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The 2010–11 Australian region cyclone season was a near average tropical cyclone season, with eleven tropical cyclones forming compared to an average of 12. The season was also the costliest recorded in the Australian region basin, with a total of $3.62 billion (2011 USD) in damages, mostly from the destructive Cyclone Yasi. [1]
The 2011–12 Australian region cyclone season was a below average tropical cyclone season, with 7 cyclones forming rather than the usual 11. It began on 1 November 2011, and ended on 14 May 2012. It began on 1 November 2011, and ended on 14 May 2012.
2011 Atlantic hurricane season; 2011 Pacific hurricane season; 2011 Pacific typhoon season; 2011 North Indian Ocean cyclone season; 2010–11 South-West Indian Ocean cyclone season; 2011–12 South-West Indian Ocean cyclone season; 2010–11 Australian region cyclone season; 2011–12 Australian region cyclone season; 2010–11 South Pacific ...
Each of three tropical cyclone warning centres (TCWCs) of the Bureau of Meteorology in Perth, Darwin and Brisbane used its own tropical cyclone naming list until the 2008–09 season, when the three TCWCs started to use the single Australian national naming list. From the 2020–21 season, the three TCWCs were unified into one single TCWC which ...
Ahead of the 2003 Pacific hurricane season, the NOAA forecasters decided to start issuing an experimental tropical cyclone outlook for the Eastern Pacific, which was designed not to be updated during the mid-season. [5] As a result of both the 2003 and 2004 outlooks being successful, the predictions became an operational product during 2005. [6]
The Atlantic hurricane season officially began on June 1, 2011. [21] It was an above average season in which twenty tropical cyclones formed. Nineteen of the twenty depressions attained tropical storm status, tied with 1887 , 1995 , 2010 , and later the 2012 season for the fourth-highest number of named storms since record-keeping began in 1851.
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Tropical cyclones are non-frontal, low-pressure systems that develop, within an environment of warm sea surface temperatures and little vertical wind shear aloft. [1] Within the Australian region, names are assigned from three pre-determined lists, to such systems, once they reach or exceed ten–minute sustained wind speeds of 65 km/h (40 mph), near the center, by either the Australian Bureau ...