The population of Tuvalu is approximately 10,645 people (2017 Mini Census), but there are estimated to be more than 13,000 Tuvaluan speakers worldwide. In 2015 it was estimated that more than 3,500 Tuvaluans live in New Zealand, with about half that number born in New Zealand and 65 percent of the Tuvaluan community in New Zealand is able to speak Tuvaluan. (Full article...)
For 2010, the total health budget was AUD $4,696,042. (Full article...)
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Satellite picture
Niulakita is the southernmost island of Tuvalu, and also the name of the only village on this island. Niulakita has a population of 34 (2017 Census). The residents of Niulakita have moved to the island from Niutao. Niulakita is represented in the Parliament of Tuvalu by the members of the constituency of Niutao. (Full article...)
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Crime in Tuvalu is not a significant social problem due to small population, geographic isolation, and low development.
The coral reefs of Tuvalu consist of three reef islands and six atolls, containing approximately 710 km2 (270 sq mi) of reef platforms. The islands of the Tuvalu archipelago are spread out between the latitude of 5° to 10° south and longitude of 176° to 180°, west of the International Date Line. The islands of Tuvalu are volcanic in origin. On the atolls, an annular reef rim surrounds the lagoon, and may include natural reef channels. The reef islands have a different structure to the atolls, and are described as reef platforms as they are smaller tabular reef platforms that do not have a salt-water lagoon, although they may have a completely closed rim of dry land, with the remnants of a lagoon that has no direct connection to the open sea or that may be drying up. (Full article...)
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Climate change is particularly threatening for the long-term habitability of the island country of Tuvalu, which has a land area of only 26 square kilometres (10 sq mi) and an average elevation of less than 2 metres (6.6 ft) above sea level, with the highest point of Niulakita being about 4.6 metres (15 ft) above sea level. Potential threats to the country due to climate change include rising sea levels, increasingly severe tropical cyclones, high temperatures, and drought. King tides (Perigean spring tide) can combine with storm surges and the rising sea level to inundate the low lying atolls.
Tuvalu is widely considered one of the first countries likely to be significantly impacted by rising sea levels due to global climate change. According to some estimates, the highest tides could regularly flood 50% of the land area of national capital Funafuti by the mid-21st century, and 95% by 2100. The rising saltwater table could also destroy deep rooted food crops such as coconut, pulaka, and taro before they're overtaken by actual flooding. Meanwhile, one 2018 study from the University of Auckland suggested that Tuvalu may remain habitable over the next century, finding that the country's islands have even grown in area overall in recent decades, though the authors stressed that "Climate change remains one of the single greatest environmental threats to the livelihood and well-being of the peoples of the Pacific" and that "Sea-level rise and climatic change threaten the existence of atoll nations". (Full article...)
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Tuvalu consists of nine separate islands: six atolls and three reef islands. An atoll typically consists of several motus: Tuvalu has a total of 124 islands and islets. Each island is surrounded by a coral reef. The soils of Tuvalu's islands are usually shallow, porous, alkaline, coarse-textured, with carbonate mineralogy and high pH values of up to 8.2 to 8.9. The soils are usually deficient in most of the important nutrients needed for plant growth, so garden beds need to be enhanced with mulch to increase their fertility. Tuvalu's small, widely scattered atolls have a total land area of only about 26 square kilometres (10 square miles) making Tuvalu the fourth-smallest country in the world.
The sea level at the Funafuti tide gauge has been rising at a rate of 3.9 mm per year, and it has been determined that rising sea levels are causing more wave energy to be transferred across reef surfaces, which has tended to push more sand onto island shorelines, increasing islands’ land area. Over a recent four-decade period, there was a net increase in the land area of the islets of 2.9% (73.5 ha), although the changes were not uniform: About 74% of them increased in size and about 27% decreased in size. (Full article...)
