Australian cyclone season 2010-2011

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Australian cyclone season 2010-2011
All the storms of the season
All the storms of the season
Formation of the
first storm
October 28, 2010
Dissolution of the
last storm
April 20, 2011
Strongest storm Yasi - 929  hPa  ( mbar ), 115  kn  (215  km / h )  (10 minutes)
Tropical lows 28
Tropical cyclones 11
Tropical cyclones 6th
Total number of victims 3 total
Total damage Unknown
Australian cyclone
seasons 2008-09 , 2009-10 , 2010-11 , 2011-12 , 2012-13
Bureau of Meteorology
Intensity of Tropical Cyclones
category Wind 10 minutes
continuously
Gusts
Trop.
Deep
<34 kn
<63 km / h
-
one 34-47 kn
63-87 km / h
<66 kn
<122 km / h
Two 48-63 kn
88-142 km / h
67-90 kn
122-167 km / h
Three 64-85 kn
143-158 km / h
91-121 kn
167-224 km / h
Four 86-110 kn
159-204 km / h
122-150 kn
205-278 km / h
five > 111 kn
> 205 km / h
> 151 kn
> 279 km / h

The 2010–2011 Australian cyclone season officially began on November 1, 2010 and lasted through April 30, 2011 .

The operational plan of the World Meteorological Organization also provides for a “tropical cyclone year” for the waters in the southern hemisphere . This began on July 1, 2010 and will end on June 30, 2011.

The Australian cyclone season includes storms that form south of the equator between 90th and 160th degrees east. These include Australia, Papua New Guinea , the western part of the Solomon Islands , East Timor and the southern areas of Indonesia . Tropical cyclones in this area are monitored by five Tropical Cyclone Warning Centers (TCWCs): the Bureau of Meteorology in Perth , Darwin and Brisbane , Australia; the TCWC Djakarta in Indonesia and the TCWC Port Moresby in Papua New Guinea.

The Joint Typhoon Warning Center issues unofficial warnings for this region for U.S. facilities. The extension "S" is used if the storm forms west of 135 ° east longitude and a "P" if this happens east of this line.

Season forecasts

Bureau of Meteorology

Since the Australian cyclone season 2009–2010 , the National Climate Center (NCC) of the Bureau of Meteorology has issued a forecast prior to the cyclone season that predicts tropical cyclone activity in the entire basin between 90 ° E and 160 ° E. For the first time this season, the NCC not only predicted the total number of cyclones in the waters around Australia for the tropical cyclone year from July 2010 to June 2011, but also divided the forecast into the regions west, northwest, north and east. For the cyclone year 2010–2011, the BoM assumed that due to the La Niña effect, cyclone activity could start about two weeks earlier than usual.

Forecasts of tropical cyclonic activity
Warning
center
date Average
activity
Predicted
activity
Actual
activity
All in all October 2010 12 20-22 0
west October 2010 7th 11-12 0
northwest October 2010 6th 7-8 0
North October 2010 4th 5 0
east October 2010 4th 6-7 0
Source: BoM's seasonal forecast for tropical cyclones.
––––––––––––––––––––––––––––––––––––––––––
total November 2010 12-15 19th 4th
west November 2010 9-10 14th 3
east November 2010 5-6 7th 1
Source: GCACIC seasonal forecast for tropical cyclones.

For the cyclone year 2010/2011, the NCC assumed that the Australian region could have the most active cyclone season since the cyclone season 1983–1984 , with 20–22 tropical cyclones forming in or migrating into the region to the average of twelve tropical cyclones. For the western part of the Bureau of Meteorology's area of ​​responsibility, the NCC predicts the formation of eleven to twelve tropical cyclones, as opposed to the average of seven. The NCC estimates seven to eight cyclones forming or passing through the northwest, with an average of six in this part of the basin. For the northern region, the NCC stated that it anticipates five cyclones in this area. However, the NCC pointed out that forecasting skills of meteorologists in this area were rather poor. For the eastern part of the Australian waters, the NCC announced that it anticipates six to seven cyclones, with an average of four in this area.

