Cyclone Fantala (original) (raw)
Siklon Fantala adalah topan tropis terkuat di Samudra Hindia Barat Daya dalam hal angin yang berkelanjutan. Bagian dari musim siklon 2015-16, Fantala terbentuk pada 11 April di sebelah selatan Diego Garcia, sebuah pulau di tengah Samudra Hindia.
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| dbo:abstract | Very Intense Tropical Cyclone Fantala was the most intense tropical cyclone recorded in the South-West Indian Ocean in terms of sustained winds. Part of the 2015–16 cyclone season, Fantala formed on 11 April to the south of Diego Garcia, an island in the central Indian Ocean. With a ridge to the south, the storm moved westward for several days while gaining strength, aided by warm waters and decreasing wind shear. Late on 17 April, the Météo-France office on Réunion (MFR) estimated peak 10-minute winds of 250 km/h (155 mph), making Fantala the strongest tropical cyclone of the basin in terms of 10-minute sustained winds. The Joint Typhoon Warning Center (JTWC) estimated peak 1-minute winds of 285 km/h (180 mph), equivalent to Category 5 intensity on the Saffir-Simpson scale, also the strongest on record in the South-West Indian Ocean, in terms of maximum sustained wind speed. Early on 18 April, Fantala reached its peak intensity, with a minimum central pressure of 910 millibars (27 inHg). While near peak intensity, Fantala passed near the Farquhar Group of the Seychelles, damaging most of the buildings in the small archipelago. Later on 18 April, Fantala had weakened to an intense tropical cyclone and slowed its forward motion, eventually reversing its direction of movement. After fluctuating in strength, the disorganized system reversed direction again, making its closest approach to Madagascar. Fantala degenerated into a remnant low on 24 April, and the remnants continued toward Tanzania. There, heavy rainfall resulted in flooding that washed away roads and houses, killing 13 people. Rains extended further into Kenya, with similar effects. (en) Siklon Fantala adalah topan tropis terkuat di Samudra Hindia Barat Daya dalam hal angin yang berkelanjutan. Bagian dari musim siklon 2015-16, Fantala terbentuk pada 11 April di sebelah selatan Diego Garcia, sebuah pulau di tengah Samudra Hindia. (in) O ciclone tropical muito intenso Fantala foi o ciclone tropical mais forte que se formou no sudoeste do Oceano Índico em termos de ventos sustentados. Parte da temporada de ciclones de 2015–16, o Fantala se formou em 11 de abril ao sul de Diego Garcia, uma ilha na região central do Oceano Índico. Com uma crista ao sul, a tempestade moveu-se para oeste por vários dias enquanto ganhava força, auxiliada pelas águas quentes e diminuindo o cisalhamento do vento. No final de 17 de abril, o escritório da Météo-France em Reunião (MFR) estimou o pico de ventos de 10 minutos em 250 km/h (160 mph), tornando Fantala o ciclone tropical mais forte da bacia em termos de ventos sustentados de 10 minutos. O Joint Typhoon Warning Center (JTWC) estimou o pico de ventos de 1 minuto em 285 km/h (177 mph), equivalente à intensidade da Categoria 5 na escala Saffir-Simpson, também a mais forte já registada no sudoeste do Oceano Índico, em termos de velocidade máxima do vento sustentado. No início de 18 de abril, Fantala atingiu o seu pico de intensidade, com uma pressão central mínima de 910 mbar (27 inHg). Enquanto estava perto do pico de intensidade, Fantala passou perto do Grupo Farquhar das Seychelles, danificando a maioria dos edifícios do pequeno arquipélago. Mais tarde, em 18 de abril, Fantala enfraqueceu para um intenso ciclone tropical e desacelerou seu movimento para a frente, eventualmente revertendo a sua direção de movimento. Depois de flutuar em força, o sistema desorganizado inverteu a direção novamente, aproximando-se mais de Madagáscar. Fantala degenerou em um ponto baixo remanescente em 24 de abril, e os remanescentes continuaram em direção à Tanzânia. Lá, chuvas fortes resultaram em inundações que destruíram estradas e casas, matando 13 pessoas. As chuvas se estenderam ainda mais no Quênia, com efeitos semelhantes. (pt) 特強熱帶氣旋凡塔拉是西南印度洋有氣象記錄以來最強烈的熱帶氣旋。就最大持續風速而言。凡塔拉是2015－2016年西南印度洋熱帶氣旋季的一部分，2016年4月11日，一個熱帶擾動在印度洋中部的迪戈加西亞島南部生成。風暴受南部的高壓脊影響，凡塔拉開始在在獲得风力的同時逐漸向西移動。在溫暖的海水和減少的風切變的幫助下。4月18日，凡塔拉強度到達巔峰。法國氣象局駐留尼汪氣象中心（MFR）認定凡塔拉巔峰強度（十分鐘）風速為250公里（155英里），使凡塔拉成為西南印度洋有氣象記錄以來最強烈的熱帶氣旋。聯合颱風警報中心認為凡塔拉一分鐘最大持續風速為285公里（180英里）並評定凡塔拉中心最低氣壓為910百帕（毫巴）（27英寸汞柱）。 凡塔拉在達到巔峰強度時席捲了塞舌爾的法夸爾群島，島上大部分建築都被損壞。4月18日晚，凡塔拉減弱為強烈熱帶氣旋，並減緩了移動速度，導致其行進方向發生扭轉。強度減弱後，凡塔拉的行進方向再次發生扭轉，使其開始向馬達加斯加前進。4月24日，凡塔拉退化成殘留低氣壓，其殘留云系抵達坦桑尼亞，並導致坦桑尼亞因大雨而洪水氾濫，道路被衝毀，並造成13人死亡。凡塔拉的殘餘雲系更深入到了肯尼亞境內，造成了與坦桑尼亞類似的影響， (zh) |
