2012–13 South-West Indian Ocean Cyclone Season
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2012–13 South-West Indian Ocean Cyclone Season
The 2012–13 South-West Indian Ocean cyclone season was a slightly above average event in tropical cyclone formation in the Southern hemisphere tropical cyclone year starting on July 1, 2012, and ending on June 30, 2013. Within this basin, tropical and subtropical disturbances are officially monitored by the Regional Specialised Meteorological Centre on Réunion island, while the Mauritius and Madagascar weather services assign names to significant tropical and subtropical disturbances. The first tropical disturbance of the season developed on October 12 and rapidly developed into the earliest known intense tropical cyclone on record during October 14. __TOC__ Seasonal summary ImageSize = width:800 height:200 PlotArea = top:10 bottom:80 right:20 left:20 Legend = columns:3 left:30 top:58 columnwidth:250 AlignBars = early DateFormat = dd/mm/yyyy Period = from:01/10/2012 till:01/06/2013 TimeAxis = orientation:horizontal ScaleMinor = grid:black unit:month increment:1 s ...
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Cyclone Felleng
Intense Tropical Cyclone Felleng was a powerful tropical cyclone that caused destruction across Seychelles, Madagascar, and Réunion. The seventh Tropical Disturbance, sixth named storm, and the third Intense Tropical Cyclone of the 2012–13 South-West Indian Ocean cyclone season, Felleng originated from an area of atmospheric convection embedded in the Intertropical Convergence Zone. In total, Felleng caused 18 fatalities and above US$10 million in damages. Meteorological history After the Madden–Julian oscillation left its suppressive phase in the South-West Indian Ocean, a low-pressure area embedded in the Intertropical Convergence Zone was noted by Météo-France La Réunion (MFR) on 24 January. Convection was mainly active in the northeast portion of the system, with winds reaching in some places. The system's low-level circulation was poorly defined by 25 January, with the system as a whole being negatively affected by wind shear. At 18:00 Coordinated Universal Time ...
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West Sumatra
West Sumatra () is a Provinces of Indonesia, province of Indonesia. It is on the west coast of the island of Sumatra and includes the Mentawai Islands off that coast. West Sumatra borders the Indian Ocean to the west, as well as the provinces of North Sumatra to the north, Riau to the northeast, Jambi to the southeast, and Bengkulu to the south. The province has an area of , or about the same size as Switzerland, with a population of 5,534,472 at the 2020 Indonesian census, 2020 census.Badan Pusat Statistik, Jakarta, 2021. The official estimate at mid 2023 was 5,757,210 (comprising 2,900,270 males and 2,856,940 females).Badan Pusat Statistik, Jakarta, 28 February 2024, ''Provinsi Sumatera Barat Dalam Angka 2024'' (Katalog-BPS 1102001.13) The province is List of regencies and cities in West Sumatra, subdivided into twelve Regency (Indonesia), regencies and seven City status in Indonesia#Kota, cities. It has relatively more cities than other provinces outside Java, although several o ...
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Subtropical Ridge
The horse latitudes are the latitudes about 30 degrees north and south of the Equator. They are characterized by sunny skies, calm winds, and very little precipitation. They are also known as subtropical ridges or highs. It is a high-pressure area at the divergence of trade winds and the westerlies. Etymology A likely and documented explanation is that the term is derived from the "dead horse" ritual of seamen (see Beating a dead horse). In this practice, the seaman paraded a straw-stuffed effigy of a horse around the deck before throwing it overboard. Seamen were paid partly in advance before a long voyage, and they frequently spent their pay all at once, resulting in a period of time without income. This period was called the "dead horse" time, and it usually lasted a month or two. The seaman's ceremony was to celebrate having worked off the "dead horse" debt. As west-bound shipping from Europe usually reached the subtropics at about the time the "dead horse" was worke ...
