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List Of Off-season Australian Region Tropical Cyclones
An off-season Australian region tropical cyclone, Australian tropical cyclone is a tropical cyclone that existed in the Australian Region, between 90°E and 160°E, outside of the official season. The World Meteorological Organization currently defines the season as occurring between 1 November and 30 April, of the following year, which is when the majority of all tropical cyclones exist. During the off-season, systems are more likely to either develop during or persist until May, with approximately 52% of such storms occurring during that month. Occasionally, however, storms develop in October, with approximately 34% of such storms occurring during that month. As of 2022, there have been 94 tropical cyclones known to have occurred off-season. Off-season cyclones are most likely to occur in the Coral Sea, with most affecting land in some way. Cumulatively, at least 4 deaths occurred due to the storms, the most recent off-season storm was a Tropical Cyclone 01U in July 2022. Syste ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cyclone Carol (1976)
In meteorology, a cyclone () is a large air mass that rotates around a strong center of low atmospheric pressure, counterclockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere as viewed from above (opposite to an anticyclone). Cyclones are characterized by inward-spiraling winds that rotate about a zone of low pressure. The largest low-pressure systems are polar vortices and extratropical cyclones of the largest scale (the synoptic scale). Warm-core cyclones such as tropical cyclones and subtropical cyclones also lie within the synoptic scale. Mesocyclones, tornadoes, and dust devils lie within smaller mesoscale. Upper level cyclones can exist without the presence of a surface low, and can pinch off from the base of the tropical upper tropospheric trough during the summer months in the Northern Hemisphere. Cyclones have also been seen on extraterrestrial planets, such as Mars, Jupiter, and Neptune. Cyclogenesis is the process of cyclone formation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cyclone Lisa (1991)
In meteorology, a cyclone () is a large air mass that rotates around a strong center of low atmospheric pressure, counterclockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere as viewed from above (opposite to an anticyclone). Cyclones are characterized by inward-spiraling winds that rotate about a zone of low pressure. The largest low-pressure systems are polar vortices and extratropical cyclones of the largest scale (the synoptic scale). Warm-core cyclones such as tropical cyclones and subtropical cyclones also lie within the synoptic scale. Mesocyclones, tornadoes, and dust devils lie within smaller mesoscale. Upper level cyclones can exist without the presence of a surface low, and can pinch off from the base of the tropical upper tropospheric trough during the summer months in the Northern Hemisphere. Cyclones have also been seen on extraterrestrial planets, such as Mars, Jupiter, and Neptune. Cyclogenesis is the process of cyclone formation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tropical Storm 02S (1989)
The tropics are the regions of Earth surrounding the Equator. They are defined in latitude by the Tropic of Cancer in the Northern Hemisphere at N and the Tropic of Capricorn in the Southern Hemisphere at S. The tropics are also referred to as the tropical zone and the torrid zone (see geographical zone). In terms of climate, the tropics receive sunlight that is more direct than the rest of Earth and are generally hotter and wetter as they aren't affected as much by the solar seasons. The word "tropical" sometimes refers to this sort of climate in the zone rather than to the geographical zone itself. The tropical zone includes deserts and snow-capped mountains, which are not tropical in the climatic sense. The tropics are distinguished from the other climatic and biomatic regions of Earth, which are the middle latitudes and the polar regions on either side of the equatorial zone. The tropics constitute 40% of Earth's surface area and contain 36% of Earth's landmass. , t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
1989–90 Australian Region Cyclone Season
The 1989–90 Australian region cyclone season was an above average tropical cyclone season. It was also an event in the ongoing cycle of tropical cyclone formation. It ran from 1 November 1989 to 30 April 1990. The regional tropical cyclone operational plan also defines a ''tropical cyclone year'' separately from a ''tropical cyclone season'', and the "tropical cyclone year" ran from 1 July 1989 to 30 June 1990. Tropical cyclones in this area were monitored by four Tropical Cyclone Warning Centres (TCWCs): the Bureau of Meteorology (Australia), Australian Bureau of Meteorology in Perth, Western Australia, Perth, Darwin, Northern Territory, Darwin, and Brisbane, Queensland, Brisbane; and TCWC Port Moresby in Papua New Guinea. Seasonal summary ImageSize = width:825 height:205 PlotArea = top:10 bottom:80 right:20 left:20 Legend = columns:3 left:30 top:58 columnwidth:270 AlignBars = early DateFormat = dd/mm/yyyy Period = from:01/07/1989 till:01/05/1990 TimeAxis = orientation:horiz ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cyclone Meena (1989)
Severe Tropical Cyclone Meena was the first of four tropical cyclones to impact the Cook Islands during February 2005. The system was first identified within a trough of low pressure, about to the northwest of Pago Pago in American Samoa. Meteorological history During February 1, an area of low pressure was identified within a trough of low pressure, about to the northwest of Pago Pago in American Samoa. During that day, the system moved south-westwards and started to consolidate, before the Fiji Meteorological Service (FMS) classified the system as Tropical Depression 07F. At this stage, the depression was poorly organised with atmospheric convection displaced to the north of the systems low level circulation center, while it was located to the south of a ridge of high pressure in an area of moderate vertical wind shear. Over the next day, the system's organisation significantly improved with the development of a small central dense overcast, while its outflow was enhanced ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cyclone Namu