City University of Hong Kong

Since the 2009–2010 cyclone season , the Guy Carpenter Asia-Pacific Climate Impact Center (GCACIC) at the City University of Hong Kong (CityUHK) has published seasonal forecasts for the coming cyclone season. This forecast of cyclone activity will be made for the region as a whole and separately for the western part of the basin between 90 ° E and 135 ° E and will be published in November.

  1. a b This area has been defined by the Bureau of Meteorology as between 105 ° E and 130 ° E.

Storms

Tropical cyclone Anggrek

Tropical low ( BoM )
Tropical storm
Anggrek 2 November 2010.jpg Anggrek 2010 track.png
Duration October 28th - November 4th
intensity 40 kn (75 km / h ) (10 minutes) , 995 hPa

On October 28, the TCWCs of the Bureau of Meteorology in Perth and Darwin reported that in the area of ​​responsibility of the TCWC in Jakarta, about 650 km west of Jakarta and about 530 km north of the Cocos Islands, a westward moving tropical low had formed. The system then turned on a southeastern trajectory and intensified continuously over the following days. Early on October 31, the TCWC Djakarta determined that the system had reached the strength of a tropical cyclone and named the storm Anggrek . Anggrek moved further south and reached the area of ​​responsibility of the TCWC in Perth. Meanwhile, it had intensified into a Category 2 cyclone on the Bureau of Meteorology scale. On November 2, the cyclone passed east of the Cocos Islands - for which the highest warning level has meanwhile been declared and where heavy rain and gusty winds were recorded during the passage from Anggrek - and weakened again due to increasing wind shear. The cyclone then made a curve to the right towards the southwest and weakened further in the process. Eventually the remaining low drifted westward and continued to lose intensity. On November 4th, the TCWC in Perth reported the weakening to a tropical low and issued the final warning.

Tropical cyclone Abele

Tropical Category 2 Cyclone ( BoM )
Category 1 cyclone
Abele dec 1 2010.jpg Abele 2010 track.png
Duration December 2nd (from Southwestern India) - December 4th
intensity 50 kn (95 km / h ) (10 minutes) , 987 hPa

On November 29, a tropical low pressure area formed west of the 90th east longitude, which was classified by the TCWC Perth as tropical low 02U . The system initially moved south and intensified in the south-west of the Indic to a tropical cyclone, but then moved in a south-easterly direction and on December 3 came under the responsibility of the TCWC in Perth. RSMC La Reunion issued its final warning to Abele when the cyclone had already crossed 90 degrees east in a southeast direction. According to this warning, Abele had the intensity of a Category 2 cyclone on the Australian scale. The Bureau of Meteorology took over responsibility for Abele a few hours later and downgraded the system to a Category 1 cyclone. On December 4, the storm turned to a south-southeast migratory direction and weakened to a tropical low, so that the TCWC in Perth issued the final warning on Abele. The remaining low of the previous cyclone moved slowly in a south-easterly direction for two days and continued to lose strength and dissolved completely on December 6th.

Tropical low 03U

Tropical low ( BoM )
Temporary cyclone south.svg 03U 2010 track.png
Duration December 15 - December 20
intensity 30 kn (55 km / h ) (10 minutes) , 989 hPa

On December 15, a monsoon depression formed off the coast of Western Australia , around 500 km northwest of Exmouth , which slowly drifted to the south-east. Gusts and heavy rain reached areas far from the center of the low that crossed the coastline near Coral Bay on December 18 . Shortly after landfall, the system swung sharply to the south-west, reaching the waters of the Indian Ocean west of Carnarvon on December 19 . The system then moved away from the coast and disintegrated late on December 20 about 500 km west of Geraldton .

