the-french-artist/wikipedia_20220301.simple_sentence_embeddings huggingface dataset:
Gaelic football 
 Gaelic football is played by teams of 15 on a rectangular grass pitch with H-shaped goals at each end.
Gaelic football 
 The object is to score by kicking/striking the ball with your hand and getting it through the goals.
Gaelic football 
 Players advance the ball up the field with a combination of carrying, soloing (dropping and then toe-kicking the ball upward into the hands), kicking, and hand-passing to their team-mates.
Gaelic football 
 Gaelic football is one of four Gaelic Games run by the Gaelic Athletic Association, the largest sporting organization in Ireland.
Gaelic football 
 The game is believed to have come from ancient Irish football known as caid which dates back to 1537, although the modern game took shape in 1887.
Gaelic football 
 The same pitch is used for hurling; the GAA, which organizes both sports, decided this to facilitate dual usage.
Gaelic football 
 All Gaelic football matches last for 60 minutes, divided into two halves of thirty minutes, with the exception of senior inter-county games which last for 70 minutes (two halves of 35 minutes).
Gaelic football 
 Teams consist of fifteen players (a goalkeeper, two corner backs, a full back, three half backs, two mid fielders, three half forwards, two corner forwards and a full forward) plus up to fifteen substitutes, of which five may be used.
Gaelic football 
 Each player is numbered 1–15, starting with the goalkeeper, who must wear a different coloured jersey.
Gaelic football 
 The game is played with a round leather football, similar to a soccer ball, but heavier, and with horizontal stitching rather than the hexagon and pentagon panels often used on soccer balls, and similar to a standard volleyball.
Caid (sport) 
 Some people believe that caid has influenced the modern sport of Gaelic football the rules of which were officially published in 1887.
Caid (sport) 
 The first recorded mention of football in Ireland was in 1308, when John McCrocan, a spectator at a football game was charged with accidentally stabbing a player named William Bernard.
Caid (sport) 
 Football games are mentioned in the Statute of Galway, 1527, which allowed the playing of football and archery, but banned "hokie" – the hurling of a little ball with sticks or staves, as well as other sports.
Caid (sport) 
 There is some evidence that caid was taken around the world by the Irish diaspora, and that it may have influenced the development of Australian rules football, although this is controversial.
Longue paume 
 It was part of the Paris 1900 Summer Olympics, but not all think that the medals that were awarded  for longue paume at that Olympics have full value.
Longue paume 
 The governing body of the sport is the Fédération Française de Longue Paume with its headquarter in Amiens.
Pallone 
 Pallone (Italian for an inflated ball, similar to the word balloon) is the name of several traditional ball games, played in various regions of Italy, with minimal differences in regulations.
Pallone 
 Pallone col bracciale was particularly popular throughout Italy in the 18th century then in 19th century and 20th century until 1930 was the most popular sport of ancient Italian national sports; its first official regulations date back to 1555.
Pallone 
 The pallone col bracciale players are called pallonisti and during 19th century Italian professional pallonisti were richest and best rewarded sportsmen of all the world.
Pallone 
 This sport and his champions were described by Johann Wolfgang von Goethe, Giacomo Leopardi, Edmondo de Amicis, Antonio Francesco Grazzini, Ottavio Rinuccini, Gabriello Chiabrera, Tommaso Grossi, Giuseppe Gioachino Belli.
Pallone 
 Balls are struck back and forth with a wooden cylinder, called bracciale, worn over the forearm, if carelessly played, a broken arm can result: in fact bracciale weighs 2 or 1 kilogram.
Pallone 
 A special feature is that the ball is put into play by a designated server, who otherwise is not part of the game.
Pallone 
 Registered players of official championships dispute their matches in a kind of stadium named sferisterio or sferodromo in Italian language.
Pallone 
 Nowadays they play two forms of this sport: 3 players a side with lateral wall and 4 players a side in open playing field without lateral wall.
