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Statements

Subject Item
dbr:2009_North_Indian_Ocean_cyclone_season
rdf:type
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rdfs:label
2009 North Indian Ocean cyclone season Temporada de ciclones no Índico Norte de 2009 Temporada de ciclones en el Índico Norte de 2009 Zyklonsaison im Nordindik 2009 2009年北印度洋氣旋季
rdfs:comment
La temporada de ciclones en el Índico Norte de 2009 fue un evento en el ciclo anual de la formación de ciclones tropicales. La temporada de ciclones del océano Índico Norte no tiene límites, pero los ciclones tienden a formarse entre abril y diciembre, con mayor incidencia entre mayo y noviembre. Estas fechas convencionalmente delimitan el período de cada año cuando la mayoría de los ciclones tropicales se forman en el norte del océano Índico. The 2009 North Indian Ocean cyclone season was an event in the annual cycle of tropical cyclone formation. The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and December, with peaks in May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. A temporada de ciclones no Oceano Índico norte de 2009 foi um evento em andamento do ciclo anual de formação de ciclones tropicais. A temporada de ciclones no oceano Índico não há limites específicos, embora a maioria dos ciclones tende a se formar em abril e dezembro, com picos em Maio e Novembro. Estas épocas do ano delimitam convencionalmente o período de cada ano quando a maioria dos ciclones tropical tende a se formar no Oceano Índico norte. Die Zyklonsaison im Nordindik 2009 hatte keine offizielle Grenzen wie in anderen Becken üblich, sondern lief das ganze Jahr hindurch. Die tropischen Wirbelstürme bilden sich allerdings in diesem Becken in der Regel zwischen April und Dezember, wobei die Monate vor und nach der Monsunsaison, also April/Mai und Oktober/November, die aktivsten sind. Einen tropischen Wirbelsturm im Indischen Ozean bezeichnet man als Zyklon. 2009年北印度洋氣旋季泛指在2009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。）
foaf:depiction
n5:BOB_03_2009_track.png n5:Phyan_2009-11-11_0325Z.jpg n5:Phyan_2009_track.png n5:Bijli_2009_track.png n5:Depression_ARB_01_2009-06-23_0600Z.jpg n5:03B_2009_track.png n5:Cyclonic_Storm_Bijli_2009-4-16.jpg n5:ARB_02_2009_track.png n5:Aila_2009_track.png n5:ARB_02_Jun_25_2009_0900Z.jpg n5:ARB_01_2009_track.png n5:Deep_Depression_BOB_03_2009.jpg n5:2009_North_Indian_Ocean_cyclone_season_summary.png n5:Ward_2009_track.png n5:Ward_2009-12-12_0455Z.jpg n5:TC_03B_5_September_2009.jpg n5:SCS_Aila_at_peak_intensity.jpg
dcterms:subject
dbc:2009_North_Indian_Ocean_cyclone_season dbc:Articles_which_contain_graphical_timelines dbc:Tropical_cyclones_in_2009
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dbo:thumbnail
n5:2009_North_Indian_Ocean_cyclone_season_summary.png?width=300
dbp:seasonTimeline
Timeline of the 2009 North Indian Ocean cyclone season
dbp:1MinWinds
40 45 50 65
dbp:3MinWinds
45 40 60 30 25
dbp:basin
NIO North Indian Ocean
dbp:deaths
419
dbp:dissipated
0001-06-24 0001-06-25 0001-11-11 0001-04-17 0001-05-26 0001-07-21 0001-12-16 0001-09-07
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2009-04-14
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9223372036854775807
dbp:lastStormDissipated
2009-12-16
dbp:strongestStormName
dbr:Cyclone_Aila
dbp:strongestStormWinds
60
dbp:totalHurricanes
1
dbp:totalStorms
4
dbp:damage
>
dbp:damages
1300
dbp:date
2010-03-01
dbp:dates
0001-04-14
dbp:fatalities
419
dbp:formed
0001-09-04 0001-06-23 0001-12-10 0001-07-20 0001-06-25 0001-05-23 0001-11-04 0001-04-14
dbp:pressure
968 988 996 998
dbp:track
Bijli 2009 track.png 2009 ARB 02 2009 track.png Phyan 2009 track.png BOB 03 2009 track.png Ward 2009 track.png 3 Aila 2009 track.png ARB 01 2009 track.png
dbp:type
cyclone niodepression
dbp:url
n14:JTWC
dbp:year
2000 2009
dbp:atlanticSeason
2009
dbp:eastPacificSeason
2009
dbp:totalDisturbances
8
dbp:westPacificSeason
2009
dbp:tc's
8
dbp:winds
110.0
dbp:averageWindSpeed
3
dbp:strongestStormPressure
968
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6
dbo:abstract
