When Cyclone Larry hit Australia in 2006, the lithosphere, which is the solid outer layer of the Earth, remained largely unaffected. Cyclones mainly impact the atmosphere and hydrosphere, causing high winds, heavy rainfall, and flooding, but they do not cause significant changes to the lithosphere itself.
Cyclone Larry was a Category 5 tropical cyclone, which made landfall in Australia on March 20, 2006. It had wind gusts estimated to be reaching up to 290 km/h (180 mph) and caused significant damage in the areas it impacted.
Cyclone Larry made landfall in north Queensland, Australia near the town of Innisfail on March 20, 2006. It caused significant damage to the area, including destroying homes, crops, and infrastructure.
The name Larry was given to the cyclone by the Fiji Meteorological Service. In the South Pacific region, cyclones are named by designated meteorological authorities. The name Larry was chosen from a list of pre-determined names for the season.
Cyclones are essentially caused by a combination of warm ocean temperatures, high humidity and low wind shear, which means differences in wind velocity and direction at different heights. If the wind shear is high, it can pull a cyclone apart. Low wind shear increases the chances of the cyclone developing. Cyclone Larry was caused by these factors, in particular, the warm waters of the Coral Sea, where it formed.
Cyclone Wanda itself caused no deaths. It was a relatively low-category cyclone (the actual category does not seem to be recorded anywhere) but its beiggest claim to fame was the amount of rain it dumped on the Brisbane catchment area, contributing significantly to the Brisbane floods of January 1974. These floods resulted in 14 deaths.
Cyclone Larry hit the north coast of Queensland.
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Cyclone Larry, which hit Australia in 2006, made landfall near Innisfail in far North Queensland.
Cyclone Larry was a Category 5 tropical cyclone, which made landfall in Australia on March 20, 2006. It had wind gusts estimated to be reaching up to 290 km/h (180 mph) and caused significant damage in the areas it impacted.
Cyclone Larry crossed the Queensland coast on 7 April 2006.
Cyclone Larry made landfall in north Queensland, Australia near the town of Innisfail on March 20, 2006. It caused significant damage to the area, including destroying homes, crops, and infrastructure.
Cyclone Larry made landfall near Innisfail in north Queensland, Australia on March 20, 2006. It then tracked southwestward across inland Queensland before dissipating. The cyclone caused significant damage to crops, infrastructure, and homes in the region.
Cyclone Larry, like all cyclones, began as a low pressure system, and it first began to be monitored by Australia's Bureau of Meteorology as a low pressure system on 16 March 2006. It developed into a cyclone two days later, on 18 March.Cyclone Larry then crossed the Queensland coast between between 6:20am and 7:20am on 20 March 2006.
In the 2006's many things occurred such as: Saddam Hussein was charged with crimes against humanity and Cyclone Larry reached Australia.
cyclone Larry damage alot of netrual evironments and they are: trees, bridges, farm, land, animals.
The name Larry was given to the cyclone by the Fiji Meteorological Service. In the South Pacific region, cyclones are named by designated meteorological authorities. The name Larry was chosen from a list of pre-determined names for the season.
Cyclones are essentially caused by a combination of warm ocean temperatures, high humidity and low wind shear, which means differences in wind velocity and direction at different heights. If the wind shear is high, it can pull a cyclone apart. Low wind shear increases the chances of the cyclone developing. Cyclone Larry was caused by these factors, in particular, the warm waters of the Coral Sea, where it formed.