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Plaine Des Cafres
The Plaine des Cafres is a plateau on Réunion Island, one of the French volcanic islands in the Mascarene Islands, Mascarene Archipelago in the southwestern Indian Ocean. It is part of the Communes of France, commune of Le Tampon. It is named after the :fr:Cafres, Cafres, black slaves who hid in the area during and before the 18th century. « Entre ces plaines [...] la plus remarquable, et dont personne n’a rien écrit, est celle qu’on a nommée la plaine des Cafres, à cause qu’une troupe de Cafres, esclaves des habitants de l’île, s’y étaient allés cacher, après avoir quitté leurs maîtres. [...] Cette plaine était inconnue avant la fuite des Cafres » (‘The most remarkable among the plains – one which nobody has written about – is one named the ''Plaine des Cafres'', for the group of Cafres (slaves of the islanders) who escaped there in hiding, after leaving their masters. [...] This plain was unknown before the Cafres escaped [to dwell there].’) Geo ...
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Vatovavy-Fitovinany
Vatovavy-Fitovinany was a region of Madagascar Madagascar, officially the Republic of Madagascar, is an island country that includes the island of Madagascar and numerous smaller peripheral islands. Lying off the southeastern coast of Africa, it is the world's List of islands by area, f ... from 2004 to 2021. Vatovavy-Fitovinany that was split on 16 June 2021 to become the regions Vatovavy and Fitovinany. Administrative divisions Fitovinany Region was divided into six districts, which are sub-divided into 125 communes. Districts * Ifanadiana - 14 communes * Ikongo - 17 communes * Manakara-Atsimo - 42 communes * Mananjary - 25 communes * Nosy Varika - 19 communes * Vohipeno - 17 communes References Former subdivisions of Madagascar Regions of Madagascar {{Madagascar-geo-stub ...
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Antananarivo
Antananarivo (Malagasy language, Malagasy: ; French language, French: ''Tananarive'', ), also known by its colonial shorthand form Tana (), is the Capital city, capital and largest city of Madagascar. The administrative area of the city, known as Antananarivo-Renivohitra ("Antananarivo-Mother Hill" or "Antananarivo-Capital"), is the capital of Analamanga region. The city sits at above sea level in the center of the island, making it the List of capital cities by elevation, highest national capital by elevation among the Island country, island countries. It has been the country's largest population center since at least the 18th century. The President of Madagascar, Presidency, National Assembly of Madagascar, National Assembly, Senate of Madagascar, Senate, and Supreme Court are located there, as are List of diplomatic missions in Madagascar, 21 diplomatic missions and the headquarters of many national and international businesses and Non-governmental organization, non-governme ...
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Rodrigues
Rodrigues ( ; Mauritian Creole, Creole: ) is a Autonomous administrative division, autonomous Outer islands of Mauritius, outer island of the Republic of Mauritius in the Indian Ocean, about east of Mauritius. It is part of the Mascarene Islands, which include Mauritius and Réunion. Like Agaléga, Rodrigues is a constituent island of the Mauritius, Republic of Mauritius, under the Constitution of Mauritius and still remains, as explicitly defined by the same Constitution, part of the Sovereignty of Mauritius, together with the following islands: "Agaléga, Tromelin Island, Tromelin, Cargados Carajos (Saint Brandon), Chagos Archipelago ... Diego Garcia and other islands included in the State of Mauritius". Rodrigues is of volcanic origin and is surrounded by coral reef, and some tiny uninhabited islands lie just off its coast. The island used to be the tenth District of Mauritius; it gained autonomous status on 12 October 2002, and is governed by the Rodrigues Regional Assemb ...