The Gascoyne River and its catchment area fell heavily on December 16-19, causing one of the worst floods on the river in recorded history. The tropical rainfall also had on other river basins in the region, including the Wooramel River , Murchison River , Lyndon River , Minilya River, and Ashburton River . For the period from December 16 to 20, some weather stations reported rainfall of up to 300 mm, which corresponds to the long-term average annual rainfall in the region. The station at Carnarvon Airport reported the highest amount of precipitation within 24 hours on December 17 with 207.8 mm, which is the highest amount of precipitation measured there within one day since records began in Carnarvon in 1883. The previous record of 119.4 mm was measured on March 24, 1923.

According to preliminary estimates, the damage amounted to around 100 million Australian dollars (about US $ 100.4 million), and at least 2,000 head of cattle drowned by the flood.

Tropical low 04U

Tropical low ( BoM )
Temporary cyclone south.svg
Duration December 22nd - December 24th
intensity 30 kn (55 km / h ) (10 minutes)

Tropical cyclone Tasha

Tropical Category 1 Cyclone ( BoM )
Tropical storm
Tasha dec 25 2010 0040Z.jpg Tasha 2010 track.png
Duration December 20th - December 25th
intensity 40 kn (75 km / h ) (10 minutes) , 993 hPa

Tasha was a relatively weak cyclone, but it brought large amounts of rainfall to Queensland . On December 20, a tropical low formed in the northern Coral Sea, southeast of Papua New Guinea. The system slowly moved in a roughly south-westerly direction and finally on December 24th came into an environment favorable to the development of a tropical storm. Within a few hours, the system gained enough power to be classified as a Category 1 cyclone by the TCWC Brisbane. Only a few hours later, the center of the cyclone reached Gordonvale , between Cairns and Innisfail , across the tropical north of the state. Over land, the cyclone was soon downgraded to a tropical low before breaking up on December 25th.

On the south side of the cyclone, rainfall was recorded between 150 and 250 mm. Tasha thus soaked the soil and in combination with prolonged monsoon rains in the following days, the strongest floods for decades occurred .

Tropical low 06U

Tropical low ( BoM )
06U jan 1 2011 0220Z.jpg 06U 2010 track.png
Duration December 30th - January 4th
intensity 30 kn (55 km / h ) (10 minutes) , 993 hPa

At the end of December, a tropical low formed over the top end of the Northern Territory , which migrated continuously in a west-southwest direction to Western Australia . TCWC Perth began on December 30th when the system swept across the Kimberley and reached the Indian Ocean north of Broome . 06U slowly intensified over the warm ocean waters , but dissolved on January 4th, so the TCWC in Perth issued the final warning about the system that day.

Tropical low 07U

Tropical low ( BoM )
Temporary cyclone south.svg
Duration January - January
intensity 30 kn (55 km / h ) (10 minutes)

Tropical low 08U

Tropical low ( BoM )
Temporary cyclone south.svg
Duration January - January
intensity 30 kn (55 km / h ) (10 minutes)

Tropical cyclone Vince

Tropical Category 1 Cyclone ( BoM )
Tropical storm
Temporary cyclone south.svg Vince 2011 track.png
Duration January 10th - January 15th
intensity 40 kn (75 km / h ) (10 minutes) , 986 hPa

On January 10, a tropical low formed about 700 km north-northwest of Onslow off the coast of Western Australia, which initially moved westward. It intensified into a cyclone two days later and abruptly changed direction on January 12th. Over the next few days, the system, named Vince by the TCWC in Perth , moved east-south-east. Predictions initially assumed that Vince would intensify into a Category 2 cyclone, but on January 14th the cyclone lost its organization and weakened to a tropical low.

