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Hurricane Charlie
The name Charley or Charlie has been used for eight tropical cyclones and one subtropical cyclone in the Atlantic Ocean, and for one tropical cyclone in the Australian region of the South Pacific Ocean. In the Atlantic: * Hurricane Charlie (1950), Category 2 hurricane that did not affect land * Hurricane Charlie (1951), Category 4 hurricane that struck Jamaica, the Yucatán Peninsula, and northeastern Mexico. * Hurricane Charlie (1952), struck the Dominican Republic as a tropical storm before strengthening to a Category 3 hurricane and moving out to sea * Subtropical Storm Charlie (1972), remained over the open ocean * Hurricane Charley (1980), Category 1 hurricane that looped across the open ocean * Hurricane Charley (1986), Category 1 hurricane that made landfall along the North Carolina coast, then moved out over the ocean, going on to hit Ireland and Great Britain as a strong extratropical storm * Hurricane Charley (1992), Category 2 hurricane, ...
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Tropical Cyclone
A tropical cyclone is a rapidly rotating storm system characterized by a low-pressure center, a closed low-level atmospheric circulation, strong winds, and a spiral arrangement of thunderstorms that produce heavy rain and squalls. Depending on its location and strength, a tropical cyclone is referred to by different names, including hurricane (), typhoon (), tropical storm, cyclonic storm, tropical depression, or simply cyclone. A hurricane is a strong tropical cyclone that occurs in the Atlantic Ocean or northeastern Pacific Ocean, and a typhoon occurs in the northwestern Pacific Ocean. In the Indian Ocean, South Pacific, or (rarely) South Atlantic, comparable storms are referred to simply as "tropical cyclones", and such storms in the Indian Ocean can also be called "severe cyclonic storms". "Tropical" refers to the geographical origin of these systems, which form almost exclusively over tropical seas. "Cyclone" refers to their winds moving in a circle, whirling ...
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Subtropical Cyclone
A subtropical cyclone is a weather system that has some characteristics of both tropical and an extratropical cyclone. As early as the 1950s, meteorologists were uncertain whether they should be characterized as tropical or extratropical cyclones. They were officially recognized and titled by the National Hurricane Center in 1972. Beginning in 2002, subtropical cyclones received names from the official tropical cyclone lists in the North Atlantic, South-west Indian Ocean, and South Atlantic basins. There are two definitions currently used for subtropical cyclones depending on their location. Across the north Atlantic and southwest Indian Ocean, they require some central convection fairly near the center surrounding a warming core existing in the mid-levels of the troposphere. Across the eastern half of the northern Pacific however, they require a mid-tropospheric cyclone to be cut off from the main belt of the westerlies and with only a weak surface circulation. Subtropical cy ...
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Hurricane Charlie (1950)
The 1950 Atlantic hurricane season was the first year in the Atlantic hurricane database (HURDAT) that storms were given names in the Atlantic basin. Names were taken from the Joint Army/Navy Phonetic Alphabet, with the first named storm being designated "Able", the second "Baker", and so on. It was a very active season with sixteen tropical storms, with eleven of them developing into hurricanes. Six of these hurricanes were intense enough to be classified as major hurricanes—a denomination reserved for storms that attained sustained winds equivalent to a Category 3 or greater on the present-day Saffir–Simpson scale. One storm, the twelfth of the season, was unnamed and was originally excluded from the yearly summary, and three additional storms were discovered in re-analysis. The large quantity of strong storms during the year yielded, prior to modern reanalysis, what was the highest seasonal accumulated cyclone energy (ACE) of the 20th century in the Atlantic basin; 1 ...
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Hurricane Charlie (1951)
Hurricane Charlie was the deadliest tropical cyclone of the 1951 Atlantic hurricane season. The third named storm, second hurricane, and second major hurricane of the season, it developed from a tropical wave east of the Lesser Antilles. It moved briskly west-northwest, passing between the islands of Dominica and Guadeloupe. It strengthened to a hurricane in the eastern Caribbean Sea, and it struck Jamaica with winds near Category 3 intensity. It strengthened to a peak intensity of 130 mph (215 km/h) prior to landfall on Quintana Roo, Yucatán Peninsula. It weakened over land, and it re-strengthened over the Gulf of Mexico before it made a final landfall near Tampico. In its path, Charlie caused more than 250 deaths. The hurricane produced Jamaica's deadliest natural disaster of the 20th century, causing more than 152 deaths and $50,000,000 in damages. The hurricane was described as Tampico's worst tropical cyclone since 1936, and it caused more than 100 fatalities ...
