see" pos:(713,23) text:"scales)"
The first tropical depression of the season developed on October 28 to the northeast of Guadalcanal in the Solomon Islands. Over the next few days the system moved westwards and moved into the Australian region during October 30. There were no significant tropical disturbances observed during November, before Tropical Depression 02F developed to the north of Vanuatu during December 3. The system subsequently meandered over the ocean between Vanuatu and Fiji, before it was last noted to the southeast of Vanuatu during December 14. While Tropical Depression 02F was active, the third tropical depression of the season, developed to the south of Tuvalu on December 5. The system subsequently moved south-eastwards, before it was last noted during December 10 to the east of Nuku'alofa, Tonga. The fourth tropical disturbance of the season developed during December 21 and subsequently moved south-westwards, before it was named Judy during December 24, as it developed into the first tropical cyclone of the season.
| Basin: | SPac |
| Track: | Judy 2004 track.png |
| Formed: | December 21 |
| Dissipated: | December 27 |
| 10-Min Winds: | 45 |
| Pressure: | 989 |
On December 21, RSMC Nadi reported that Tropical Disturbance 04F had developed, along an active and slow-moving monsoon trough near French Polynesia.[1] The depression was in an area of high shear, with the deep convection located to the northeast of the center. The low level circulation center at this time was exposed but was developing despite the high shear associated with the system. Early on December 24 deep convection associated with the system moved over the low level circulation center whilst the system was getting better organized. Later that day at 1800 UTC the Depression was upgraded to a category one tropical cyclone and was named Judy whilst located about 510km (320miles) southeast of Tahiti and moving towards the southwest. During the next few hours under strengthening shear, Judy struggled to maintain itself. However, as it moved further to the south it came under a strengthening steering field which was being enhanced by a trough of low pressure to the west of the steering field which helped to neutralize the effect of the shear over the cyclone. Judy then intensified slightly further and reached its peak intensity of 85 km/h (50 mph), with a peak pressure of 989 hPa late on December 25 whilst turning towards the south towards TCWC Wellington's area of responsibility. Judy degenerated into an extratropical cyclone during December 27, before it was last noted later that day as it merged with an area of low pressure to the south of Tahiti.[1]
| Basin: | SPac |
| Track: | Kerry 2005 track.png |
| Formed: | January 5 |
| Dissipated: | January 14 |
| 10-Min Winds: | 65 |
| 1-Min Winds: | 90 |
| Pressure: | 970 |
Tropical Cyclone Kerry developed from Tropical Depression 05F on January 5, 315nmi northeast of Port Vila, Vanuatu. Kerry moved to the southwest with 40-1NaN-1 winds as it moved over Vanuatu. Once past the island, Kerry moved on a west-southwest course and it began to intensify after turning to the west. The storm reached a peak intensity of 85kn before turning towards the south-southeast. The storm began to weaken under vertical shear and was downgraded to a depression on January 13.[2]
| Basin: | SPac |
| Track: | Lola 2005 track.png |
| Formed: | January 26 |
| Dissipated: | February 2 |
| 10-Min Winds: | 40 |
| Pressure: | 990 |
Tropical Storm Lola developed from Tropical Depression 06F on January 31, 100nmi west-southwest of Tongatapu. Lola reached a peak intensity of 40kn, but was downgraded to a depression on February 2.[3]
See main article: Cyclone Meena.
| Basin: | SPac |
| Track: | Meena 2005 track.png |
| Formed: | February 1 |
| Dissipated: | February 8 |
| 10-Min Winds: | 115 |
| 1-Min Winds: | 125 |
| Pressure: | 915 |
On February 1, the RSMC Nadi began monitoring a tropical disturbance, which they designated as 07F, to the west of the Northern Cook Islands.[1] The next day, a small area of deep convection developed.[4]
| Basin: | SPac |
| Track: | Olaf 2005 track.png |
| Formed: | February 10 |
| Dissipated: | February 20 |
| 10-Min Winds: | 115 |
| 1-Min Winds: | 145 |
| Pressure: | 915 |
See main article: Cyclone Olaf. The most intense system of the season, Tropical Cyclone Olaf developed rapidly like Nancy. By February 16, Olaf had attained maximum sustained winds of 145kn and was thrashing American Samoa. However bad the damage was, it could have been worse as Olaf veered east, its eyewall missing the islands.
