1980–81 South Pacific Cyclone Season
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1980–81 South Pacific Cyclone Season
The 1980–81 South Pacific cyclone season was an above-average season. Seasonal summary This season marked the first time that the United States Joint Typhoon Warning Center issued warnings and performed best track analysis on significant tropical cyclones in the Southern Hemisphere. Systems Tropical Cyclone Diola Diola existed from November 27 to November 30. Severe Tropical Cyclone Arthur Arthur existed from January 11 to January 17. Tropical Cyclone Betsy Betsy existed from January 30 to February 4. Severe Tropical Cyclone Cliff Cliff developed on February 9, near Vanua Lava, Vanuatu. The cyclone reached peak intensity on February 12, with an estimated central pressure of 975 hPa. It passed over New Caledonia at near peak intensity, with sustained winds . After crossing into the Australian region, Cliff struck Queensland on February 14, making landfall near Bundaberg. The cyclone caused some crop and structural damages in South East Queensland, and beach erosion occ ...
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1978–79 South Pacific Cyclone Season
The 1978–79 South Pacific cyclone season ran year-round from July 1 to June 30. Tropical cyclone activity in the Southern Hemisphere reaches its peak from mid-February to early March. __TOC__ Systems Tropical Cyclone Fay Severe Tropical Cyclone Gordon Gordon developed on January 3 and left the basin on January 9. Tropical Cyclone Henry Henry existed from January 29 to February 5. Tropical Storm 11P This storm moved in the circular path, entering the basin on February 3 and returning to the Australian region on February 6. Tropical Cyclone Kerry Tropical Cyclone Kerry has the distinction of being the longest lived cyclone in the Australian region. It formed on February 13, 1979, and caused severe damage in the Solomon Islands. It then tracked across the Coral Sea making landfall near Mackay, Queensland on March 1 and dissipated on March 6. Its lowest pressure was 955hPa.Bureau of Meteorology (1992). ''Climate of Queensland'', Commonwealth of Australia Tropical ...
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1980 Atlantic Hurricane Season
The 1980 Atlantic hurricane season featured nine hurricanes, the most since 1969. The season officially began on June 1, 1980, and lasted until November 30, 1980. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic Ocean. The season was fairly active, with sixteen tropical cyclones forming, eleven of which intensified into a tropical storm. It was the first time since the 1971 season that there were no active tropical cyclones in the Atlantic basin during the month of June. The season occurred during an ENSO-neutral phase, having neither an El Niño nor a La Niña. Three tropical cyclones in the Atlantic Ocean in 1980 were notable. Hurricane Allen was the then-earliest Category 5 hurricane on record, reaching that intensity on August 5. The storm devastated portions of the Caribbean, Mexico, and the United States. Overall, Allen caused about $2.57 billion and at least 269 deaths. Tropical St ...
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South Pacific Cyclone Seasons
South is one of the cardinal directions or compass points. The direction is the opposite of north and is perpendicular to both east and west. Etymology The word ''south'' comes from Old English ''sūþ'', from earlier Proto-Germanic ''*sunþaz'' ("south"), possibly related to the same Proto-Indo-European root that the word ''sun'' derived from. Some languages describe south in the same way, from the fact that it is the direction of the sun at noon (in the Northern Hemisphere), like Latin meridies 'noon, south' (from medius 'middle' + dies 'day', cf English meridional), while others describe south as the right-hand side of the rising sun, like Biblical Hebrew תֵּימָן teiman 'south' from יָמִין yamin 'right', Aramaic תַּימנַא taymna from יָמִין yamin 'right' and Syriac ܬܰܝܡܢܳܐ taymna from ܝܰܡܝܺܢܳܐ yamina (hence the name of Yemen, the land to the south/right of the Levant). Navigation By convention, the ''bottom or down-facing side'' of a ...
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1980–81 South Pacific Cyclone Season
The 1980–81 South Pacific cyclone season was an above-average season. Seasonal summary This season marked the first time that the United States Joint Typhoon Warning Center issued warnings and performed best track analysis on significant tropical cyclones in the Southern Hemisphere. Systems Tropical Cyclone Diola Diola existed from November 27 to November 30. Severe Tropical Cyclone Arthur Arthur existed from January 11 to January 17. Tropical Cyclone Betsy Betsy existed from January 30 to February 4. Severe Tropical Cyclone Cliff Cliff developed on February 9, near Vanua Lava, Vanuatu. The cyclone reached peak intensity on February 12, with an estimated central pressure of 975 hPa. It passed over New Caledonia at near peak intensity, with sustained winds . After crossing into the Australian region, Cliff struck Queensland on February 14, making landfall near Bundaberg. The cyclone caused some crop and structural damages in South East Queensland, and beach erosion occ ...
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1981 North Indian Ocean Cyclone Season
The 1981 North Indian Ocean cyclone season was part of the annual cycle of tropical cyclone formation. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India. The official Regional Specialized Meteorological Centre in this basin is the India Meteorological Department, India Meteorological Department (IMD), while the Joint Typhoon Warning Center, Joint Typhoon Warning Center (JTWC) releases unofficial advisories. An average of five tropical cyclones form in the North Indian Ocean every season with peaks in May and November. Cyclones occurring between the meridians 45th meridian east, 45°E and 100th meridian east, 100°E are included in the season by the IMD. Systems There were 12 dep ...
