The 2011 North Indian Ocean cyclone season was the least active tropical cyclone season in the North Indian Ocean since 1993. Only two cyclonic storms formed, below the average of four to six. 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
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| - Die Zyklonsaison im Nordindik 2011 hat keine offiziellen Grenzen wie in anderen Becken üblich, sondern läuft 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.
- 2011年北印度洋氣旋季泛指在2011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。）
- 2011년 북인도양 사이클론 (2011 North Indian cyclone season)에서는 2011년에 발생한 북인도양 사이클론과 열대성 저기압의 활동에 대해 기록한다. 을 시작으로, 2011년동안 10개의 저기압, 6개의 발달한 저기압, 2개의 사이클론, 1개의 매우 강한 사이클론이 발생하였다.
- The 2011 North Indian Ocean cyclone season was the least active tropical cyclone season in the North Indian Ocean since 1993. Only two cyclonic storms formed, below the average of four to six. 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. This is the first season to have only two named storms since the 1993 North Indian Ocean cyclone season. However, multiple Depressions along with Cyclonic Storm Keila and Very Severe Cyclonic Storm Thane wreaked damage worth at least US$1.64 million and killing some 360 people overall. It is believed that La Niña, a quasiperiodic climate pattern that causes a rise in surface pressure over the Indian Ocean and makes the region drier is the main cause behind the below normal activity in the basin.
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| - Die Zyklonsaison im Nordindik 2011 hat keine offiziellen Grenzen wie in anderen Becken üblich, sondern läuft 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.
- 2011年北印度洋氣旋季泛指在2011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。）
- 2011년 북인도양 사이클론 (2011 North Indian cyclone season)에서는 2011년에 발생한 북인도양 사이클론과 열대성 저기압의 활동에 대해 기록한다. 을 시작으로, 2011년동안 10개의 저기압, 6개의 발달한 저기압, 2개의 사이클론, 1개의 매우 강한 사이클론이 발생하였다.
- The 2011 North Indian Ocean cyclone season was the least active tropical cyclone season in the North Indian Ocean since 1993. Only two cyclonic storms formed, below the average of four to six. 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
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| - 2011 North Indian Ocean cyclone season
- 2011年北印度洋氣旋季
- 2011년 북인도양 사이클론
- Zyklonsaison im Nordindik 2011
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