Severe tropical cyclone Zelia

Tropical Category 4 Cyclone ( BoM )
Category 2 cyclone
Zelia 16 January 2011.jpg Zelia 2011 track.png
Duration January 13 - January 16 (East of 160 ° East)
intensity 100 kn (185 km / h ) (10 minutes) , 943 hPa

On January 13, a tropical low of 10U formed in the Coral Sea northeast of Willis Island . This initially bobbed to the west and north, before embarking on a south-eastern railway over the east. On January 14, the system had intensified about 750 km northeast of Cairns to such an extent that it was upgraded to a tropical cyclone by the TCWC in Brisbane and given the name Zelia . Zelia continued on its southeastern trajectory and reached the western Coral Sea under the influence of a subtropical ridge . On January 15, the system intensified rapidly to a Category 3 cyclone and a day later the storm west of New Caledonia reached its greatest intensity. On that day, Zelia crossed the 160th east longitude and reached the South Pacific Basin , quickly losing strength due to increasing wind shear and decreasing water surface temperatures. It was downgraded to a tropical low on January 18 and lost its tropical properties in the Tasman Sea northwest of New Zealand.

Tropical cyclone Anthony

Tropical Category 2 Cyclone ( BoM )
Tropical storm
Anthony jan 22 2011.jpg Anthony 2011 track.png
Duration January 21st - January 31st
intensity 55 kn (100 km / h ) (10 minutes) , 984 hPa

Moving parallel to the coast of Queensland, a low pressure area slowly developed, which on January 22nd, northeast of Cairns, was classified by the TCWC in Brisbane as Tropical Low 11U . The system then moved northeast and intensified. Late on January 22nd UTC, the system was upgraded to a tropical cyclone and named Anthony . After Anthony passed Willis Island to the north, the cyclone embarked on an east-southeast trajectory towards New Caledonia . On January 24th, the system reached the South Pacific Basin, but the slowing speed of the migratory system initiated a reversal of migratory direction, so the TCWC in Brisbane retained responsibility for primary monitoring of the system. During the day, strong wind shear and poor system organization led to a weakening to a tropical low. This moved briefly in a southerly direction, but then swung on a west-northwest orbit.

Back in the area of ​​responsibility of the TCWC in Brisbane, the low intensified and regained cyclone status on January 29th. The cyclone hooked north before drifting steadily in a southwesterly direction until it made landfall north of Bowen in southeast Queensland. In doing so, Anthony intensified into a Category 2 cyclone, but quickly lost power after crossing the coast and was downgraded to a tropical low.

Heavy tropical cyclone Bianca

Tropical Category 4 Cyclone ( BoM )
Category 2 cyclone
Bianca 28 jan.jpg Bianca 2011 track.png
Duration January 23rd - January 30th
intensity 90 kn (165 km / h ) (10 minutes) , 945 hPa

Tropical low 13U

Tropical low ( BoM )
Temporary cyclone south.svg
Duration January - January
intensity 25 kn (45 km / h ) (10 minutes) , 1006 hPa

Severe tropical cyclone Yasi

Tropical Category 5 Cyclone ( BoM )
Category 4 cyclone
Cyclone Yasi February 2, 2011 approaching Queensland.jpg Yasi 2011 track.png
Duration January 31st (From the South Pacific) - February 3rd
intensity 115 kn (215 km / h ) (10 minutes) , 929 hPa

On January 26th, a tropical disturbance had already formed in the area of ​​responsibility of the RSMC Nadi, which had intensified to such an extent by January 30th that it was named Yasi as a category 1 cyclone . The cyclone moved westward over Vanuatu , intensified further and crossed the 160th longitude east as a Category 3 cyclone on January 31. In the Coral Sea, Yasi intensified rapidly and on February 1 reached category 5 on the Australian cyclone scale. Even though Yasi weakened slightly before landfall, it still reached the coast near Innisfail on February 2, still in the highest category. Even before the cyclone hit, the Queensland government had ordered the evacuation of the particularly endangered areas. Thousands of residents were brought to safety.

Overland, the cyclone quickly lost its power and steadily weakened. It lost cyclone status about 50 km east of Mount Isa on February 3 .

