The 2010–11 South-West Indian Ocean cyclone season was the least active cyclone season on record in the basin, tied with 1982–83, producing only three systems of gale intensity. This was due to cooler than normal water temperatures and the Walker circulation – a broad atmospheric circulation – causing unusually moist conditions in the eastern Indian Ocean and unusually dry conditions in the western Indian Ocean. The basin includes the waters of the ocean south of the equator and west of 90º E to the eastern coast of Africa.
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| - The 2010–11 South-West Indian Ocean cyclone season was the least active cyclone season on record in the basin, tied with 1982–83, producing only three systems of gale intensity. This was due to cooler than normal water temperatures and the Walker circulation – a broad atmospheric circulation – causing unusually moist conditions in the eastern Indian Ocean and unusually dry conditions in the western Indian Ocean. The basin includes the waters of the ocean south of the equator and west of 90º E to the eastern coast of Africa. There were nine tropical or subtropical cyclones during the season, including five weak tropical disturbances or depressions, mostly in the northeastern portion of the basin or to the east of Madagascar. The first of these systems developed on 25 October 2010, which had its origins in the northeastern portion of the basin. On 29 November, the first named storm – Abele – also formed in the same area, strengthening to become one of the season's two tropical cyclones – storms with maximum sustained winds of at least 120 km/h (75 mph). The strongest system of the season was Cyclone Bingiza, which attained peak winds of 160 km/h (100 mph) off the northeastern coast of Madagascar in February. Bingiza was also the only storm to cause severe effects on land, causing heavy damage and 34 fatalities across Madagascar. Moderate Tropical Storm Cherono developed in March and traversed much of the ocean, only brushing by the island of Rodrigues. The final system was a subtropical depression that intensified south of Madagascar, becoming extratropical on 16 April to end the season.
- Die Zyklonsaison im Südwestindik 2010–2011 begann offiziell am 15. November 2010 und endete am 30. April 2011, mit Ausnahme von Mauritius und den Seychellen, wo sie erst am 15. Mai 2011 endete. Diese Daten begrenzen konventionell die Zeit des meteorologischen Jahres der Südhalbkugel, in denen sich im südwestlichen Indik die meisten tropischen Wirbelstürme bilden. Das erste tropische System bildete sich jedoch bereits am 25. Oktober 2010. Die tropischen Wirbelstürme in diesem Becken werden durch das Regional Specialized Meteorological Centre (RSMC) in La Réunion, Frankreich überwacht. Das Verantwortungsgebiet von Météo-France umfasst den Indischen Ozean südlich des Äquators und westlich von 90° östlicher Länge. Tropische Wirbelstürme in diesem Bereich werden Zyklone genannt. Das Joint Typhoon Warning Center (JTWC) in Honolulu beobachtet ebenfalls das Wettergeschehen in diesem Seegebiet; es gibt Sturmwarnungen aus, die sich primär an Einrichtungen der Streitkräfte der Vereinigten Staaten im Indischen Ozean richten.
- 2010－2011年西南印度洋熱帶氣旋季在2010年11月15日開始，並在2011年4月30日完結（某些地區的熱帶氣旋季在2011年5月15日完結）。 此文內容只包含在西南印度洋形成的熱帶氣旋的介紹。 風暴是由留尼汪氣象部發出報告。如果一個熱帶低氣壓在南緯0-40度，東經31-55度之間增強為中度熱帶風暴的話，馬達加斯加就會為它命名。如果一個熱帶低氣壓在南緯0-40度，東經55-90度之間增強為中度熱帶風暴的話，模里西斯就會為它命名。
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| - The 2010–11 South-West Indian Ocean cyclone season was the least active cyclone season on record in the basin, tied with 1982–83, producing only three systems of gale intensity. This was due to cooler than normal water temperatures and the Walker circulation – a broad atmospheric circulation – causing unusually moist conditions in the eastern Indian Ocean and unusually dry conditions in the western Indian Ocean. The basin includes the waters of the ocean south of the equator and west of 90º E to the eastern coast of Africa.
- 2010－2011年西南印度洋熱帶氣旋季在2010年11月15日開始，並在2011年4月30日完結（某些地區的熱帶氣旋季在2011年5月15日完結）。 此文內容只包含在西南印度洋形成的熱帶氣旋的介紹。 風暴是由留尼汪氣象部發出報告。如果一個熱帶低氣壓在南緯0-40度，東經31-55度之間增強為中度熱帶風暴的話，馬達加斯加就會為它命名。如果一個熱帶低氣壓在南緯0-40度，東經55-90度之間增強為中度熱帶風暴的話，模里西斯就會為它命名。
- Die Zyklonsaison im Südwestindik 2010–2011 begann offiziell am 15. November 2010 und endete am 30. April 2011, mit Ausnahme von Mauritius und den Seychellen, wo sie erst am 15. Mai 2011 endete. Diese Daten begrenzen konventionell die Zeit des meteorologischen Jahres der Südhalbkugel, in denen sich im südwestlichen Indik die meisten tropischen Wirbelstürme bilden. Das erste tropische System bildete sich jedoch bereits am 25. Oktober 2010.
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| - 2010~2011년 남서인도양 사이클론
- 2010–11 South-West Indian Ocean cyclone season
- 2010－2011年西南印度洋熱帶氣旋季
- Zyklonsaison im Südwestindik 2010–2011
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| - SWI
- South-West Indian Ocean
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| - --10-29
- --03-23
- --12-02
- --01-03
- --04-16
- --02-17
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![[RDF Data]](/fct/images/sw-rdf-blue.png)
