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1984–85 South Pacific Cyclone Season
The 1984–85 South Pacific cyclone season was an above-average tropical cyclone season, with nine tropical cyclones occurring within the basin between 160°E and 120°W. The season ran from November 1, 1984, to April 30, 1985, with tropical cyclones officially monitored by the Fiji Meteorological Service (FMS), Australian Bureau of Meteorology (BoM) and New Zealand's MetService. The United States Joint Typhoon Warning Center (JTWC) and other national meteorological services including Météo-France and NOAA also monitored the basin during the season. During the season there was nine tropical cyclones occurring within the basin, including three that moved into the basin from the Australian region. The BoM, MetService and RSMC Nadi all estimated sustained wind speeds over a period of 10-minutes, which are subsequently compared to the Australian tropical cyclone intensity scale, while the JTWC estimated sustained winds over a 1-minute period, which are subsequently compared to the Sa ...
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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 Tropical cyclone basin#South Pacific, South Pacific basin between 160th meridian east, 160°E and 120th meridian west, 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 ...
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Viti Levu
Viti Levu (pronounced ; ) is the largest island in Fiji. It is the site of the country's capital and largest city, Suva, and home to a large majority of Fiji's population. Geology Fiji lies in a plate tectonics, tectonically complex area between the Australian plate and the Pacific plate. The Fiji Platform lies in a zone bordered by active extension fault lines, around which most of the shallow earthquakes in the area have been centred. These fault lines are: the Fiji Fracture Zone (FFZ) to the north; the Spreading ridge, 176° Extension Zone (176°E EZ) to the west; and the Hunter fracture zone (HFZ) and Lau-Colville Ridge, Lau Ridge to the east. The oldest rocks on the island are those formed during the Eocene and Early Miocene epochs that belong to the Wainimala Group (geology), group. The lower portion of the group is made up of volcanic flows and volcaniclastics, which grade from basalt to trachyte and rhyolite. Geographically, this group is found south of Nadi, including ...
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New Zealand
New Zealand () is an island country in the southwestern Pacific Ocean. It consists of two main landmasses—the North Island () and the South Island ()—and List of islands of New Zealand, over 600 smaller islands. It is the List of island countries, sixth-largest island country by area and lies east of Australia across the Tasman Sea and south of the islands of New Caledonia, Fiji, and Tonga. The Geography of New Zealand, country's varied topography and sharp mountain peaks, including the Southern Alps (), owe much to tectonic uplift and volcanic eruptions. Capital of New Zealand, New Zealand's capital city is Wellington, and its most populous city is Auckland. The islands of New Zealand were the last large habitable land to be settled by humans. Between about 1280 and 1350, Polynesians began to settle in the islands and subsequently developed a distinctive Māori culture. In 1642, the Dutch explorer Abel Tasman became the first European to sight and record New Zealand. ...
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Wellington
Wellington is the capital city of New Zealand. It is located at the south-western tip of the North Island, between Cook Strait and the Remutaka Range. Wellington is the third-largest city in New Zealand (second largest in the North Island), and is the administrative centre of the Wellington Region. It is the world's southernmost capital of a sovereign state. Wellington features a temperate maritime climate, and is the world's windiest city by average wind speed. Māori oral tradition tells that Kupe discovered and explored the region in about the 10th century. The area was initially settled by Māori iwi such as Rangitāne and Muaūpoko. The disruptions of the Musket Wars led to them being overwhelmed by northern iwi such as Te Āti Awa by the early 19th century. Wellington's current form was originally designed by Captain William Mein Smith, the first Surveyor General for Edward Wakefield's New Zealand Company, in 1840. Smith's plan included a series of inter ...
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New Zealand Meteorological Service
Meteorological Service of New Zealand Limited, or simply MetService (), is the national meteorological service of New Zealand. MetService was established as a State-owned enterprises of New Zealand, state-owned enterprise in 1992. It employs about 300 staff, and its headquarters are in Wellington, New Zealand. Prior to becoming a state-owned enterprise, New Zealand's national meteorological service has existed in a number of forms since the appointment of the country's first Director of Meteorological Stations in August 1861. As New Zealand's national meteorological service, MetService produces and issues forecasts and official weather warnings on behalf of New Zealand's New Zealand Ministry of Transport, Ministry of Transport and is certified by the Civil Aviation Authority of New Zealand. International media, aviation and energy business is conducted under the ''MetraWeather'' brand. MetService has been certified to the ISO 9000, ISO 9001 standard since November 1995. From ...
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List Of Category 2 South Pacific Tropical Cyclones
Category 2 the fourth-highest classification on the Australian tropical cyclone intensity scale is used to classify tropical cyclones, that have 10-minute sustained winds of . 71 tropical cyclones have peaked as a category 2 tropical cyclone in the South Pacific tropical cyclone basin, which is denoted as the part of the Pacific Ocean to the south of the equator and to the east of 160°E. This list does not include any tropical cyclones that went on to peak as a Category 3, 4 or 5 severe tropical cyclones, while in the Southern Pacific tropical cyclone basin. Background The South Pacific tropical cyclone, South Pacific tropical cyclone basin is located to the south of the Equator between 160°E and 120°W. The basin is officially monitored by the Fiji Meteorological Service and the New Zealand MetService, while other meteorological services such as the Australian Bureau of Meteorology, Météo-France as well as the United States Joint Typhoon Warning Center also monitor the basi ...