Tropical low 15U

Tropical low ( BoM )
Tropical storm
15U 8 February 2011.jpg 15U 2011 track.png
Duration February 8th - February 13th
intensity 30 kn (55 km / h ) (10 minutes) , 996 hPa

On February 8, a low pressure area formed off the coast of Western Australia, which moved steadily in a west-southwest direction over the following days. On February 11, the Bureau of Meteorology in Perth classified the system as a tropical low and gave it the identification 15U . The JTWC began issuing warnings under the designation 14S a few hours later . The TCWC in Perth assumed an intensification of the system into a tropical category 1 cyclone, but strong wind shear and a cool water surface hindered the organization, so that the system remained a low and dissolved on February 13th.

Severe tropical cyclone Dianne

Category 3 cyclone ( BoM )
Category 1 cyclone
Dianne feb 20 2011 0635Z.jpg Dianne 2011 track.png
Duration February 11th - February 22nd
intensity 70 kn (130 km / h ) (10 minutes) , 962 hPa

On February 11th, an intensifying low pressure area developed off the north coast of Western Australia. Due to the proximity to the coast, the TCWC issued a cyclone warning for the coastal towns between Onslow and Coral Bay on January 15, because the system had developed into a tropical low 350 km north-northwest of Exmouth. Late on February 16, 16U intensified into a tropical cyclone and was named Dianne .

Severe tropical cyclone Carlos

Category 3 cyclone ( BoM )
Category 1 cyclone
Carlos 24 February 2011.jpg Carlos 2011 track.png
Duration February 12th - February 27th
intensity 65 kn (120 km / h ) (10 minutes) , 968 hPa

On February 14, the Tropical Cyclone Warning Center (TCWC) in Darwin reported that a tropical depression had developed over land at 13.2 ° S and 130.7 ° E, about 40 km west-southwest of Batchelor . A severe weather warning was issued for the northwest of the Darwin-Daly district and the Tiwi Islands . The system was initially steered through a strong subtropical ridge from north to north-northeast. The slowly moving system intensified into a tropical cyclone on February 16 and was named Carlos . Once over water, Carlos turned east. As the ridge south of the cyclone was slowly weakening, the meteorologists predicted a clockwise loop before Carlos embarked on a southwestern trajectory.

Heavy rain fell in the region on February 15, with the Marrara measuring stations reporting 179.4 mm and Darwin Airport 131.0 mm of precipitation. During the same period, Darwin fell 339.6 mm of precipitation, which is the highest amount of rain ever recorded in Darwin in a 24-hour period. The cyclone knocked down trees and caused building damage. Schools, the international airport and the port on the East Arm were closed.

Back overland, the system weakened and was downgraded to a tropical low. A total of 684.8 mm of precipitation was recorded within three days due to the slowly moving cyclone at Darwin's airport. The system then slowly retreated southwest of Darwin and moved towards the border between the Northern Territory and Western Australia. In the settlement of Daly River , 442 mm of precipitation was measured in connection with Carlos. On February 19, the system reached the north of the Kimberley region . However, at 90 mm in Wyndham and 80 mm in Kalumburu , rainfall was not as high as in the previous days.

Early on February 21, Carlos crossed the Indian Ocean after crossing Kimberley, which led to renewed intensification into a cyclone. In the mining town of Karratha , a line of gusts from the cyclone generated a total of four tornadoes , damaging 38 houses and numerous vehicles as well as a school. Carlos intensified steadily into a category 2 cyclone above water.

On February 22nd, the system moved parallel to the Pilbara coast . Varanus Island reported 59 mm of rain and the strongest gust of wind in the area was measured on Bedout Island at 120 km / h. The system continued to organize itself better. On February 23, a new rain record was set at this station at 283 mm on Barrow Island . The strongest gusts on this day were registered on Varanus Island at 139 km / h. The cyclone crossed the North West Cape and hit Onslow and Exmouth with rain and strong winds of up to 155 km / h .

Carlos continued to move south-westerly, moving away from the west coast of Australia. The storm intensified into a severe tropical cyclone on February 24th. The storm broke up on February 27th over increasingly cool water.