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1980 North Indian Ocean Cyclone Season
The 1980 North Indian Ocean cyclone season was part of the annual cycle of tropical cyclone formation. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India. The official Regional Specialized Meteorological Centre in this basin is the India Meteorological Department (IMD), while the Joint Typhoon Warning Center (JTWC) releases unofficial advisories. An average of five tropical cyclones form in the North Indian Ocean every season with peaks in May and November. Cyclones occurring between the meridians 45°E and 100°E are included in the season by the IMD. __TOC__ Systems There were 14 depressions during the season. The first depression lasted from May 15–19, moving from the ...
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1981 Pacific Typhoon Season
The 1981 Pacific typhoon season was a slightly above average season that produced 29 tropical storms, 13 typhoons and two intense typhoons. The season ran throughout 1981, though most tropical cyclones typically develop between May and October.Gary PadgettMay 2003 Tropical Cyclone Summary. Retrieved 2007-01-05. The season's first named storm, Freda, developed on March 12 while the final storm, Lee, dissipated on December 29. Tropical cyclones only accounted for 12 percent of the rainfall in Hong Kong this season, the lowest percentage for the protectorate since 1972.Hong Kong Royal Observatory (1982)Meteorological Results 1981: Part III - Tropical Cyclone Summaries.Retrieved of 2008-11-10. The scope of this article is limited to the Pacific Ocean to the north of the equator between 100°E and 180th meridian. Within the northwestern Pacific Ocean, there are two separate agencies that assign names to tropical cyclones which can often result in a cyclone having two names. The ...
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1980 Pacific Typhoon Season
The 1980 Pacific typhoon season has no official bounds; it ran year-round in 1980, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. Tropical storms which formed in the entire west Pacific basin were assigned a name by the Joint Typhoon Warning Center. Tropical depressions that enter or form in the Philippine area of responsibility are assigned a name by the Philippine Atmospheric, Geophysical and Astronomical Services Administration or PAGASA. This can often result in the same storm having two names. A total of 28 tropical depressions formed this year in the Western Pacific, of which 24 became tropical storms. Beginning in March, tropical cyclones formed in each subsequent month through December. Of the 28, 15 storms reached typhoon intensity, of which 2 reached super typhoon strength. Seven tropical cyc ...
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1981 Pacific Hurricane Season
The 1981 Pacific hurricane season was a slightly below average Pacific hurricane season. The season officially started on May 15 in the eastern Pacific basin and June 1 in the central Pacific basin. Both basins' seasons ended on November 30; these dates conventionally delimit the period during which most tropical cyclones form in the northeastern Pacific Ocean. The first tropical cyclone of the season was designated on May 30, and the final storm of the season, Hurricane Otis, dissipated on October 30. The season produced fifteen named storms and a total of eight hurricanes, which was near normal. However, the total of one major hurricane was below the average of three. The strongest tropical cyclone of the season was Hurricane Norma, which was a powerful Category 3 hurricane on the Saffir–Simpson Hurricane Scale. The storm caused six deaths – five in Texas, and one in Mexico, due to severe flooding. Additionally, the storm caused $74 million (equivalent to $ m ...
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1980 Pacific Hurricane Season
The 1980 Pacific hurricane season officially started May 15, 1980, in the eastern Pacific and June 1, 1980, in the central Pacific, lasting until November 30, 1980. These dates conventionally delimit each year when most tropical cyclones form in the northeastern and central Pacific Ocean. This season was relatively uneventful; since no tropical cyclones made landfall, there were no reports of casualties or damage. Overall, the 1980 season was slightly below the long-term average, with 16 tropical cyclones forming. Of those, 15 were named, 7 reached hurricane intensity, and only 3 became major hurricanes by attaining category 3 status or higher on the Saffir–Simpson scale. All eastern Pacific systems this year formed in the eastern Pacific proper and two storms crossed into the central Pacific: Carmen from the west and Kay from the east. The season had an early start when Carmen crossed over the International Date Line in April. The strongest storm of this season is Hurricane ...
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1981 Atlantic Hurricane Season
The 1981 Atlantic hurricane season featured direct or indirect impacts from nearly all of its 12  tropical or subtropical storms. Overall, the season was fairly active, with 22 tropical depressions, 12 of which became a namable storm, while 7 of those reached hurricane status and 3 intensified into major hurricanes. The season officially began on June 1, 1981, and lasted until November 30, 1981. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. However, tropical cyclogenesis can occur before these dates, as demonstrated with the development of two tropical depressions in April and Tropical Storm Arlene in May. At least one tropical cyclone formed in each month between April and November, with the final system, Subtropical Storm Three, becoming extratropical on November 17, 1981. Although many tropical cyclones impacted land, few caused significant damage. Tropical Depression ...
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Bureau Of Meteorology
The Bureau of Meteorology (BOM or BoM) is an executive agency of the Australian Government responsible for providing weather services to Australia and surrounding areas. It was established in 1906 under the Meteorology Act, and brought together the state meteorological services that existed before then. The states officially transferred their weather recording responsibilities to the Bureau of Meteorology on 1 January 1908. History The Bureau of Meteorology was established on 1 January 1908 following the passage of the ''Meteorology Act 1906''. Prior to Federation in 1901, each colony had had its own meteorological service, with all but two colonies also having a subsection devoted to astronomy. In August 1905, federal home affairs minister Littleton Groom surveyed state governments for their willingness to cede control, finding South Australia and Victoria unwilling. However, at a ministerial conference in April 1906 the state governments agreed to transfer responsibility for m ...
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