2011 North Indian Ocean cyclone season | |
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![]() Season summary map | |
Seasonal boundaries | |
First system formed | February 2, 2011 |
Last system dissipated | December 31, 2011 |
Strongest storm | |
Name | Thane |
• Maximum winds | 140 km/h (85 mph) (3-minute sustained) |
• Lowest pressure | 969 hPa (mbar) |
Seasonal statistics | |
Depressions | 10 |
Deep depressions | 6 |
Cyclonic storms | 2 |
Severe cyclonic storms | 1 |
Very severe cyclonic storms | 1 |
Total fatalities | 367 total |
Total damage | $603 million (2011 USD) |
Related articles | |
The 2011 North Indian Ocean cyclone season was the least active tropical cyclone season in the North Indian Ocean since 1993.[1] 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 season was the first season since 1993 where only two named storms formed. However, the systems that formed would cause damages of greater than $1.64 million USD and cause approximately 360 fatalities. It is believed that La Niña, a quasiperiodic climate pattern which causes a rise in surface pressure over the Indian Ocean, making the region drier, was the main cause for the below-active activity in the basin.[2]