Tropical low 18U

Tropical low ( BoM )
Temporary cyclone south.svg 18U 2011 track.png
Duration February 23 - February 28
intensity 30 kn (55 km / h ) (10 minutes) , 992 hPa

On February 25, the Tropical Cyclone Warning Center (TCWC) in Perth announced that a tropical depression had formed about 75 km west-northwest of Kalumburu and 445 km northeast of Derby , which slowly moved in a south-westerly direction parallel to the coast of Kimberley. In the early hours of February 28, the low in King Sound moved across the country. To the east of Port Hedland , the Dampier Peninsula recorded some significant rainfall, which affected the catchment areas of the Telfer River and partly De Gray River . Derby recorded 83 mm of rain, Camballin recorded 142 mm of rainfall and Looma 105 mm. The tropical depression continued to move inland and the Bureau of Meteorology issued the final warning on the system on February 28th.

Tropical low 19U

Tropical low ( BoM )
Temporary cyclone south.svg
Duration February 24 - Unknown
intensity Unknown wind force

Tropical low 20U

Tropical low ( BoM )
Temporary cyclone south.svg
Duration February 26 - Unknown
intensity Unknown wind force

Tropical low 21U

Tropical low ( BoM )
Temporary cyclone south.svg 12F 2011 track.png
Duration March 7th - March 8th ( East of 160 ° E )
intensity 25 kn (45 km / h ) (10 minutes) , 1004 hPa

On March 7, the TCWC Brisbane reported that a tropical low had formed in the Coral Sea about 1200 km west of Port Vila , Vanuatu . During the course of the day, the system moved eastwards and intensified continuously the following day, before it moved from the area of ​​responsibility of the Australian meteorologists to the South Pacific basin and there became Tropical Depression 12F .

Tropical low 22U

Tropical low ( BoM )
Temporary cyclone south.svg
Duration March 10th - March 15th
intensity Wind strength unknown, 1001 hPa

Tropical low 23U (Cherono)

Tropical low ( BoM )
Cherono 2011 track.png
Duration March 10 - March 14 (West of 90 ° E)
intensity Wind strength unknown, 1006 hPa

On March 10, the TCWC Perth reported that a tropical depression had formed in the area of ​​responsibility of the TCWC Djakarta, about 1640 km west of Djakarta, Indonesia. The system migrated slowly over the next two days. It came under the responsibility of the TCWC in Perth on March 13, before moving westward from the Australian region to the south-western Indian region. There it eventually developed into the Moderate Tropical Storm Cherono .

Tropical low 24U (Bune)

On March 23, the TCWC Brisbane classified Tropical Depression 13F in Becker in the South Pacific as Tropical Low 24U when it was located about 250 km northwest of Tonga. In the course of the following week 24U / 13F intensified continuously to the severe tropical cyclone Bune, which finally lost its tropical properties 1,450 km northeast of New Zealand. During its existence, Bune always stayed east of the 160th east longitude and was therefore not part of the Australian cyclone season.

Tropical low 25U

Tropical low ( BoM )
Tropical storm
TL 25U apr 2 2011 0205Z.jpg 25U 2011 track.png
Duration March 26th - April 6th
intensity 30 kn (55 km / h ) (10 minutes) , 995 hPa

Tropical low 25U formed off the north coast of Australia on March 26th. On March 31, the system was reported northwest of Darwin. The system initially drifted west, but moved south from April 1. On the night of April 2, 25U finally struck a south-west route to the Kimberley coast, which has already been exposed to heavy flooding after extensive rainfall. On April 6, the low disappeared completely.

Tropical low 26U

Tropical low ( BoM )
Temporary cyclone south.svg 26U 2011 track.png
Duration March 26th - April 2nd
intensity Wind strength unknown, 1006 hPa

Tropical low 27U

Tropical low ( BoM )
Temporary cyclone south.svg 08R 2011 track.png
Duration March 26th - April 2nd
intensity Wind strength unknown, 1006 hPa

On March 26, the TCWC Perth reported that a weak tropical low had formed about 315 km northwest of the Cocos Islands . During the next two days, the system slowly moved westwards and briefly came under the responsibility of the RSMC Le Réunion, then returned to the responsibility of the TCWC, and then bobbed around 90 degrees east longitude for a few days. On April 2, 27U completely dissolved over the open ocean.

