Cyclone Inigo

{{storm path|Inigo 2003 track.png}}

On 26 March, an area of disturbed weather was located within the near-equatorial trough near Papua New Guinea. Initially located within an area of easterly wind shear, it tracked westward, due to the presence of a ridge to its south, and on 27 March, a low-pressure area formed over Western New Guinea. Thunderstorm activity increased around a mid-level circulation as it crossed into the Arafura Sea, and its overall organisation continued to increase. On 29 March, a low-level circulation was visible, though significant tropical development was prevented due to wind shear and land interaction with islands in the Indonesian archipelago. The system developed into a tropical low on 30 March. After turning to the southwest, the tropical low crossed the island of Flores on 31 March; upon doing so, the storm's convection greatly increased, due to increased upper-level divergence, which produced heavy rainfall on Flores and Timor. On 1 April, wind shear decreased as the system crossed into the Savu Sea, and the storm developed into a tropical cyclone to the northeast of Sumba.{{cite web|author=Bureau of Meteorology Special Services Unit|year=2003|title=Tropical Cyclone Inigo (30 March – 8 April)|publisher=Government of Australia|access-date=5 January 2008|url=http://ssu1.bom.gov.au/wa/cyf/reports/Inigo/Inigo.htm|url-status=dead|archive-url=https://web.archive.org/web/20060827151915/http://ssu1.bom.gov.au/wa/cyf/reports/Inigo/Inigo.htm|archive-date=27 August 2006}}

At 1200 UTC on 1 April, the Joint Typhoon Warning Center (JTWC) issued its first advisory on the system, classifying it as Tropical Cyclone 26S. At 0000 UTC on 2 April, the Bureau of Meteorology (BOM) warning centre in Perth classified the system as Tropical Cyclone Inigo.{{cite web|author=Gary Padgett|year=2003|title=April 2003 Worldwide Tropical Weather Summary|access-date=5 January 2008|url=http://www.australiansevereweather.com.au/cyclones/2003/summ0304.htm}} The storm quickly intensified as it tracked southwestward, aided by low wind shear and strong divergence. An eye featured gradually organised, and early on 3 April, the BOM classified Inigo as a severe tropical cyclone, with winds of {{convert|80|mph|km/h|abbr=on}}. Later that day, the cyclone underwent rapid intensification, as the eye became increasingly better defined. On 4 April, Inigo attained Category 5 status on the Australian cyclone scale, and at 0600 UTC, Inigo reached peak winds of {{convert|240|km/h|mph|abbr=on}} and an estimated minimum pressure of 900 hPa (mbar), while located about {{convert|950|km|mi|abbr=on}} north of Onslow, Western Australia. Around the same time, the JTWC assessed Inigo as a powerful cyclone with 1-min winds of {{convert|260|km/h|mph|abbr=on}}. With a minimum pressure of 900 hPa, Inigo tied Cyclone Gwenda of the 1998–99 season as the most intense tropical cyclone on record in the Australian cyclone region.{{Cite FTP |author=Bureau of Meteorology|year=2006|title=Australian Region Best Track 1907–2006|access-date=4 November 2007|format=Zip|server=FTP server|url-status=dead|url=ftp://ftp.bom.gov.au/anon2/home/ncc/cyclone/cyclones_newformat.zip}}

Upon reaching peak intensity, Inigo maintained an eyewall {{convert|32|km|mi|abbr=on}} in diameter. Late on 4 April, an approaching upper-level trough increased wind shear over the system, which caused a steady weakening trend. On 5 April, the eye became cloud-filled, and later that day the cyclone reached its westernmost point before the approaching trough turned it to the southeast. By 7 April, its winds decreased to below severe tropical cyclone status, or below {{convert|120|km/h|mph|abbr=on}}. The convection continued to decrease, leaving the centre exposed from the convection as it made landfall early on 8 April, in the Pilbara region of Western Australia. Upon moving ashore, Inigo had winds of around {{convert|75|km/h|mph|abbr=on}}. Inigo's circulation dissipated within 12 hours after moving ashore.