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Cyclone Raja on 28 December
Severe Tropical Cyclone Raja was a tropical cyclone that holds the 24-hour rainfall record of 674.9 mm (26.57 in) for the French Overseas Territory of Wallis and Futuna. The system was first noted by the Fiji Meteorological Service (FMS) as a weak tropical disturbance northeast of Tokelau in mid-December 1986. The system developed further as it moved southwest over the next few days, and it was classified as Tropical Cyclone Raja on 23 December. The newly named system slowed and unexpectedly recurved southeast towards the French territory of Wallis and Futuna on 24 December. Over the next two days, Raja interacted with what would become Severe Cyclone Sally and executed a tight loop, passing within 55 km (35 mi) of Futuna. The system peaked as a Category 3 severe tropical cyclone on 28 December, with estimated 10-minute sustained winds of 90 mph (150 km/h). The storm turned southwest the next day and threatened Fiji, where it passed within 20 km (10 mi) of Vanua Levu and near (or over) several smaller islands in the Lau group during the following day. Raja gradually weakened over the next few days as it moved south of Fiji; it was last noted on 5 January 1987 after it filled up over the north Tasman Sea.
Raja caused one death as it impacted the island nations of Tuvalu, Wallis and Futuna, Tonga and Fiji. Gusty winds and rough seas associated with the system caused extensive damage to crops, coastal installations and buildings in Tuvalu, and flooded low-lying areas. The island of Futuna was the worst hit, with crops, coastal installations and buildings damaged or destroyed by the system. Raja affected the main islands of Fiji twice between 24 and 30 December, and was responsible for the worst flood of the Labasa River since 1929. As a result of the damage to Fiji and portions of Polynesia, the name Raja was retired from the South Pacific naming lists. (Full article...)
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Maatia ToafaOBE (born 1 May 1954) is a Tuvaluan politician, representing Nanumea, who served two non-consecutive terms as Prime Minister of Tuvalu. He first served as prime minister, and foreign minister, from 2004 to 2006, from the resignation of his predecessor, Saufatu Sopoanga, until the defeat of his Cabinet in the 2006 general election. From 2004 to 2006 he also held the role of foreign minister.
The 2011 Tuvalu drought was a period of severe drought afflicting Tuvalu, a South Pacific island country of approximately 10,500 people, in the latter half of 2011. A state of emergency was declared on September 28, 2011; with rationing of available fresh-water. The La Niña event that caused the drought ended in April–May 2012. By August 2012 the El Niño-Southern Oscillation (ENSO) Conditions indicated that the tropical Pacific Ocean was on the brink of an El Niño event. (Full article...)
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The Law of Tuvalu comprises the legislation voted into law by the Parliament of Tuvalu and statutory instruments that become law; certain Acts passed by the Parliament of the United Kingdom (during the time Tuvalu was either a British protectorate or British colony); the common law; and customary law (particularly in relation to the ownership of land). The land tenure system is largely based on kaitasi (extended family ownership). (Full article...)
Motufoua Secondary School is a boarding school for children on Vaitupu atoll, Tuvalu. As of 2000[update] it is the largest high school in Tuvalu. As Tuvalu consists of nine islands, the students reside on Vaitupu during the school year and return to their home islands during the school vacations.
The school received worldwide attention in March 2000, when a fire in a dormitory at the school killed 19 girls and an adult supervisor. It was later discovered that the fire was caused by a student using a candle to read during the night. The school celebrated 100 years of education in 2005. (Full article...)
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Fred Whibley, Island trader on Niutao 1898 to 1909 (Fred Whibley c.1888)
Fredrick George Whibley (1855–1919) abandoned a career as clerk in a London bank to escape from the constraints and social expectations of respectability in the Victorian era. He ended up as a copra trader on Niutao in the Ellice Islands in the central Pacific Ocean.
Nui is an atoll and one of nine districts of the Pacific Ocean state of Tuvalu. It has a land area of 3.37 km2 and a population of 610 (2017 Census).
Traditionally Nuian culture is organised in three family circles – Tekaubaonga, Tekaunimala and Tekaunibiti families. Most people live on the western end of Fenua Tapu. In the 2012 census, 321 people live in Alamoni – Maiaki and 221 people live in Manutalake – Meang (Tanrake). The junior school is Vaipuna Primary School. (Full article...)
Image 2Polynesia is the largest of three major cultural areas in the Pacific Ocean. Polynesia is generally defined as the islands within the Polynesian triangle. (from History of Tuvalu)
Image 201st Lt. Louis Zamperini, peers through a hole in his B-24D Liberator 'Super Man' made by a 20mm shell over Nauru, 20 April 1943. (from History of Tuvalu)
Image 28The atoll of Funafuti; borings into a coral reef and the results, being the report of the Coral Reef Committee of the Royal Society (1904). (from History of Tuvalu)
Image 29Interior of a maneapa on Funafuti, Tuvalu (from History of Tuvalu)