Tropical cyclone Errol

Tropical Category 2 Cyclone ( BoM )
Tropical storm
Errol Apr 16 2011 0505Z.jpg Errol 2011 track.png
Duration April 10th - April 20th
intensity 55 kn (100 km / h ) (10 minutes) , 986 hPa

A tropical depression formed north of the Tiwi Islands on April 10, and it developed slowly as it moved westward. The system suddenly changed direction and moved southeast from April 12-14. On April 15th, the system intensified into a tropical storm and was named Errol. After another course change, cyclone Errol migrated northwest and intensified on April 16 in category 2 cyclone on the Australian scale. On April 20th, Errol broke up.

Season overview

Zyklon Yasi

Storm names

The various Tropical Cyclone Warning Centers give names to storms that form in their respective areas of responsibility. The storms keep their name as they move from one jurisdiction to another. However, storms that are under the responsibility of Météo-France on Réunion will be renamed there. Storms that come from there into the area of ​​responsibility of the TCWC in Perth keep the name given in the south-western Indian Ocean. On the following lists of names, names that have not yet been assigned this cyclone season are shown in light gray .

TCWC Djakarta

The TCWC in Djakarta observes tropical cyclones that form between the equator and 10 ° south latitude and between 90 ° and 125 ° east longitude. Special storm warnings are being issued in this area by the Australian Bureau of Meteorology . Should a tropical cyclone form within this area of ​​responsibility, the TCWC Djakarta will assign a name from the following list; the only name given in 2010 was Anggrek. In the 2009-2010 season, no storm was named by the TCWC Djakarta.

  • Anggrek
  • Bakung  (unused)
  • Cempaka  (unused)
  • Dahlia  (unused)
  • Flamboyan  (unused)
  • Kenanga  (unused)
  • Lili  (unused)
  • Mawar  (unused)
  • Seroja  (unused)
  • Teratai  (unused)

TCWC Port Moresby

Tropical cyclones that form between 10 ° south and the equator and between 141 ° and 160 ° east are given names by the Tropical Cyclone Warning Center in Port Moresby , Papua New Guinea . The formation of tropical cyclones in this area is rare; during the 2007-2008 season there was only one storm, cyclone Guba. The following list names the names given by the TCWC in Port Moresby. It is unclear what the next name will be given. In the 2009-2010 season, no storm was named by the TCWC Port Moresby.

  • Aluminum  (unused)
  • Buri  (unused)
  • Dodo  (unused)
  • Emau  (unused)
  • Fere  (unused)
  • Hibu  (unused)
  • Ila  (unused)
  • Kama  (unused)
  • Lobu  (unused)
  • Maila  (unused)

TCWCs in Perth, Darwin and Brisbane

Since the beginning of the cyclone season 2008-2009, the Australian Bureau of Meteorology has only used a single list of names, but still operates three TCWCs, in Perth , Darwin and Brisbane . These monitor all tropical cyclones that form between 90 ° and 160 ° east longitude and issue special warnings if cyclones occur in the areas of responsibility of the TCWCs in Djakarta or Port Moresby. The first name given was Tasha .