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Convection
Convection is single or Multiphase flow, multiphase fluid flow that occurs Spontaneous process, spontaneously through the combined effects of material property heterogeneity and body forces on a fluid, most commonly density and gravity (see buoyancy). When the cause of the convection is unspecified, convection due to the effects of thermal expansion and buoyancy can be assumed. Convection may also take place in soft solids or mixtures where particles can flow. Convective flow may be Transient state, transient (such as when a Multiphasic liquid, multiphase mixture of oil and water separates) or steady state (see convection cell). The convection may be due to Gravity, gravitational, Electromagnetism, electromagnetic or Fictitious force, fictitious body forces. Convection (heat transfer), Heat transfer by natural convection plays a role in the structure of Earth's atmosphere, its oceans, and its Earth's mantle, mantle. Discrete convective cells in the atmosphere can be identified by ...
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RAAF Learmonth
RAAF Base Learmonth, also known as Learmonth Airport , is a joint use Royal Australian Air Force base and civil airport. It is located near the town of Exmouth on the north-west coast of Western Australia. RAAF Base Learmonth is one of the RAAF's three bare bases. It is maintained by the RAAF's 25 Squadron and a small caretaker staff during peacetime. The RAAF also operates the Learmonth Air Weapons Range which covers about and is located south-west of the airbase. History During World War II a little-known landing field was constructed on the western shore of Exmouth Gulf. It was code-named "Potshot" and maintained by No. 76 Operational Base Unit, in support of Operation Potshot. In the 1950s the landing field was further developed as a military base and named RAAF Learmonth in honour of Wing Commander Charles Learmonth DFC and Bar, who, while leading No. 14 Squadron, was killed in a flying accident off Rottnest Island, Western Australia on 6 January 1944. Starting i ...
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Euro
The euro (currency symbol, symbol: euro sign, €; ISO 4217, currency code: EUR) is the official currency of 20 of the Member state of the European Union, member states of the European Union. This group of states is officially known as the euro area or, more commonly, the eurozone. The euro is divided into 100 1 euro cent coin, euro cents. The currency is also used officially by the institutions of the European Union, by International status and usage of the euro, four European microstates that are not EU members, the British Overseas Territory of Akrotiri and Dhekelia, as well as unilaterally by Montenegro and Kosovo. Outside Europe, a number of special territories of EU members also use the euro as their currency. The euro is used by 350 million people in Europe and additionally, over 200 million people worldwide use currencies pegged to the euro. It is the second-largest reserve currency as well as the second-most traded currency in the world after the United Sta ...
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Flic-en-Flac
Flic-en-Flac () is a seaside List of places in Mauritius, village on the west coast of Mauritius in the Districts of Mauritius, district of Rivière Noire District, Black River. The name most likely comes from an Old Dutch phrase, "Fried Landt Flaak", meaning free, flat land. Its public white sandy beach is one of the longest on the island. This public beach attracts local families, tourists and visitors throughout the year. Its lagoon is protected by the surrounding coral reefs. The beach provides scenic views over the Indian Ocean horizon and of Le Morne Brabant Peninsula located in the southwest of Mauritius. Flic-en-Flac is a few kilometres from Tamarin, Mauritius, Tamarin beach. The Casela Bird Park near Flic-en-Flac features orchids, over 140 species of birds and the endemic and endangered rare pink pigeon. Flic-en-Flac is in a non-industrial part of Mauritius, with a coastline of about . It is geared towards tourism with many luxury hotels in Mauritius, experiencing about ...
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Anticyclone
A high-pressure area, high, or anticyclone, is an area near the surface of a planet where the atmospheric pressure is greater than the pressure in the surrounding regions. Highs are middle-scale meteorological features that result from interplays between the relatively larger-scale dynamics of an entire planet's atmospheric circulation. The strongest high-pressure areas result from masses of cold air which spread out from polar regions into cool neighboring regions. These highs weaken once they extend out over warmer bodies of water. Weaker—but more frequently occurring—are high-pressure areas caused by atmospheric subsidence: Air becomes cool enough to precipitate out its water vapor, and large masses of cooler, drier air descend from above. Within high-pressure areas, winds flow from where the pressure is highest, at the center of the area, towards the periphery where the pressure is lower. However, the direction is not straight from the center outwards, but curved du ...
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