Pallone 
 Pallapugno, one time named pallone elastico, is a game from Piedmont and Liguria and it is played with a bandaged fist; rubber ball has diameter of 10,5
Pallone 
 Scoring is also by fifteens, but in this version a second bounce can result in a "chase" rather than an outright point, similar to real tennis.
Pallone 
 Professional players dispute their matches in sferisterio 90 metres long and 18 metres large with lateral wall.
Pallone 
 Pallapugno leggera is played in courtfield which has same size of volleyball's courtfield without net (device).
Pallone 
 First action of every match consisted of shot pushing up the ball for rebound on a roof called pantalera in Piedmontese language.
Pallone 
 Pallonetto or pallonetto ligure al lungo is generally played on the urban streets with tennis balls without covering felt.
Pallone 
 Playing field is long between 60 and 90 metres and it's large 18 metres with or without lateral wall.
Palla 
 In Italian they also call pallacanestro for basketball, pallavolo for volleyball, pallamano for handball and pallanuoto for water polo.
Palla 
 The game is played by facing teams who strike, not catch, the ball with either a bare or gloved hand: every team include 3, 4 or 5 athletes.
Palla 
 Courts are marked out with painted lines on town streets, but there is no net, and players can move between sides.
Palla 
 Similar to real tennis, a second bounce can result in a "chase" rather than an outright point, marked in chalk where the ball stops rolling.
Palla 
 Palla elastica is a team game: every team include 5 athletes who catch a rubber ball,  similar to tennis ball, with either a bare hand.
Palla 
 Registered players of official championships dispute their matches in a kind of stadium, 75 metres long with lateral wall, named sferisterio or sferodromo in Italian language.
Palla 
 Pallacorda or palla della corda is the Italian name of ancient form of real tennis where a cord of rope was strung across the street and players used hands, racket or tamburello alias tambourine in English language.
Palla 
 Pisa, Prato, Rome, Siena, and various Tuscan towns still have streets named via Pallacorda or via Della Corda.
Palla 
 Pallamaglio is an other ancient game called pall mall in English language and his modern form named skittles is played in England, Germany, Austria and Switzerland currently.
Palla 
 Pallina means small ball and it is a team game: every team include 4, 5 or 6 athletes who catch a rubber ball, of almost 50 grams, with either a bare hand.
Pellet 
 Pellet is a term used for a small particle or grain, typically one created by compressing an original material.
Pellet 
 Bird pellets are the round balls of undigested matter that some bird species occasionally regurgitate
Storm history of Hurricane Katrina 
 Hurricane Katrina was a highly destructive Category 5 hurricane which formed as Tropical Depression Twelve near the Bahamas.
Storm history of Hurricane Katrina 
 Katrina continued on to make landfall on the southern part of the U.S. state of Florida as a Category 1 hurricane.
Storm history of Hurricane Katrina 
 However, the warm waters of the Gulf of Mexico allowed it to rapidly intensify to the sixth strongest Atlantic hurricane in recorded history.
Storm history of Hurricane Katrina 
 Afterwards, Katrina made landfall as a Category 3 hurricane near Buras-Triumph, Louisiana, and once more near the Mississippi/Louisiana border.
Storm history of Hurricane Katrina 
 Katrina did not stop going northward through the central United States and finally dissipated near the Great Lakes, where it was absorbed by a cold front.
Storm history of Hurricane Katrina 
 Tropical Depression Twelve formed over the southeastern Bahamas at 5:00 p.m. EDT (2100 UTC) on August 23, 2005, some of the tropical depression was from the remains of Tropical Depression Ten, which had dissipated from the effects of a nearby upper tropospheric trough.
Storm history of Hurricane Katrina 
 While the normal standards for numbering tropical depressions in the Atlantic shows that the old name/number is kept when a depression dissipates and regenerates, satellite data indicated that a second tropical wave combined with Tropical Depression Ten north of Puerto Rico to form a new, much more advanced system, which was then named as Tropical Depression Twelve.
Storm history of Hurricane Katrina 
 Simultaneously, the trough in the upper troposphere weakened, causing the wind shear in the area to decrease, also allowing the new tropical depression to develop.
