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Cyclone Heta

South Pacific cyclone in 2003 and 2004

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The damage Heta caused on Tonga, Niue, and American Samoa was estimated at $150 million (2004 USD), with most of the damage occurring in American Samoa; the cyclone was also responsible for one death. Heta precipitated a massive relief and clean-up operation that lasted throughout 2004.

Meteorological history

During December 25, 2003 the Fiji Meteorological Service reported that Tropical Disturbance 03F had developed underneath the subtropical ridge of high pressure about halfway between Fiji and Rotuma. At this time, the disturbance was poorly organised with atmospheric convection surrounding the system displaced by about a degree to the north and east of its low-level circulation centre. Over the next few days, the system gradually developed further and was classified as a tropical depression by the FMS during December 28, as it slowly moved eastwards to the north of Fiji. During the next day, as the depression passed about 40 km (25 mi) to the northeast of Futuna, the system started to move north-eastwards towards Tokelau.

The depression migrated first northward and then eastward until January 2, 2004, when it reached tropical storm strength and was named Heta. At this point, low wind shear and high sea surface temperatures caused Heta to intensify rapidly. On January 3, Heta, aided by a weak steering current, slowly began to move to the southeast as it became a Category 1 hurricane.

The center of Heta passed 70 miles (110 km) west of Samoa as the storm reached Category 2 status. Heta reached a peak intensity of 260 km/h (160 mph) at midnight UTC on January 5, and maintained it for 24 hours as it continued its south-southeastward track. Heta passed close to the island of Niue at 03:00 UTC January 6 as it began slowly weakening. By January 7, Cyclone Heta had exited the Nadi RMSC's area of responsibility and entered that of the Tropical Cyclone Warning Center at Wellington, New Zealand. The storm slowly weakened as it encountered the cooler waters of the far South Pacific. Heta became extratropical 845 km (525 mi) south of the island of Rarotonga later on the 7th. These remnants of Heta slowed even further and moved westward, where they finally dissipated on January 11 east of Norfolk Island.

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