La temporada de ciclones en el Índico Norte de 2009 fue un evento en el ciclo anual de la formación de ciclones tropicales. La temporada de ciclones del océano Índico Norte no tiene límites, pero los ciclones tienden a formarse entre abril y diciembre, con mayor incidencia entre mayo y noviembre. Estas fechas convencionalmente delimitan el período de cada año cuando la mayoría de los ciclones tropicales se forman en el norte del océano Índico. El ámbito de este artículo se limita a la del océano Índico en el Hemisferio Norte, al este del Cuerno de África y al oeste de la península Malaya. Hay dos principales mares en el norte del océano Índico: el mar Arábigo, al oeste del subcontinente indio, abreviado ARB y la bahía de Bengala al este, abreviado BOB por el IMD. El Centro Meteorológico Regional Especializado en esta cuenca es el Departamento de Meteorología de la India (IMD), mientras que el Centro Conjunto de Advertencia de Tifones (JTWC) emite informes no oficiales. La escala de ciclones tropicales para esta cuenca se detalla en la derecha. En promedio, entre 4 a 6 tormentas se forman de esta cuenca cada temporada.​ Die Zyklonsaison im Nordindik 2009 hatte keine offizielle Grenzen wie in anderen Becken üblich, sondern lief das ganze Jahr hindurch. Die tropischen Wirbelstürme bilden sich allerdings in diesem Becken in der Regel zwischen April und Dezember, wobei die Monate vor und nach der Monsunsaison, also April/Mai und Oktober/November, die aktivsten sind. Einen tropischen Wirbelsturm im Indischen Ozean bezeichnet man als Zyklon. Das zuständige Regional Specialized Meteorological Centre (RSMC) ist das India Meteorological Department in Neu-Delhi. Dieses vergibt für diejenigen tropischen Wirbelstürme, die mindestens den Status eines Zyklons erreichen, einen Namen. Tiefdruckgebiete (je nach Windgeschwindigkeit depressions oder deep depressions) werden fortlaufend nummeriert, wobei die Buchstabenkombination BOB anzeigt, dass sich das System im Golf von Bengalen bildete. Die Buchstaben ARB stehen sinngemäß für das Arabische Meer. Durch das Joint Typhoon Warning Center (JTWC) in Honolulu werden für die US-amerikanischen Einrichtungen im Indischen Ozean eigenständige Warnungen und Prognosen ausgegeben. Durch das JTWC erfolgt die Einstufung nach der Saffir-Simpson-Hurrikan-Windskala, das RSMC wendet für die Einstufung eigene Kriterien an, denen unter anderem die Messung der andauernden Windgeschwindigkeit auf Basis einer dreiminütigen Beobachtung zugrunde liegt. 2009年北印度洋氣旋季泛指在2009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。） The 2009 North Indian Ocean cyclone season was an event in the annual cycle of tropical cyclone formation. The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and December, with peaks in May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. The scope of this article is limited to the Indian Ocean in the Northern Hemisphere, east of the Horn of Africa and west of the Malay Peninsula. There are two main seas in the North Indian Ocean — the Arabian Sea to the west of the Indian subcontinent, abbreviated ARB by the India Meteorological Department (IMD); and the Bay of Bengal to the east, abbreviated BOB by the IMD. The official Regional Specialized Meteorological Centre in this basin is the India Meteorological Department (IMD), while the Joint Typhoon Warning Center releases unofficial advisories. The tropical cyclone scale for this basin is detailed on the right. On average, 4 to 6 storms form in this basin every season. A temporada de ciclones no Oceano Índico norte de 2009 foi um evento em andamento do ciclo anual de formação de ciclones tropicais. A temporada de ciclones no oceano Índico não há limites específicos, embora a maioria dos ciclones tende a se formar em abril e dezembro, com picos em Maio e Novembro. Estas épocas do ano delimitam convencionalmente o período de cada ano quando a maioria dos ciclones tropical tende a se formar no Oceano Índico norte. A temporada iniciou-se efetivamente em meados de abril, quando o ciclone Bijli formou-se no golfo de Bengala. Bijli causou seis fatalidades ao atingir a costa de Bangladexe dias depois. O ciclone Aila foi o mais intenso e o mais desastroso ciclone tropical da temporada, quando causou mais de 330 fatalidades também em Bangladexe no final de maio. O ciclone Phyan foi o único ciclone tropical dotado de nome no mar Arábico em 2009, e atingiu a costa da Índia, causado outras sete fatalidades. O , que se formou em meados de dezembro, foi último ciclone da temporada, e causou apenas danos mínimos no Seri Lanca.
gold:hypernym
dbr:Event
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