2004 North Indian Ocean cyclone season
http://dbpedia.org/resource/2004_North_Indian_Ocean_cyclone_season an entity of type: Abstraction100002137
2004年北印度洋氣旋季泛指在2004年全年內的任何時間，於北印度洋水域所產生的熱帶氣旋。雖然有關方面並沒有設下本颱風季的指定期限，但大部份北印度洋的熱帶氣旋通常都會於四月至十二月期間形成。 本條目的範圍僅侷限於北印度洋水域。在北印度洋產生的氣旋風暴是由隶属于的印度氣象局新德里颱風中心命名，而在該地區的熱帶低氣壓的編號都以 A/B 字母作結。 在香港天文台的天氣圖上也包括東北印度洋地區，若有熱帶氣旋形成，則採用世界氣象組織級別法，最高強度都稱之為「颱風」，所有風暴都是無命名的。 （以下各氣旋風暴資訊以氣旋風暴存在期間的最強形態為名稱。）
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The 2004 North Indian Ocean cyclone season was the first in which tropical cyclones were officially named in the basin. Cyclone Onil, which struck Pakistan, was named in late September. The final storm, Cyclone Agni, was also named, and crossed into the southern hemisphere shortly before dissipation. This storm became notable during its origins and became one of the storms closest to the equator. The season was fairly active, with ten depressions forming from May to November. The India Meteorological Department designated four of these as cyclonic storms, which have maximum sustained winds of at least 65 km/h (40 mph) averaged over three minutes. The Joint Typhoon Warning Center also issued warnings for five of the storms on an unofficial basis.
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A temporada de ciclones no Oceano Índico norte de 2004 foi um evento do ciclo anual da formação de ciclones tropicais. Não há limites específicos para o começo ou o término da temporada de ciclones no Oceano Índico Norte, mas os ciclones tendem a se formar entre abril e dezembro, com picos em maio e novembro. Estas datas delimitam convencionalmente o período de cada ano quando a maioria dos ciclones tropicais se forma no Oceano Índico Norte.
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2004 North Indian Ocean cyclone season
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Temporada de ciclones no Índico Norte de 2004
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2004年北印度洋氣旋季
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NIO
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North Indian Ocean
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587
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--05-10
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2004-05-05
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2004-12-02
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May 5 –
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2004
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ARB02 2004 track.png
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Agni 2004 track.png
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BOB02 2004 track.png
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Cyclone 01A 2004 track.png
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Cyclone 02B 2004 track.png
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Cyclone 04A 2004 track.png
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LAND01 2004 track.png
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Onil 2004 track.png
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cyclone
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2004
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2004
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The 2004 North Indian Ocean cyclone season was the first in which tropical cyclones were officially named in the basin. Cyclone Onil, which struck Pakistan, was named in late September. The final storm, Cyclone Agni, was also named, and crossed into the southern hemisphere shortly before dissipation. This storm became notable during its origins and became one of the storms closest to the equator. The season was fairly active, with ten depressions forming from May to November. The India Meteorological Department designated four of these as cyclonic storms, which have maximum sustained winds of at least 65 km/h (40 mph) averaged over three minutes. The Joint Typhoon Warning Center also issued warnings for five of the storms on an unofficial basis. In early May, two tropical storms formed on opposite sides of India. The first formed on May 5 and meandered while intensifying, dropping 1,840 mm (72 in) in Aminidivi in the Lakshadweep group offshore western India, which was the highest daily rainfall total in the basin. A week later, a cyclone – the strongest of the season – struck Myanmar, killing 236 people and leaving 25,000 people homeless. Depressions also formed on opposite sides of India in June. A depression in September killed 59 people after dropping torrential rainfall over Bangladesh and adjacent West Bengal. In October, another depression struck the region, killing 273 people. There was also a short-lived cyclonic storm in the Arabian Sea in November.
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A temporada de ciclones no Oceano Índico norte de 2004 foi um evento do ciclo anual da formação de ciclones tropicais. Não há limites específicos para o começo ou o término da temporada de ciclones no Oceano Índico Norte, mas os ciclones tendem a se formar entre abril e dezembro, com picos em maio e novembro. Estas datas delimitam convencionalmente o período de cada ano quando a maioria dos ciclones tropicais se forma no Oceano Índico Norte. Convencionalmente, decidiu-se separar o Oceano Índico em diferentes áreas de monitoramento de ciclones tropicais. O objetivo deste artigo é detalhar os ciclones tropicais que se formam ao norte da linha do Equador, ou seja, detalhar os ciclones tropicais que se formaram na parte do Oceano Índico situada no Hemisfério norte, entre o Chifre da África e a Península da Malásia. Nesta área, há dois mares principais: o Mar Arábico a oeste do Subcontinente Indiano, abreviada pelo Departamento Meteorológico da Índia (DMI) como ARB; e o Golfo de Bengala a leste do Subcontinente Indiano, abreviada pelo DMI como BOB. Em meados da temporada de 2004, o sistema de nomeação de ciclones tropicais foi estabelecido no Índico Norte. Antes disso, não havia uma lista de nomes para os ciclones tropicais no Índico Norte. No início de outubro de 2004, a formação do marcou a primeira vez que um ciclone tropical formado no Índico Norte recebeu um nome. A iniciativa do Departamento Meteorológico da Índia foi aprovada pela Organização Meteorológica Mundial, e ciclones tropicais com intensidade igual ou superior a 65 km/h são nomeados desde então.
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2004年北印度洋氣旋季泛指在2004年全年內的任何時間，於北印度洋水域所產生的熱帶氣旋。雖然有關方面並沒有設下本颱風季的指定期限，但大部份北印度洋的熱帶氣旋通常都會於四月至十二月期間形成。 本條目的範圍僅侷限於北印度洋水域。在北印度洋產生的氣旋風暴是由隶属于的印度氣象局新德里颱風中心命名，而在該地區的熱帶低氣壓的編號都以 A/B 字母作結。 在香港天文台的天氣圖上也包括東北印度洋地區，若有熱帶氣旋形成，則採用世界氣象組織級別法，最高強度都稱之為「颱風」，所有風暴都是無命名的。 （以下各氣旋風暴資訊以氣旋風暴存在期間的最強形態為名稱。）
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