Storm history of Hurricane Katrina 
 In a later re-analysis, it was found that the low-level circulation of TD Ten had completely detached and dissipated, with only the remnant mid-level circulation moving on and merging with the second tropical wave mentioned before.
Storm history of Hurricane Katrina 
 As the atmospheric conditions surrounding Tropical Depression Twelve were good for tropical development, the system began to strengthen, was upgraded to Tropical Storm status and given the name Katrina on the morning of August 24.
Storm history of Hurricane Katrina 
 A burst of convection allowed Katrina to become the fifth hurricane of the 2005 season on August 25, only two hours before it made landfall around 6:30 p.m. EST (2230 UTC) between Hallandale Beach and Aventura, Florida.
Storm history of Hurricane Katrina 
 Katrina struck the peninsula at a high speed with 80 mph (130 km/h) winds, and had a well-defined eye on Doppler radar, which managed to stay undisturbed throughout its passage over Florida.
Storm history of Hurricane Katrina 
 The storm weakened over land on August 26 to a tropical storm, but regained its strength as a hurricane at 2:00 a.m. EDT (0600 UTC), about one hour after making landfall in Florida.
Storm history of Hurricane Katrina 
 Parts of the Florida Keys experienced tropical storm force winds throughout August 26, with the Dry Tortugas briefly experiencing hurricane-force winds.
Storm history of Hurricane Katrina 
 At first, the National Hurricane Center forecasts predicted that Katrina would begin turning northward after landfall, eventually to make its second landfall on the Florida Panhandle about three to four days later.
Storm history of Hurricane Katrina 
 Katrina, however, continued a westerly and west-southwesterly track, which eventually made the forecasts change their predictions, and forecast Katrina to move westward into New Orleans.
Storm history of Hurricane Katrina 
 Right after the storm entered the Gulf of Mexico, the low wind shear, good upper-level outflow, and the warm sea surface temperatures of the Gulf Loop Current caused Katrina to intensify rapidly.
Storm history of Hurricane Katrina 
 On August 27, the storm was upgraded to Category 3 strength, becoming the third major hurricane of the season.
Storm history of Hurricane Katrina 
 An eyewall replacement cycle inhibited strengthening of its maximum winds for about 18 hours, but nearly doubled the size of the storm as a result.
Storm history of Hurricane Katrina 
 The storm then began a second period of rapid intensification starting at 7:00 p.m. CDT on August 27, and by 12:40 a.m. CDT on August 28, Katrina was upgraded to a Category 4 hurricane with maximum sustained winds of 145 mph (233 km/h).
Storm history of Hurricane Katrina 
 It became a Category 5 storm by 7:00 a.m. CDT, twelve hours after the beginning of the second round of rapid intensification, and reached its peak intensity at 1:00 p.m. CDT with maximum sustained winds of 175 mph (280 km/h), gusts of 215 mph (344 km/h) and a central pressure of 902 mbar (26.64 inHg).
Storm history of Hurricane Katrina 
 The minimum pressure made Katrina, at the time, the fourth most intense Atlantic hurricane on record (Hurricanes Rita and Wilma would later beat Katrina's record that same year).
Storm history of Hurricane Katrina 
 As the hurricane came closer New Orleans, the Weather Forecast Office in Slidell, Louisiana gave out two strongly-worded warnings of the storm's danger.
Storm history of Hurricane Katrina 
 By the afternoon of August 28, the storm was large enough that some areas of the Gulf Coast were already experiencing tropical storm-force winds.
Storm history of Hurricane Katrina 
 The center of Katrina was about 180 statute miles (290 km) from the mouth of the Mississippi River, but tropical storm-force winds extended 230 mi (370 km) from the center of the storm, and hurricane-force winds extended about 105 miles (170 km) away.
Storm history of Hurricane Katrina 
 Overnight on August 29, and into the morning of the next day, Katrina quickly weakened (in terms of maximum sustained winds) as it began to enter another eyewall replacement cycle.