| Basin: | SPac |
| Track: | Nancy 2005 track.png |
| Formed: | February 10 |
| Dissipated: | February 17 |
| 10-Min Winds: | 95 |
| 1-Min Winds: | 125 |
| Pressure: | 935 |
See main article: Cyclone Nancy. Cyclone Nancy formed on February 10 as Tropical Disturbance 09F, over the next couple of days. The disturbance gradually developed and was designated as Cyclone Nancy during February 12 due to its outflow improving and a small area of deep convection, developing over the center of circulation, whilst it was located about 485km (301miles) east-northeast of Pago Pago, American Samoa. During that day Nancy started to rapidly intensify becoming a Severe Tropical Cyclone late on February 13 as a small, irregularly shaped, eye had begun to develop.
The next day both RSMC Nadi, and the JTWC reported that Cyclone Nancy had attained its peak intensity of 175 km/h (110 mph 10-minute winds) and 230 km/h (145 mph 1-minute winds). Increasing wind shear then caused Nancy to weaken. Early on February 15, the storm passed directly over Manuae. Continued weakening took place as a trough of low pressure approached from the southwest. By February 16, Nancy weakened below hurricane intensity and turned to the southwest as it began to undergo a Fujiwhara interaction with Cyclone Olaf, strong shear associated with the outflow of Cyclone Olaf caused all convection associated with Nancy to be displaced to the southwest on February 16. Early on February 17, Nancy transitioned into an extratropical cyclone as it entered the area of responsibility of TCWC Wellington. Shortly afterwards, the low was absorbed into the larger circulation of Olaf however it was monitored by TCWC Wellington as a separate system until 1200 UTC on February 18.
Already impacted by Cyclone Meena a week earlier, the Cook Islands sustained significant damage from Cyclone Nancy. Several homes were damaged and destroyed throughout the islands. Downed trees and power lines blocked roads and cut power and minor flooding was reported along coastal areas.
| Basin: | SPac |
| Track: | Percy 2005 track.png |
| Formed: | February 24 |
| Dissipated: | March 5 |
| 10-Min Winds: | 125 |
| 1-Min Winds: | 140 |
| Pressure: | 900 |
See main article: Cyclone Percy. Percy quickly formed from an area of low pressure on February 24 and reached Category 1 status north of American Samoa. The cyclone then moved eastward, peaking at Category 5 status before turning southward. Percy then passed through the southwestern Cook Islands causing severe damage before dissipating.[5]
| Basin: | SPac |
| Track: | Rae 2005 track.png |
| Formed: | February 28 |
| Dissipated: | March 6 |
| 10-Min Winds: | 40 |
| 1-Min Winds: | 35 |
| Pressure: | 990 |
| Basin: | SPac |
| Type: | spdepression |
| Formed: | March 2 |
| Dissipated: | March 4 |
| Pressure: | 1001 |
Late on February 27, RSMC Nadi reported that a suspect tropical disturbance was developing near to the north of Rennel Island, in the Solomon Islands. Over the next couple of days the system gradually developed and before it was declared as a tropical disturbance early on March 1. At this time convection detached from the disturbance's low level circulation center, whilst vertical wind shear around the system remained weak.[6] [7] Early the next day, the Disturbance was then relocated to the northwest of Viti Levu in Fiji, before it was designated as Tropical Depression 13F later that day.[8] [9] The Depression remained weak reaching an estimated central pressure of 1001 hPa (mbar) early on March 3, however there were no winds reported by RSMC Nadi whilst they were monitoring it.[9] [10] RSMC Nadi then issued their last advisory on 13F early on March 4 after no persistent convection reported around the system since the depression reached its peak pressure.[9] [11]
| Basin: | SPac |
| Formed: | April 14 |
| Dissipated: | May 1 |
| 10-Min Winds: | 30 |
| Pressure: | 1000 |
See also: List of off-season South Pacific tropical cyclones.