Anika Anthony Alessia Alfred Ann
Billy Bianca Bruce Blanche Blake
Charlotte Carlos Christine Caleb Claudia
Dominic Dianne Dylan Debbie Damien
Ellie Errol Edna Ernie Esther
Freddy Fina Fletcher Frances Ferdinand
Gabrielle Grant Gillian Greg Gretel
Herman Heidi Hadi Hilda Harold
Ilsa Iggy Ita Ira Imogen
Jasper Jasmine Jack Joyce Joshua
Kirrily Koji Kate Kelvin Kimi
Lincoln Lua Lam Linda Lucas
Megan Mitchell Marcia Marcus Marian
Neville Narelle Nathan Nora Noah
Olga Oswald Olwyn Owen Odette
Paul Peta Quang penny Paddy
Robyn Rusty Raquel Riley Ruby
Sean Sandra Stan Savannah Seth
Tasha Tim Tatiana Trevor Tiffany
Vince Victoria Uriah Veronica Vernon
Zelia Zane Yvette Wallace -

The name Yasi is not on any of the name lists for the Australian region, but was given in the South Pacific Basin by the RSMC Nadi of the Fiji Meteorological Service when the cyclone was still in their area of ​​responsibility.

See also

Individual evidence

  1. a b Tropical Cyclone Operational plan for the South Pacific & Southeast Indian Ocean ( English , PDF; 1.7 MB) World Meteorological Organization . Retrieved October 22, 2010.
  2. a b c d e Seasonal Outlook for Tropical Cyclones . Bureau of Meteorology. October 18, 2010. Archived from the original on October 18, 2010. Retrieved October 18, 2010.
  3. Tropical Cyclone Outlook ( English ) Bureau of Meteorology. October 20, 2009. Archived from the original on October 6, 2010. Retrieved October 6, 2010.
  4. BoM warns that cyclone season could be worst in 27 years (English) , mysailing.com.au. October 8, 2010. Retrieved October 27, 2010. 
  5. ^ Tropical Cyclone three-day outlook for the Western Region 2010-10-28 ( English ) In: TCWC Perth . Bureau of Meteorology. October 28, 2010. Archived from the original on October 28, 2010. Retrieved on October 28, 2010.
  6. Tropical Cyclone Advice # 5 (TC 01U) ( English ) In: TCWC Perth . Bureau of Meteorology. October 31, 2010. Archived from the original on October 31, 2010. Retrieved on October 31, 2010.
  7. ^ Western Australian Regional Office: Severe Tropical Cyclone Abele ( English ) Bureau of Meteorology. 2010. Retrieved December 15, 2010.
  8. a b c Gascoyne River Flood . Bureau of Meteorology . 2010. Archived from the original on January 11, 2011. Info: The archive link was automatically inserted and not yet checked. Please check the original and archive link according to the instructions and then remove this notice. Retrieved January 21, 2011. @1@ 2Template: Webachiv / IABot / www.bom.gov.au
  9. ^ Queensland Regional Office: Tropical Cyclone Tasha ( English ) Bureau of Meteorology . Retrieved February 2, 2011.
  10. ^ Tropical Cyclone Advice No. 19 for Tropical Cyclone Anthony ( English ) Tropical Cyclone Warning Center, Brisbane. Archived from the original on January 30, 2011. Retrieved January 30, 2011.
  11. ^ Tropical Cyclone three-day outlook for the Western Region ( English ) Tropical Cyclone Warning Center, Perth. Archived from the original on February 8, 2011. Retrieved February 13, 2011.
  12. ^ Tropical Cyclone Technical Bulletin for Tropical Low 15U ( English ) Tropical Cyclone Warning Center, Perth. Archived from the original on February 11, 2011. Retrieved on February 13, 2011.
  13. ^ Tropical Cyclone Warning 01 for Tropical Cyclone 14S ( English ) Joint Typhoon Warning Center . Archived from the original on February 11, 2011. Retrieved on February 13, 2011.
  14. ^ Final Tropical Cyclone Technical Bulletin for Tropical Low 15U ( English ) Tropical Cyclone Warning Center, Perth. Archived from the original on February 12, 2011. Retrieved February 13, 2011.
  15. ^ Tropical Cyclone Warning Center, Perth: TROPICAL CYCLONE WATCH - TROPICAL CYCLONE ADVICE NUMBER 1 (16U) ( English ) Bureau of Meteorology. Archived from the original on February 15, 2011. Retrieved February 15, 2011.
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