{{Most intense Australian cyclones|align=left}}

Image:Inigo 07 apr 2003 0610Z.jpg

The precursor tropical disturbance dropped heavy rainfall in eastern Indonesia; on the island of Flores, Larantuka recorded {{convert|223|mm|in|abbr=on}} in a 24-hour period. The rainfall caused flash flooding and mudslides, primarily in Flores but also on West Timor{{cite web|author=United Nations Office for the Coordination of Humanitarian Affairs|date=3 April 2003|title=Indonesia – Landslides OCHA Situation Report No. 1|publisher=ReliefWeb|access-date=6 January 2008|url=http://www.reliefweb.int/rw/rwb.nsf/db900sid/ACOS-64CUJB?OpenDocument&rc=3&emid=SL-2003-0155-IDN}} and Sumba. In some locations, the depth of the floodwaters reached {{convert|5|m|ft|abbr=off|sp=us}}. The Oessao River in West Timor exceeded its banks, which flooded seven villages. In Kupang in West Timor, the system destroyed hundreds of homes and large fields of corn, bean, and rice crop. Heavy damage was reported near Ende, where flooding and mudslides destroyed 20 houses and destroyed the roads connecting to East Flores. In Ende, a total of 294 animals were killed.{{cite web|author=United Nations Office for the Coordination of Humanitarian Affairs|date=4 November 2003|title=Indonesia: OCHA Consolidated Situation Report No. 123|publisher=ReliefWeb|access-date=8 January 2008|url=http://www.reliefweb.int/rw/rwb.nsf/db900sid/ACOS-64D9XQ?OpenDocument&rc=3&emid=SL-2003-0155-IDN}} The city's airport was flooded with {{convert|1|m|ft|abbr=off|sp=us|spell=in}} of water, preventing aerial transportation and leaving the city temporarily isolated. In East Flores Regency in eastern Flores Island, the system left 75 destroyed houses, along with 77 severely damaged and a further 56 receiving light damage. Damage in Indonesia totalled less than $6 million (2003 USD, $6.8 million 2007 USD), and 102 injuries were reported. The Indonesian representative to the Tropical Cyclone Committee of the World Meteorological Organization in 2004 reported the death toll related to the disaster in Indonesia as 58 fatalities.

Additionally, the precursor disturbance produced rough seas along the coastlines, which resulting in the sinking of 12 sailing vessels.{{cite web|author=RA V Tropical Cyclone Committee for the South Pacific and South-East Indian Ocean|year=2004|title=Final Report for the Tenth Tropical Cyclone Committee Session|publisher=World Meteorological Organization|page=7|format=PDF|access-date=6 January 2008|url=http://www.wmo.ch/pages/prog/www/TCP_vO/Reports/RA5_TCC10.pdf}}{{dead link|date=August 2017 |bot=InternetArchiveBot |fix-attempted=yes }} Two ships, each with a crew of five to eight people, were reported missing to the southwest of Sumba, after Cyclone Inigo passed over their location on 3 April.

Inigo moved ashore on Australia as a weak tropical cyclone, though several locations reported winds near gale force. The storm dropped light to moderate precipitation near its landfall location, with a maximum rainfall total of {{convert|226|mm|in|abbr=on}}, of which {{convert|128|mm|in|abbr=on}} of rain fell in 80 minutes.{{cite web|author=Bureau of Meteorology|year=2003|title=Significant Weather – April 2003|publisher=Government of Australia|access-date=6 January 2008|url=http://www.bom.gov.au/inside/services_policy/public/sigwxsum/sigw0403.shtml}} No casualties or significant damage was reported in the country.

Shortly after the storm passed through Indonesia, local government and Red Cross officials distributed assistance to the storm victims, including food, medicine, clean water, and mattresses; additionally, the government sent about Rp400 million (2003 IDR, $50,000 2003 USD). The affected citizens resided in temporary shelters, including schools, police offices, and shelters built by local governments. Officials deployed machines to remove debris from the roads affected by the landslides.

As a result of its damage, the name Inigo was retired and will not be used for another tropical cyclone in the region. Its name was replaced with Iggy, which was first used in 2012.{{cite web|author=World Meteorological Organization Tropical Cyclone Programme|year=2006|title=Tropical Cyclone Operational Plan for South Pacific and Southeast Indian Ocean|access-date=8 January 2008|url=http://www.wmo.ch/pages/prog/www/tcp/documents/TCP-24OP-PLN2006edition-english.pdf|archive-url=https://web.archive.org/web/20120717054641/http://www.wmo.int/pages/prog/www/tcp/documents/TCP-24OP-PLN2006edition-english.pdf|archive-date=17 July 2012|url-status=dead}}

{{Portal|Tropical cyclones}}

• Cyclone Mahina – The most intense tropical cyclone ever recorded in the Southern Hemisphere
• Geography of Indonesia

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{{Commons category|Cyclone Inigo}}

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Inigo (2003)

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Inigo