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List Of Category 1 South Pacific Tropical Cyclones
Category 1 is the lowest classification on the Australian tropical cyclone intensity scale and is used to classify tropical cyclones, that have 10-minute sustained winds of . tropical cyclones have peaked as Category 1 tropical cyclones in the South Pacific tropical cyclone basin, which is denoted as the part of the Pacific Ocean to the south of the equator and to the east of 160°E. This list does include any tropical cyclones that went on to peak as a Category 4 or 5 severe tropical cyclone, while in the Southern Pacific tropical cyclone basin. Background The South Pacific tropical cyclone basin is located to the south of the Equator between 160°E and 120°W. The basin is officially monitored by the Fiji Meteorological Service and the New Zealand MetService, while other meteorological services such as the Australian Bureau of Meteorology, Météo-France as well as the United States Joint Typhoon Warning Center also monitor the basin. Within the basin a Category 3 severe tr ...
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Tanna (island)
Tanna (sometimes misspelled ''Tana'') is an island in southern Vanuatu. Tanna is the most populous island of Tafea Province, and the third most populous in the country (after Efate and Espiritu Santo). It is home to five indigenous languages, which also rank among the most widely spoken in the whole archipelago, ranging from 3,500 to 11,500 speakers. Tanna has been featured in numerous documentaries and TV shows around the world. This is partly due to Mount Yasur, an active volcano and a major tourist attraction. It is also of interest for its vibrant Melanesian culture, through dances and festivals. The island has attracted the attention of many anthropologists for its cargo cults. Name The name ''Tanna'', first cited by James Cook, is derived from the word ''tana'' in the Kwamera language, meaning 'earth'. Etymologically, ''Tanna'' goes back to Proto-Oceanic *''tanoq'', from Proto-Malayo-Polynesian * ''taneq'', with the same meaning. Geography Tanna is long and wide, w ...
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Aneityum
Aneityum (also known as Anatom or Keamu) is the southernmost island of Vanuatu, in the province of Tafea. Geography Aneityum is the southernmost island of Vanuatu (not counting the Matthew and Hunter Islands, which are disputed with New Caledonia, but considered by the people of Aneityum Island part of their custom ownership). Its southeastern cape Nétchan Néganneaing is the southernmost point of land in Vanuatu, more southerly than the southern satellite islet Inyeug. The latter, however, is surrounded by Intao Reef, that extends even further south, albeit submerged, thus being the southernmost feature of Vanuatu. The island is in size. It rises to an elevation of in Mount Inrerow Atamein. The larger of its two villages is Anelcauhat ( Anelghowhat), on the south side. Population Aneityum had a population of 915 in 2009. This population is believed to have been between 9,000 and 20,000 prior to the arrival of the Europeans, in 1793. However, introduced diseases and bl ...
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Rotuma
Rotuma () is a self-governing heptarchy, generally designated a Local government in Fiji, dependency of Fiji. Rotuma commonly refers to the Rotuma Island, the only permanently inhabited and by far the largest of all the islands in the Rotuma Group. Officially, the Rotuma Act declares that Rotuma consists of Rotuma Island as well as its neighbouring islands, rocks, and reefs across the entire Rotuma Group. The dependency is situated around 500 km west of the French islands of Wallis and Futuna and a similar distance north of the Fijian mainland. Its capital is Ahau, a hamlet consisting of a number of Colony of Fiji, colonial-era buildings. Rotuma exists as a dependency of Fiji but itself contains its own socioreligious enclave, pene-enclave known traditionally as ''Faguta'' where the chiefs (of Juju (district), Juju and Pepjei) and their villages adhere to the practices of worship, Fara (Rotuman festivity), festival dates, and French language, French-based writing system of th ...
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Monsoon Trough
The monsoon trough is a convergence zone between the wind patterns of the southern and northern hemispheres. It is a portion of the Intertropical Convergence Zone in the Western Pacific,Bin WangThe Asian Monsoon.Retrieved 2008-05-03. and is depicted by a line on a weather map showing the locations of minimum sea level pressure. Westerly monsoon winds lie in its equatorward portion while easterly trade winds exist poleward of the trough. Right along its axis, heavy rains can be found which usher in the peak of a location's respective rainy season. The monsoon trough plays a role in creating many of the world's rainforests. The term ''monsoon trough'' is most commonly used in monsoonal regions of the Western Pacific such as Asia and Australia. The migration of the ITCZ/monsoon trough into a landmass heralds the beginning of the annual rainy season during summer months. Depressions and tropical cyclones often form in the vicinity of the monsoon trough, with each capable of produc ...
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Fiji Meteorological Service
The Fiji Meteorological Service (FMS) is a Department of the government of Fiji responsible for providing weather forecasts and is based on the grounds of Nadi Airport in Nadi. The current director of Fiji Meteorological Service is Misaeli Funaki. Since 1985, FMS has been responsible for naming and tracking tropical cyclones in the Southwest Pacific region. Current Meteorologists working at FMS have a Graduate Diploma in Meteorology from the Australian Bureau of Meteorology. History Before World War II, weather observations in Fiji were the responsibility of the harbour board and limited to recording various meteorological details at various locations around the island nation. During the 1939 Defence Conference in Wellington, New Zealand, Fiji's capital Suva was identified as the location of an upgraded meteorological service for the Pacific region. As a result, a facility was established at Laucala Bay during 1940, before it was expanded during the following year to support the ...
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