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| dbp:1MinWinds | 155 (xsd:integer) |
| dbp:areas | dbr:Madagascar dbr:Agaléga dbr:Tanzania dbr:Seychelles |
| dbp:basin | SWI (en) |
| dbp:damages | 4.500000 (xsd:double) |
| dbp:date | 2017-01-02 (xsd:date) |
| dbp:dissipated | 2016-04-27 (xsd:date) |
| dbp:fatalities | 13 (xsd:integer) |
| dbp:formed | 2016-04-11 (xsd:date) |
| dbp:gusts | 190 (xsd:integer) |
| dbp:hurricaneSeason | 2015 (xsd:integer) |
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| dbp:name | Very Intense Tropical Cyclone Fantala (en) |
| dbp:pressure | 910 (xsd:integer) |
| dbp:remnantLow | 0001-04-23 (xsd:gMonthDay) |
| dbp:type | tropical cyclone (en) |
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| rdfs:comment | Siklon Fantala adalah topan tropis terkuat di Samudra Hindia Barat Daya dalam hal angin yang berkelanjutan. Bagian dari musim siklon 2015-16, Fantala terbentuk pada 11 April di sebelah selatan Diego Garcia, sebuah pulau di tengah Samudra Hindia. (in) 特強熱帶氣旋凡塔拉是西南印度洋有氣象記錄以來最強烈的熱帶氣旋。就最大持續風速而言。凡塔拉是2015－2016年西南印度洋熱帶氣旋季的一部分，2016年4月11日，一個熱帶擾動在印度洋中部的迪戈加西亞島南部生成。風暴受南部的高壓脊影響，凡塔拉開始在在獲得风力的同時逐漸向西移動。在溫暖的海水和減少的風切變的幫助下。4月18日，凡塔拉強度到達巔峰。法國氣象局駐留尼汪氣象中心（MFR）認定凡塔拉巔峰強度（十分鐘）風速為250公里（155英里），使凡塔拉成為西南印度洋有氣象記錄以來最強烈的熱帶氣旋。聯合颱風警報中心認為凡塔拉一分鐘最大持續風速為285公里（180英里）並評定凡塔拉中心最低氣壓為910百帕（毫巴）（27英寸汞柱）。 凡塔拉在達到巔峰強度時席捲了塞舌爾的法夸爾群島，島上大部分建築都被損壞。4月18日晚，凡塔拉減弱為強烈熱帶氣旋，並減緩了移動速度，導致其行進方向發生扭轉。強度減弱後，凡塔拉的行進方向再次發生扭轉，使其開始向馬達加斯加前進。4月24日，凡塔拉退化成殘留低氣壓，其殘留云系抵達坦桑尼亞，並導致坦桑尼亞因大雨而洪水氾濫，道路被衝毀，並造成13人死亡。凡塔拉的殘餘雲系更深入到了肯尼亞境內，造成了與坦桑尼亞類似的影響， (zh) Very Intense Tropical Cyclone Fantala was the most intense tropical cyclone recorded in the South-West Indian Ocean in terms of sustained winds. Part of the 2015–16 cyclone season, Fantala formed on 11 April to the south of Diego Garcia, an island in the central Indian Ocean. With a ridge to the south, the storm moved westward for several days while gaining strength, aided by warm waters and decreasing wind shear. Late on 17 April, the Météo-France office on Réunion (MFR) estimated peak 10-minute winds of 250 km/h (155 mph), making Fantala the strongest tropical cyclone of the basin in terms of 10-minute sustained winds. The Joint Typhoon Warning Center (JTWC) estimated peak 1-minute winds of 285 km/h (180 mph), equivalent to Category 5 intensity on the Saffir-Simpson scale, also the stron (en) O ciclone tropical muito intenso Fantala foi o ciclone tropical mais forte que se formou no sudoeste do Oceano Índico em termos de ventos sustentados. Parte da temporada de ciclones de 2015–16, o Fantala se formou em 11 de abril ao sul de Diego Garcia, uma ilha na região central do Oceano Índico. Com uma crista ao sul, a tempestade moveu-se para oeste por vários dias enquanto ganhava força, auxiliada pelas águas quentes e diminuindo o cisalhamento do vento. No final de 17 de abril, o escritório da Météo-France em Reunião (MFR) estimou o pico de ventos de 10 minutos em 250 km/h (160 mph), tornando Fantala o ciclone tropical mais forte da bacia em termos de ventos sustentados de 10 minutos. O Joint Typhoon Warning Center (JTWC) estimou o pico de ventos de 1 minuto em 285 km/h (177 mph), equi (pt) |
| rdfs:label | Cyclone Fantala (en) Siklon Fantala (in) Ciclone Fantala (pt) 氣旋凡塔拉 (zh) |
| owl:sameAs | yago-res:Cyclone Fantala wikidata:Cyclone Fantala dbpedia-id:Cyclone Fantala dbpedia-pt:Cyclone Fantala dbpedia-zh:Cyclone Fantala https://global.dbpedia.org/id/2FWqv |
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