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Until the start of the 1985–86 tropical cyclone season the basin only extended to 80°E, with the 10 degrees between 80 and 90E considered to be a part of the Australian region. [31] On average about 9 cyclones per year develop into tropical storms, while 5 of those go on to become tropical cyclones that are equivalent to a hurricane or a ...
The strongest cyclone on record in the Bay of Bengal was a super cyclonic storm in 1999, which made landfall on Paradeep, Odisha, in October 1999, with winds of 260 km/h (160 mph). [94] The cyclone killed 9,887 people across Odisha, with 1.6 million houses damaged or destroyed. [96] Damage was estimated at US$1.5 billion. [97]
A tropical cyclone is the generic term for a warm-cored, non-frontal synoptic-scale low-pressure system over tropical or subtropical waters around the world. [4] [5] The systems generally have a well-defined center which is surrounded by deep atmospheric convection and a closed wind circulation at the surface. [4]
Map shows path of cyclone Chido (Mateo France) Hundreds of poor people living in shacks with sheet metal roofs were hit especially hard as the storm tore up many of their homes.
During four years (1887, [48] 1953, [49] 2003, and 2007), tropical cyclones formed in the North Atlantic Ocean both during or before May and during December. [ 50 ] 1887 holds the record for being the year with the most storms outside the hurricane season, with four off-season storms having occurred during it. [ 48 ]
Some agencies provide track storms in their immediate vicinity, [42] while others cover entire ocean basins. One can choose to track one storm per map, use the map until the table is filled, or use one map per season. Some tracking charts have important contact information in case of an emergency or to locate nearby hurricane shelters. [9]
According to the National Hurricane Center, there have been an estimated 42 tropical cyclones that have reached Category 5 status in the Atlantic Basin since 1924 — the most recent being ...
Tropical cyclones develop or strengthen when water evaporated from the ocean is released as the saturated air rises, resulting in condensation of water vapor contained in the moist air. They are fueled by a different heat mechanism than other cyclonic windstorms such as nor'easters , European windstorms , and polar lows .