cyclones are formed over the Pacific Ocean
Cyclone Yasi formed in the waters just off Fiji.
Cyclone Iggy did not hit Indonesia. It affected the coastal regions of Western Australia in 2012.
Cyclone Yasi formed on the 26th of January, 2011 in the Coral Sea off the coast of Queensland, Australia.
Cyclone Yasi formed as a tropical low in the Coral Sea, northeast of Queensland, Australia. It rapidly intensified into a Category 5 tropical cyclone before making landfall along the coast of Queensland in February 2011.
The Aila cyclone formed in the Bay of Bengal near the Andaman Islands before moving northward towards the coastlines of India and Bangladesh.
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Cyclone Yasi formed in the waters just off Fiji.
Cyclone Iggy did not hit Indonesia. It affected the coastal regions of Western Australia in 2012.
Cyclone Yasi formed on the 26th of January, 2011 in the Coral Sea off the coast of Queensland, Australia.
Cyclone Tracy hit Darwin, Northern Territory, Australia on the 25th of December 1974 but she had formed on the 20th.
Cyclone Selma formed in the southern Indian Ocean in late March 2018.
Cyclone Yasi formed as a tropical low in the Coral Sea, northeast of Queensland, Australia. It rapidly intensified into a Category 5 tropical cyclone before making landfall along the coast of Queensland in February 2011.
The Aila cyclone formed in the Bay of Bengal near the Andaman Islands before moving northward towards the coastlines of India and Bangladesh.
Yes. A cyclone is essentially an organized low-pressure system.
As with all cyclones, Cyclone Yasi was generated from a low pressure system out at sea some days earlier. The sea temperatures and weather conditions were simply right for a cyclone to be generated from the tropical low.
The Bhola Cyclone of 1970 formed over the central Bay of Bengal. It developed whenthe remnants of Tropical storm Nora which had broiled in the South China Sea moved over the Malay Peninsula and joined a depression in the Bay of Bengal, helping to intensify the depression into a cyclone.
Cyclone Yasi formed in the Coral Sea due to a combination of warm ocean waters, low wind shear, and favorable atmospheric conditions. These factors contributed to the development of a strong tropical cyclone that eventually made landfall in northeastern Australia in 2011.