1987–88 South Pacific Cyclone Season
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1987–88 South Pacific Cyclone Season
The 1987–88 South Pacific cyclone season was a quiet tropical cyclone season with five tropical cyclones and 3 severe tropical cyclones, observed within the South Pacific basin to the east of 160°E. __TOC__ Seasonal summary ImageSize = width:825 height:195 PlotArea = top:10 bottom:80 right:20 left:20 Legend = columns:3 left:30 top:58 columnwidth:270 AlignBars = early DateFormat = dd/mm/yyyy Period = from:01/12/1987 till:01/05/1988 TimeAxis = orientation:horizontal ScaleMinor = grid:black unit:month increment:1 start:01/12/1987 Colors = id:canvas value:gray(0.88) id:GP value:red id:TDi value:rgb(0,0.52,0.84) legend:Tropical_Disturbance id:TD value:rgb(0.43,0.76,0.92) legend:Tropical_Depression id:C1 value:rgb(0.3,1,1) legend:Category_1_=_63-87_km/h_(39-54_mph) id:C2 value:rgb(0.75,1,0.75) legend:Category_2_=_88-142_km/h_(55-74_mph) id:C3 value:rgb(1,0.85,0.55) legend:Category_3_=_143-158-km/h_(75-98_mph) id:C4 valu ...
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1985–86 South Pacific Cyclone Season
The 1985–86 South Pacific cyclone season was an average tropical cyclone season, in terms of tropical cyclone formation, with ten tropical cyclones occurring within the basin between 160°E and 120°W. The season ran from February 5, 1985, to May 22, 1986, 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. __TOC__ Seasonal summary ImageSize = width:900 height:220 PlotArea = top:10 bottom:80 right:20 left:20 Legend = columns:3 left:30 top:58 columnwidth:270 AlignBars = early DateFormat = dd/mm/yyyy Period = from:01/02/1986 till:01/06/1986 TimeAxis = orien ...
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1987–88 Australian Region Cyclone Season
The 1987–88 Australian region cyclone season was the one of least active Australian region tropical cyclone seasons on record. It officially started on 1 November 1987, and officially ended on 30 April 1988. The regional tropical cyclone operational plan defines a "tropical cyclone year" separately from a "tropical cyclone season"; the "tropical cyclone year" began on 1 July 1987 and ended on 30 June 1988. Seasonal summary ImageSize = width:800 height:195 PlotArea = top:10 bottom:80 right:20 left:20 Legend = columns:3 left:30 top:58 columnwidth:270 AlignBars = early DateFormat = dd/mm/yyyy Period = from:01/12/1987 till:31/05/1988 TimeAxis = orientation:horizontal ScaleMinor = grid:black unit:month increment:1 start:01/12/1987 Colors = id:canvas value:gray(0.88) id:GP value:red id:TL value:rgb(0.43,0.76,0.92) legend:Tropical_Low_=_<63_km/h_(<39_mph) id:C1 value:rgb(0.3,1,1) legend:Category_1_=_63–88_km/h_(39-55_mph) id:C2 value:rgb(0.75,1,0.7 ...
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Temotu Province
Temotu (or Te Motu, literally "the island" in Polynesian) is the easternmost province of Solomon Islands. The province was formerly known as Santa Cruz Islands Province. It consists, essentially, of two chains of islands which run parallel to each other from the northwest to the southeast. Its area is . Administrative divisions Temotu Province is sub-divided into the following wards: Temotu Province (pop 21,362) * Reef Islands ** Polynesian Outer Islands (353) ** Fenualoa (1,305) ** Nipua/Nopoli (880) ** Lipe/Temua (796) ** Manuopo (1,030) ** Nenumpo (1,163) * Santa Cruz Islands ** Graciosa Bay (1,264) ** North East Santa Cruz (1,843) ** Nanggu/Lord Howe (1,863) ** Nea/Noole (1,770) ** Nevenema (947) ** Luva Station (2,335) ** Neo (1,558) * isolated islands and groups ** Duff Islands (509) ** Utupua (1,168) ** Vanikoro (1,293) ** Tikopia (1,285) Islands The islands or island groups which make up the province are: * Anuta * Duff Islands (including Taumako) * ...
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Fujiwhara Effect
The Fujiwhara effect, sometimes referred to as the Fujiwara effect, Fujiwara interaction or binary interaction, is a phenomenon that occurs when two nearby cyclonic vortices move around each other and close the distance between the circulations of their corresponding low-pressure areas. The effect is named after Sakuhei Fujiwara, the Japanese meteorologist who initially described the effect. Binary interaction of smaller circulations can cause the development of a larger cyclone, or cause two cyclones to merge into one. Extratropical cyclones typically engage in binary interaction when within of one another, while tropical cyclones typically interact within of each other. Description When cyclones are in proximity of one another, their centers will circle each other cyclonically (counter-clockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere) about a point between the two systems due to their cyclonic wind circulations. The two vortices will be attract ...
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Coral Sea
The Coral Sea () is a marginal sea of the Pacific Ocean, South Pacific off the northeast coast of Australia, and classified as an Interim Biogeographic Regionalisation for Australia, interim Australian bioregion. The Coral Sea extends down the Australian northeast coast. Most of it is protected by the France, French Natural Park of the Coral Sea () and the Australian Coral Sea Marine Park. The sea was the location for the Battle of the Coral Sea, a major confrontation during World War II between the navies of the Empire of Japan, and the United States and Australia. The sea contains numerous islands and coral reef, reefs, as well as the world's largest reef system, the Great Barrier Reef (GBR), which was declared a World Heritage Site by UNESCO in 1981. All previous oil exploration projects were terminated at the GBR in 1975, and fishing is restricted in many areas. The reefs and islands of the Coral Sea are particularly rich in birds and aquatic life and are a popular touris ...