| Basin: | SPac |
| Track: | Sheila 2005 track.png |
| Formed: | April 20 |
| Dissipated: | April 23 |
| 10-Min Winds: | 40 |
| Pressure: | 990 |
Tropical Depression 01F developed on October 28, within the monsoon trough about 420round=5NaNround=5 to the northeast of Guadalcanal.[12] [13] Over the next couple of days the system moved westwards and moved into the Australian region, during October 30, where it was monitored for a few days by TCWC Brisbane.[12] The second tropical depression of the season developed on December 3, about 280km (170miles) to the north of Port Villa, Vanuatu.[14] Over the next week the poorly organised system meandered over the ocean between Vanuatu and Fiji, before it started to organise during December 12, with RSMC Nadi issuing gale warnings on the system.[14] The system subsequently moved southwards between Vanuatu and Fiji, before it was last noted during December 14, while it was located to the southeast of Port Villa.[14] While Tropical Depression 02F was active, the third tropical depression of the season, developed to the south of Tuvalu on December 5.[14] The system subsequently moved south-eastwards, before it was last noted during December 10 to the east of Nuku'alofa, Tonga.[14]
During February 26, RSMC Nadi reported that Tropical Depression 11F had formed, within the Tuamotu Archipelago of islands in French Polynesia.[15] During the next day the system moved eastwards before it was last noted during the next day as it degenerated into a tropical disturbance.[16] [17]
During April 20 Tropical Disturbance 16F developed within a monsoon trough, about 570km (350miles) to the southeast of Apia on the Samoan island: Upolu.[18] During April 21, the disturbance moved towards the southwest and affected Niue while starting to rapidly weaken, before it was last noted during April 22 wrapping into Cyclone Sheila's circulation.[19] [20] [21] Tropical Depression 17F then developed on April 26 while located about 710km (440miles) to the northeast of Pago-Pago in American Samoa.
During April 29, Tropical Depression 18F developed within a monsoon trough about 635km (395miles), to the northeast of Suva, Fiji.[22] Over the next 24 hours the system moved towards the southeast while deep convection surrounding the system failed to become organized and started to weaken.[23] The depression was last noted during the next day, as it dissipated about 445km (277miles), to the northeast of Suva.[20]
This table lists all the storms that developed in the South Pacific to the east of longitude 160°E during the 2004–05 season. It includes their intensity on the Australian Tropical cyclone intensity scale, duration, name, landfalls, deaths, and damages. All data is taken from RSMC Nadi and/or TCWC Wellington, and all of the damage figures are in 2005 USD.
|-| || || bgcolor=#| || bgcolor=#| || bgcolor=#| || || || ||[24] |-| || || bgcolor=#| || bgcolor=#| || bgcolor=#| || || || ||[25] |-| || || bgcolor=#| || bgcolor=#| || bgcolor=#| || || || ||[25] |-| || || bgcolor=#| || bgcolor=#| || bgcolor=#| || || || ||[26] |-| || || bgcolor=#| || bgcolor=#| || bgcolor=#| || || || ||[26] |-| || || bgcolor=#| || bgcolor=#| || bgcolor=#| || || || ||[26] |-| || || bgcolor=#| || bgcolor=#| || bgcolor=#| || Cook Islands || || None ||[26] |-| || || bgcolor=#| || bgcolor=#| || bgcolor=#| || Samoan Islands, Cook Islands || || None ||[26] |-| || || bgcolor=#| || bgcolor=#| || bgcolor=#| || Samoan Islands, Cook Islands || || None ||[26] |-| || || bgcolor=#| || bgcolor=#| || bgcolor=#| || Tokelau, Samoan Islands, Cook Islands || || None ||[26] |-| || || bgcolor=#| || bgcolor=#| || bgcolor=#| || French Polynesia || None || None |||-| || || bgcolor=#| || bgcolor=#| || bgcolor=#| || No areas affected || None || None ||[26] |-| || || bgcolor=#| || bgcolor=#| || bgcolor=#| || || || ||[27] |-| || || bgcolor=#| || bgcolor=#| || bgcolor=#| || || || ||[28] |-| || || bgcolor=#| || bgcolor=#| || bgcolor=#| || || || ||[26] |-| || || bgcolor=#| || bgcolor=#| || bgcolor=#| || Niue || || |||-| || || bgcolor=#| || bgcolor=#| || bgcolor=#| || || || ||[28] |-| || || bgcolor=#| || bgcolor=#| || bgcolor=#| || || || ||[28] |-