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Cyclone Inigo

Severe Tropical Cyclone Inigo is tied with Cyclone Gwenda for being the most intense recorded cyclone in the Australian region in terms of pressure, with the possible exception of Cyclone Mahina. Inigo developed from a tropical low that crossed eastern Indonesia in late March 2003. Becoming a named tropical cyclone on 1 April, Inigo rapidly intensified as it tracked southwestward, reaching a minimum central pressure of 900 hPa on 4 April with maximum 1 minute sustained winds of 170 mph. An approaching trough weakened the cyclone and turned it to the southeast, and on 8 April, Inigo dissipated after making landfall on Western Australia, as a minimal tropical storm.

Meteorological history
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. 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. The storm quickly intensified as it tracked southwestward, aided by low wind shear and strong divergence. An eye featured gradually organised, Upon reaching peak intensity, Inigo maintained an eyewall 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 . 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 . Inigo's circulation dissipated within 12 hours after moving ashore. ==Impact==
Impact
The precursor tropical disturbance dropped heavy rainfall in eastern Indonesia; and Sumba. The city's airport was flooded with 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. 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. No casualties or significant damage was reported in the country. ==Aftermath==
Aftermath
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. ==See also==
Source: Wikipedia ↗
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