Severe Tropical Cyclone Namu was considered to be one of the worst tropical cyclones to impact the Solomon Islands on record, after it caused over 100 deaths within the island nations. It was first noted as a weak tropical depression to the north of the Solomon Islands during May 15, 1986. Over the next couple of days, the system Located north of the Solomon Islands, the storm steadily intensified while meandering. After briefly moving west, the storm attained Category 2 intensity on the Australian intensity scale on May 18, as it moved through the island chain on the next day. Cyclone Namu attained peak intensity of . After retaining its peak intensity for a day, Namu turned south and weakened steadily. By May 21, the winds of Cyclone Namu had been reduced to only . Continuing to weaken, Namu turned east and dissipated on May 22, away from the island chain. The system impacted the Solomon Islands, Vanuatu and New Caledonia and caused over 100 deaths, as well as varying amount ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cyclone Billy-Lila (1986)
In meteorology, a cyclone () is a large air mass that rotates around a strong center of low atmospheric pressure, counterclockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere as viewed from above (opposite to an anticyclone). Cyclones are characterized by inward-spiraling winds that rotate about a zone of low pressure. The largest low-pressure systems are polar vortices and extratropical cyclones of the largest scale (the synoptic scale). Warm-core cyclones such as tropical cyclones and subtropical cyclones also lie within the synoptic scale. Mesocyclones, tornadoes, and dust devils lie within smaller mesoscale. Upper level cyclones can exist without the presence of a surface low, and can pinch off from the base of the tropical upper tropospheric trough during the summer months in the Northern Hemisphere. Cyclones have also been seen on extraterrestrial planets, such as Mars, Jupiter, and Neptune. Cyclogenesis is the process of cyclone formation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cyclone Oscar (1983)
Severe Tropical Cyclone Oscar was one of the worst tropical cyclones to affect Fiji. The system was first noted as a shallow depression on 23 February, while it was located to the north of Fiji's capital Suva. The system subsequently developed further as it moved westwards and was named as Tropical Cyclone Oscar during the next day. Over the next few days Oscar subsequently intensified as it moved westwards and gradually developed further and equivalent to a Category 3 severe tropical cyclone, on the modern day Australian tropical cyclone intensity scale during 27 February. The system subsequently turned and started to move south-eastwards towards Fiji. Meteorological history On 23 February, the Fiji Meteorological Service (FMS) started to monitor a shallow depression, that had developed about to the north-northwest of Suva, Fiji. The system subsequently developed further as it moved westwards and was declared a tropical cyclone and named Oscar by the FMS during February 24. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cyclone Naomi (1983)
In meteorology, a cyclone () is a large air mass that rotates around a strong center of low atmospheric pressure, counterclockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere as viewed from above (opposite to an anticyclone). Cyclones are characterized by inward-spiraling winds that rotate about a zone of low pressure. The largest low-pressure systems are polar vortices and extratropical cyclones of the largest scale (the synoptic scale). Warm-core cyclones such as tropical cyclones and subtropical cyclones also lie within the synoptic scale. Mesocyclones, tornadoes, and dust devils lie within smaller mesoscale. Upper level cyclones can exist without the presence of a surface low, and can pinch off from the base of the tropical upper tropospheric trough during the summer months in the Northern Hemisphere. Cyclones have also been seen on extraterrestrial planets, such as Mars, Jupiter, and Neptune. Cyclogenesis is the process of cyclone formation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cyclone Claudia (1982)
The name Claudia has been used for five tropical cyclones in the Eastern Pacific Ocean: * Tropical Storm Claudia (1962), crossed over the western portion of the Baja California peninsula, moved over water, and again struck the peninsula before dissipating * Tropical Storm Claudia (1965), never affected land * Tropical Storm Claudia (1969), downgraded to a depression only 24 hours after first becoming a tropical storm; did not make landfall * Tropical Storm Claudia (1973), made landfall approximately 30 mi (50 km) east of Acapulco; no deaths or casualties were reported * Hurricane Claudia (1977), did not make a landfall The name Claudia has also been used three times in the Australian region: * Cyclone Claudia (1982) * Cyclone Claudia (2002) (14P), did not make a landfall * Cyclone Claudia (2020), brought heavy rainfall to Darwin The name Claudia also was used to name a storm in the South-West Indian Ocean basin: * Cyclone Claudia (2012), did not make a landfall {{ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cyclone Alex (1981)
In meteorology, a cyclone () is a large air mass that rotates around a strong center of low atmospheric pressure, counterclockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere as viewed from above (opposite to an anticyclone). Cyclones are characterized by inward-spiraling winds that rotate about a zone of low pressure. The largest low-pressure systems are polar vortices and extratropical cyclones of the largest scale (the synoptic scale). Warm-core cyclones such as tropical cyclones and subtropical cyclones also lie within the synoptic scale. Mesocyclones, tornadoes, and dust devils lie within smaller mesoscale. Upper level cyclones can exist without the presence of a surface low, and can pinch off from the base of the tropical upper tropospheric trough during the summer months in the Northern Hemisphere. Cyclones have also been seen on extraterrestrial planets, such as Mars, Jupiter, and Neptune. Cyclogenesis is the process of cyclone formation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
