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Cyclone Hina

Category 3 South Pacific severe tropical cyclone in 1997

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Through Hectare

Within Tuvalu, it was difficult to assess damage done by Hina alone, after Cyclone Gavin impacted the area a week earlier. Storm surge and strong winds from both cyclones caused a severe amount of coastal erosion on all of the country’s nine atolls, with about 6.7% of land washed into the sea. Hina caused no significant damage on Walls Island, while it caused some damage to crops and destroyed parts of the road on Futuna Island. In Tonga, there were no casualties reported while the system was affecting the island nation, however, Vaiola Hospital reported that they had treated a number of patients for injuries that were caused during the system's aftermath. One indirect death was also reported, after a person suffered a heart attack while evacuating from his home. The cyclone left extensive damage to utilities and agriculture on Tongatapu, where trees were uprooted and more than 12,000 tonnes (26,000,000 lb) of fruit and food crops were destroyed, mostly to banana and coconut trees. After the cyclone, the Tongan Government requested and received emergency aid from the governments of several countries including France, Australia, New Zealand, Japan and the United Kingdom. This was after the government had provided T$5 million (US$3.97 million), or about 5% of its national budget to facilitate the immediate start of emergency relief and repairs to essential services.

Meteorological history

During March 11, 1997, a shallow tropical depression developed within the monsoon trough near the Fijian Dependency of Rotuma. Over the next two days the depression remained near Rotuma with little to no movement, as it started to develop further in an area of minimal vertical wind shear and good upper air divergence. During March 13, as the system moved northwards, the United States Joint Typhoon Warning Center (JTWC) subsequently initiated advisories on the system and designated it as Tropical Cyclone 33P. During that day after having moved to the north, Hina curved to the east and later south-eastwards, before it passed about 55 km (35 mi) to the southeast of Niulakita the southernmost island of Tuvalu during March 14. Early on March 15, after the system had passed near Niulakita, the depression developed into a category 1 tropical cyclone on the Australian tropical cyclone intensity scale and was named Hina by the Fiji Meteorological Service (FMS). After being named the system accelerated towards the south-southeast and an area of increasing vertical wind shear, as it passed near the west coast of Futuna Island. The system also crossed the 180th meridian during that day, which prompted the JTWC to pass the responsibility for warning the United States Government to the Naval Pacific Meteorology and Oceanography Center (NPMOC).

Early on March 16, as Hina passed over the southern islands of Tonga, the FMS reported that based on satellite imagery and guidance from other meteorological centers, the system had 10-minute sustained wind speeds of 85 km/h (55 mph). Hina subsequently passed over the islands of Tongatapu and ʻEua in southern Tonga at around 08:30 UTC and took less than 2 hours to inflict considerable damage on the islands. The system subsequently emerged back into the South Pacific Ocean, with the FMS estimating that the system had storm-force winds of about 95 km/h (60 mph). Later that day the NPMOC estimated that Hina had peak 1-minute sustained wind speeds of 110 km/h (70 mph) as it rapidly moved below 25°S and out of the FMS's area of responsibility. Over the next few days the system continued to move towards the south-southeast and gradually weakened, before the NPMOC issued its final advisory during March 18, as the system was undergoing a transition to become an extratropical cyclone. The system weakened below tropical cyclone intensity during the next day, before it was last noted by MetService on March 21, while it was located about 1,500 km (930 mi) to the south of the Pitcairn Islands.

After an analysis of the observed data and the damage in Tonga, the FMS found that Hina's landfall intensity had been underestimated. The observed wind data suggested that the system had storm-force sustained winds, but had peak gusts comparable to hurricane force. Furthermore, the lowest pressure values indicated that the winds had to be stronger than estimated, for it to fit known wind-pressure relationships. The FMS subsequently deduced that Hina was a minimal category 3 severe tropical cyclone, with peak 10-minute sustained wind speeds of 120 km/h (75 mph) when it passed near or over Tongatapu at around 08:30 UTC (21:30 UTC+13). The NPMOC also revised their estimate of Hina's peak 1-minute sustained wind speeds from 110 km/h (70 mph) to 140 km/h (85 mph) during post-analysis, which made the system equivalent to a category 1 hurricane on the Saffir–Simpson hurricane wind scale.

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