Lably
Skip to content

Cyclone Ita

Category 5 Australian region cyclone in 2014

  • 10 min read
  • 3 chapters
Severe Tropical Cyclone Ita on April 10, 2014
NASA · Public domain

Related on Lably

Through Pascal (unit) and Gross domestic product

Owing to the rapid degradation of the cyclone before landfall, structural damage was relatively low at A$8.4 million (US$7.9 million). However, the agricultural industry suffered extensive impacts and total losses reached A$1.1 billion (US$1 billion).

Meteorological history

On 1 April 2014, a broad, poorly defined area of low pressure consolidated over the Solomon Islands. Initially only accompanied by flaring convection, the system persisted in a region of low wind shear and strong outflow which promoted gradual development. Upon formation, the Bureau of Meteorology (BoM) office in Brisbane monitored the system as a tropical low. Banding features gradually developed and wrapped around the circulation and deep convection became persistent by 2 April. A large central dense overcast developed over the low early on 3 April, prompting the Joint Typhoon Warning Center (JTWC) to issue a Tropical Cyclone Formation Alert.

After moving away from Papua New Guinea, Ita underwent explosive intensification and attained its peak intensity as a Category 5 severe tropical cyclone early on 11 April. Winds were estimated to have reached 220 km/h (140 mph) alongside a minimum central pressure of 922 mbar (hPa; 27.23 inHg). Turning to the south-southeast, the storm weakened somewhat before making landfall near Cape Flattery as a Category 4 later on 11 April. An automated weather station on Lizard Island, roughly 5 km (3.1 mi) from the storm's centre, recorded a pressure of 954 mbar (hPa; 28.17 inHg). Once onshore Ita weakened dramatically to a Category 1 within 18 hours. Maintaining gale-force winds the storm turned southwest and accelerated, eventually moving offshore north of Mackay on 13 April. The following day Ita transitioned into an extratropical cyclone as it moved away from Australia and towards New Zealand. Ita's extratropical remnants combined with a low pressure system to the south and re-intensified. On 17 April, the low-level circulation center of the storm collapsed, as Ita affected New Zealand, bringing heavy rainfall and powerful winds. On 18 April, Ita's remnants curved to the west and the south, before dissipating offshore of New Zealand later on the same day.

Sign in to keep reading

2 more chapters are free with a Lably account.

More in Earth science