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Banks Islands
The Banks Islands (in Bislama ''Bankis'') are a group of islands in northern Vanuatu. Together with the Torres Islands to their northwest, they make up the northernmost province of Torba Province, Torba. The island group lies about north of Maewo, and includes Gaua and Vanua Lava, two of the 13 largest islands in Vanuatu. In 2009, the islands had a population of 8,533. The island group's combined land area is . Geography The largest island is Gaua (formerly called Santa Maria), which has a rugged terrain, rising to Mount Gharat, an active volcano at the centre of the island, at . Gaua's freshwater Lake Letas, in its volcanic crater, is the largest lake in Vanuatu. A slightly smaller island in the group, Vanua Lava, is higher, at ; it too has an active volcano: Mount Suretamate (also spelled Süretimiat or Sere'ama, ). To the east of Vanua Lava are two islets in the groupo, Ravenga and Kwakea (also spelled Qakea). Sola, Vanuatu, Sola, the provincial capital, is on Vanua Lava. The ...
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Ureparapara
Ureparapara (also known as ''Parapara'' for short; once known as ''Bligh Island'') is the third largest island in the Banks group of northern Vanuatu, after Gaua and Vanua Lava. The climate on the island is humid tropical. The average annual rainfall exceeds 4000 mm. Ureparapara is subject to frequent earthquakes and cyclones. Geography Ureparapara island is an old volcanic cone that has been breached by the sea on its east coast. The resulting bay is known as ''Divers' Bay'', and as ''Löyöp'' in the local language of the same name. Apart from this indentation, the island is circular in shape, with a diameter of . The land area is . History The first recorded European who arrived to Ureparapara was the Spanish explorer Pedro Fernández de Quirós on 15 June 1606. He first named the island ''Pilar de Zaragoza''; however, later on, it is charted as ''Nuestra Señora de Montserrate'' both by him and his chaplain Fray Martin de Munilla. In 1789, the island was rediscove ...
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Torres Islands
The Torres Islands are an island chain in the Torba Province of the country of Vanuatu, the country’s northernmost island group. The chain of islands that make up this micro-archipelago straddles the broader cultural boundary between Island Melanesia and several Polynesian outliers located in the neighbouring Solomon Islands. To the island chain’s north is Temotu Province of the Solomon Islands, to its south is Espiritu Santo, and to its southeast are the Banks Islands. To the west, beneath the ocean surface, is the deep Torres Trench, which is the subduction zone between the Australian Plate and Pacific Plate. The seven islands in the Torres group, from north to south, are Hiw island, Hiw or ''Hiu'' (the largest), Metoma, Tegua, Ngwel (an uninhabited islet), Linua, Lo (island), Lo or ''Loh'', and Toga (island), Toga. The island chain stretches across . The highest point of the chain is only above sea level. These islands are less rugged than the other islands of Vanuatu th ...
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Vanuatu
Vanuatu ( or ; ), officially the Republic of Vanuatu (; ), is an island country in Melanesia located in the South Pacific Ocean. The archipelago, which is of volcanic origin, is east of northern Australia, northeast of New Caledonia, east of New Guinea, southeast of Solomon Islands, and west of Fiji. Vanuatu was first inhabited by Melanesians, Melanesian people. The first Europeans to visit the islands were a Spanish expedition led by Portuguese navigator Pedro Fernandes de Queirós, Fernandes de Queirós, who arrived on the largest island, Espíritu Santo, in 1606. Queirós claimed the archipelago for Spain, as part of the colonial Spanish East Indies and named it . In the 1880s, France and the United Kingdom of Great Britain and Ireland, United Kingdom claimed parts of the archipelago, and in 1906, they agreed on a framework for jointly managing the archipelago as the New Hebrides through an Anglo-French condominium (international law), condominium. An independence movem ...
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Santa Cruz Islands
The Santa Cruz Islands form an archipelago in Temotu Province, Solomon Islands. They lie approximately to the southeast of the Solomon Islands (archipelago), Solomon Islands archipelago, just north of the archipelago of Vanuatu and are considered part of the Vanuatu rain forests ecoregion. The term Santa Cruz Islands is sometimes used to encompass all the islands of Temotu Province, Solomon Islands. Geography The largest island is Nendo Island, Nendö, which is also known as Santa Cruz Island proper. Lata, Solomon Islands, Lata, located on Nendö, is the largest town, and is the capital of Temotu Province. Other islands belonging to the Santa Cruz group are Vanikoro (which is actually made up of two islands, Banie (island), Banie and its small neighbour Teanu (island), Teanu) and Utupua. The table below provides basic data on these three islands. The Santa Cruz Islands are less than five million years old and were pushed upward by the Plate tectonics, tectonic subduction ...
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Rapid Intensification
Rapid intensification (RI) is any process wherein a tropical cyclone strengthens very dramatically in a short period of time. Tropical cyclone forecasting agencies utilize differing thresholds for designating rapid intensification events, though the most widely used definition stipulates an increase in the maximum sustained winds of a tropical cyclone of at least in a 24-hour period. However, periods of rapid intensification often last longer than a day. About 20–30% of all tropical cyclones undergo rapid intensification, including a majority of tropical cyclones with peak wind speeds exceeding . Rapid intensification constitutes a major source of error for tropical cyclone forecasting, and its predictability is commonly cited as a key area for improvement. The specific physical mechanisms that underlie rapid intensification and the environmental conditions necessary to support rapid intensification are unclear due to the complex interactions between the environment surr ...
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List Of Islands Of Tuvalu
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 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-dec ...
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