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1982–83 South Pacific cyclone season

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1982–83 South Pacific cyclone season

The 1982–83 South Pacific cyclone season was one of the most active and longest South Pacific tropical cyclone seasons on record, with 14 tropical cyclones occurring within the South Pacific basin between 160°E and 120°W. During the season tropical cyclones were monitored by the meteorological services of Australia, Fiji, French Polynesia and New Zealand. The United States Armed Forces through the Joint Typhoon Warning Center (JTWC) and Naval Pacific Meteorology and Oceanography Center (NPMOC), also monitored the basin and issued unofficial warnings for American interests. The first tropical cyclone of the season developed a day before the season officially began on October 30, while the last tropical cyclone of the season dissipated on May 16. Most of the activity during the season occurred within the far eastern parts of the basin with French Polynesia affected by an extremely high amount of storms.

The 1982–83 season was one of the most active and longest South Pacific tropical cyclone seasons on record, with fourteen tropical cyclones and nine severe tropical cyclones occurring within the South Pacific basin between 160°E and 120°W. During the season, tropical cyclones were primarily monitored by the Fiji Meteorological Service, which issued high seas and tropical cyclone warnings for the region between the Equator and 25°S, 160°E and 140°W. Tropical cyclones that moved below 25S were monitored by the New Zealand Meteorological Service (NZMS), while those that were located to the west of 160E were monitored by the Australian Bureau of Meteorology as a part of the Australian region. During the season, several tropical cyclones formed to the east of the International Dateline and out towards 120°W, which caused significant problems for the FMS, as the eastern edge of its satellite coverage was restricted to around 155°W. As a result, the FMS were dependent on data from other weather services including the United States Joint Typhoon Warning Centre, the Naval Western Oceanographic Centre, Central Pacific Hurricane Center as well as the Tahiti Meteorological Services. The NZMS also had to take over Fiji's regional responsibilities for a few days, while Severe Tropical Cyclone Oscar impacted Fiji and caused a communications outage.

The season was characterised by a very strong El Niño event, which resulted in eleven tropical cyclones occurring to the east of the International Dateline. Five of these tropical cyclones went on to affect the island nation of French Polynesia, which it was thought had not been affected by a tropical cyclone since another very strong El Niño episode in 1905–06.

During the season, ten of the fourteen tropical cyclones observed to the east of 160 E were severe tropical cyclones, with 5 of them occurring in the French Polynesia region which represented one more than was experienced in the same area over the previous 13 seasons. Damage from the storms in French Polynesia was estimated at F16 billion (US$100 million).


The first tropical disturbance was first by Honolulu on October 30

The system that was to become Tropical Cyclone Joti was first noted by the Central Pacific Hurricane Center (CPHC) during October 30, while it was located about 1000 km (620 mi) to the north-east of Port Villa in Vanuatu. Over the next day, the disturbance gradually developed further, as its outflow increased and atmospheric convection surrounding the system organized. The disturbance was subsequently named Joti at 00:00 UTC on November 1, by the FMS as it had developed into a tropical cyclone. As a result, this made Joti one of the earliest tropical cyclones ever recorded within the basin. After it was named, Joti continued to develop as it completed a cyclonic loop, before it started to move south-westwards towards Vanuatu during November 2.

During November 3, the FMS reported that Joti had peaked with 10-minute sustained winds of 110 km/h (70 mph), which made it a Category 2 tropical cyclone on the Australian scale. The JTWC subsequently reported that the system had peaked with 1-minute sustained winds of 120 km/h (75 mph), which made it equivalent to a Category 1 hurricane on the SSHWS. During that day the system started to move towards the west-south-west and made landfall on the northern Espiritu Santo. After the system had moved into the Coral Sea, it gradually weakened and turned towards the south-southwest, before it degenerated into a depression during November 7. Within northern Vanuatu, Joti damaged houses, gardens and fruit trees.

The system that was to become Tropical Cyclone Kina was first noted on November 6, while it was located just to the east of Tuvalu. Over the next few days the system moved south-westwards and gradually developed further, before the JTWC reported that the system had developed into a tropical cyclone, with peak 1-minute sustained winds of 75 km/h (45 mph) during November 10. During that day the FMS also reported that the system had developed into a Category 1 tropical cyclone on the Australian Scale and named it Kina. The FMS subsequently estimated during the next day that the system had reached its peak intensity, with 10-minute sustained winds of 75 km/h (45 mph) during November 11. Later that day the system's upper-level circulation became sheared off from its lower and moved southwards away from it. The degenerating system subsequently passed to the west of Fiji during November 13, before it was last noted during November 16, as it passed over the island of Efate in Vanuatu but no damage was reported. The system caused strong winds and rough seas on Viti Levu and in the Yasawas and Mamanutha group of islands. Tourists on the Blue Lagoon Cruise in the Yasawas were forced to take shelter from Kina, while 18 people on another boat were temporarily listed as missing as they took shelter.

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