2015 North Indian Ocean cyclone season | |
---|---|
Seasonal boundaries | |
First system formed | June 7, 2015 |
Last system dissipated | November 10, 2015 |
Strongest storm | |
Name | Chapala |
• Maximum winds | 215 km/h (130 mph) (3-minute sustained) |
• Lowest pressure | 940 hPa (mbar) |
Seasonal statistics | |
Depressions | 12 |
Deep depressions | 9 |
Cyclonic storms | 4 |
Severe cyclonic storms | 2 |
Very severe cyclonic storms | 2 |
Extremely severe cyclonic storms | 2 |
Super cyclonic storms | 0 |
Total fatalities | 380 total |
Total damage | > $1.04 billion (2015 USD) |
Related articles | |
The 2015 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 months of April and December, with the peak from May to 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. On average, three to four cyclonic storms form in this basin every season.[1]