Meteorological history | |
---|---|
Formed | 30 March 2003 |
Dissipated | 8 April 2003 |
Category 5 severe tropical cyclone | |
10-minute sustained (BOM) | |
Highest winds | 230 km/h (145 mph) |
Lowest pressure | 900 hPa (mbar); 26.58 inHg (Record low in Australian region; tied with Gwenda) |
Category 5-equivalent tropical cyclone | |
1-minute sustained (SSHWS/JTWC) | |
Highest winds | 260 km/h (160 mph) |
Lowest pressure | 898 hPa (mbar); 26.52 inHg |
Overall effects | |
Fatalities | 58 direct |
Damage | ~$6 million (2003 USD) |
Areas affected | |
IBTrACS | |
Part of the 2002–03 Australian region cyclone season |
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.[1] 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.
The precursor disturbance dropped heavy rainfall across eastern Indonesia, causing widespread flooding and mudslides. The worst of the damage was on Flores island, though damage was also reported on West Timor and Sumba. The flooding and mudslides damaged or destroyed thousands of houses, forcing many to leave their homes. A total of 58 casualties were reported in association with Inigo, as a disturbance. In Australia, Inigo produced locally heavy rainfall, but did little damage.