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Hurricane Charlie (1952)
The 1952 Atlantic hurricane season was the last Atlantic hurricane season in which tropical cyclones were named using the Joint Army/Navy Phonetic Alphabet. It was a near normal Atlantic hurricane season, although it was the least active since 1946. The season officially started on June 15; however, a pre-season unnamed storm formed on Groundhog Day, becoming the only storm on record in the month of February. The other six tropical cyclones were named using the Joint Army/Navy Phonetic Alphabet, the first of which formed on August 18. The final storm of the season dissipated on October 28, two and a half weeks before the season officially ended on November 15. Four of the tropical cyclones made landfall during the season, the first being the February tropical storm that crossed southern Florida. The first hurricane, named Able, struck South Carolina with winds of , causing heavy damage near the coast and widespread power outages. It moved up most of the Ea ...
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Subtropical Storm Charlie (1972)
The 1972 Atlantic hurricane season was a significantly below average season, having only seven named storms, four fully tropical storms (the fewest since 1930) and three subtropical storms. It officially began on June 1, 1972, and lasted until November 30, 1972. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. The first storm, Subtropical Storm Alpha, developed on May 23 off the Southeast United States and struck Florida, causing minor damage and two fatalities. Although several other tropical depressions developed, only Tropical Depression Five is known to have affected land. The most significant storm of the season was Hurricane Agnes, which at the time was the costliest United States hurricane, until Frederic in 1979. After brushing the western tip of Cuba, the hurricane made landfall on the Florida Panhandle. It caused at least $2.1 billion (1972  USD) in damage and 137 fatal ...
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Hurricane Charley (1980)
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 S ...
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Hurricane Charley (1986)
Hurricane Charley was the second hurricane to threaten the East Coast of the United States within a year's timeframe, after Hurricane Gloria of 1985. The third tropical storm and second hurricane of the season, Charley formed as a subtropical low on August 13 along the Florida panhandle. After moving off the coast of South Carolina, the system transitioned into a tropical cyclone and intensified into a tropical storm on August 15. Charley later attained hurricane status before moving across eastern North Carolina. It gradually weakened over the north Atlantic Ocean before transitioning into an extratropical cyclone on August 20. Charley's remnants remained identifiable for over a week, until after crossing Ireland and Great Britain they dissipated on August 30. The storm brought light to moderate precipitation to much of the southeastern United States. In Georgia and South Carolina, the rainfall alleviated drought conditions. In North Carolina, where the hurri ...
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Hurricane Charley (1992)
The 1992 Atlantic hurricane season was a significantly below average season, but it did feature Hurricane Andrew, the costliest Atlantic hurricane known at the time, surpassing Hugo of 1989 and later surpassed by Katrina of 2005. The season officially began on June 1, 1992, and lasted until November 30, 1992. The first storm, an unnamed subtropical storm, developed in the central Atlantic on April 21, over a month before the official start of hurricane season. On August 16, Hurricane Andrew formed and would later strike the Bahamas, as well U.S. States of Florida and Louisiana, becoming the costliest Atlantic hurricane on record until the record was surpassed just over 13 years later. Andrew caused $27.3 billion (1992 USD) in damage, mostly in Florida, as well as 65 fatalities. In addition, Andrew was also the strongest hurricane of the season, reaching winds of while approaching Florida. Later in the season, just under one month after Andrew struck land three times, Hurrica ...
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Tropical Storm Charley (1998)
Tropical Storm Charley was the third named storm of the 1998 Atlantic hurricane season. Charley was the first of two tropical storms to make landfall in Texas during that season (Frances being the other). The storm originated with a tropical wave that moved off the West African coast on August 9. The wave moved generally west-northwestward, producing occasional bursts of convection, finally arriving in the southeastern Gulf of Mexico by August 19, when animated satellite images began to indicate it had possibly developed a low pressure centre. Hurricane Hunter investigations into the system the next day revealed that this was not the case. The system lingered for two days, lacking an organized low level centre of circulation until early on the morning of August 21, when advisories were initiated on the tropical depression, east of Brownsville, Texas. The depression became a tropical storm later that day, as it moved steadily west-northwestward, strengthening, and then weakening a ...
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Hurricane Charley
Hurricane Charley was the first of four separate hurricanes to impact or strike Florida during 2004, along with Frances, Ivan and Jeanne, as well as one of the strongest hurricanes ever to strike the United States. It was the third named storm, the second hurricane, and the second major hurricane of the 2004 Atlantic hurricane season. Charley lasted from August 9 to 15, and at its peak intensity it attained winds, making it a strong Category 4 hurricane on the Saffir–Simpson scale. It made landfall in Southwest Florida at maximum strength, making it the strongest hurricane to hit the United States since Hurricane Andrew struck Florida in 1992 and at the time the strongest hurricane to hit southwest Florida in recorded history until Hurricane Ian in 2022. After moving slowly through the Caribbean, Charley crossed Cuba on Friday, August 13 as a Category 3 hurricane, causing heavy damage and four deaths. That same day, it crossed over the Dry Tortugas, just 2 ...
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Cyclone Charlie (1988)
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 ...
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