Storm history of Hurricane Katrina 
 The inner eyewall disappered before an outer eyewall had fully formed, which was one of the reasons of its rapid weakening.
Storm history of Hurricane Katrina 
 In 18 hours, the hurricane's maximum sustained winds decreased from 170 mph (280 km/h) to 125 mph (205 km/h).
Storm history of Hurricane Katrina 
 However, storm surges remained high at landfall because large waves greater than 30 feet (9.1 m) in height were generated beforehand (with a buoy recording a 55 ft/16.7 m wave at sea), when Katrina was at Categories 4 and 5 on the Saffir-Simpson Hurricane Scale.
Storm history of Hurricane Katrina 
 Katrina made its second landfall at 6:10 a.m. CDT on August 29 as a Category 3 hurricane with winds of 125 mph (205 km/h) near Buras-Triumph, Louisiana.
Storm history of Hurricane Katrina 
 Because Katrina had just weakened from Category 4 strength, and also because of the shape of the coastline, Category 4-force winds are believed to have existed on land while the eye was over water.
Storm history of Hurricane Katrina 
 At landfall, hurricane-force winds were recorded 120 miles (190 km) from the center, the storm's central pressure was 920 mbar (27.17 inHg), and its forward speed was 15 mph (10 km/h).
Storm history of Hurricane Katrina 
 As it made its way up the eastern Louisiana coastline, most communities in Plaquemines, St. Bernard Parish, and Slidell in St. Tammany Parish were severely damaged by storm surge and the strong winds of the eyewall, which also swipped over eastern New Orleans, creating $1 billion worth of damage to the city from intense flooding and wind damage.
Storm history of Hurricane Katrina 
 Original estimates recorded that Katrina had made this landfall as a Category 4 hurricane, with 135 mph (220 km/h) winds; however, as mentioned above, the storm weakened just before landfall to Category 3 intensity.
Storm history of Hurricane Katrina 
 The reasons for this weakening are not completely understood yet; while the eye-wall replacement cycle played a part, slightly increasing shear, dropping sea surface temperatures, dry air on the western semicircle of the storm and interaction with the continental landmass also may have played a role in weakening the cyclone.
Storm history of Hurricane Katrina 
 This follows the trend of previous strong cyclones in the Gulf of Mexico: all cyclones with minimum central pressures of 973 mbar (28.73 inHg) or less have weakened over the 12 hours before making landfall in the Gulf Coast of the United States.
Storm history of Hurricane Katrina 
 A few hours later, after weakening slightly, Katrina made its third landfall near the Louisiana-Mississippi border with 120 mph (195 km/h) sustained winds and 928 mbar (27.37 inHg) pressure, still at Category 3 intensity.
Storm history of Hurricane Katrina 
 Its minimum pressure at its second landfall was 920 mbar (27.17 inHg), making Katrina the third strongest hurricane on record to make landfall on the United States, behind Hurricane Camille's 909 mbar (26.85 inHg) reading in 1969, and the 1935 Labor Day Hurricane's 892 mbar (26.35 inHg) record.
Storm history of Hurricane Katrina 
 Because the storm was so large, its highly destructive eye-wall winds and the strong northeastern quadrant of the storm pushed record storm surges onshore, smashing all of the Mississippi Gulf Coast, including towns in Mississippi such as Waveland, Bay St. Louis, Pass Christian, Long Beach, Gulfport, Biloxi, Ocean Springs, Gautier and Pascagoula, and, in Alabama, Bayou La Batre.
Storm history of Hurricane Katrina 
 The surges at its peak were at 28 feet (8.5 m) in Bay St. Louis, Mississippi, and at 13 feet (4.0 m) as far away as Mobile, Alabama, which saw its highest storm surge since 1917.
Storm history of Hurricane Katrina 
 Storm surge was particularly high due to the hydrology of the region, the hurricane's extreme size, and the fact that it weakened only shortly before landfall.
Storm history of Hurricane Katrina 
 As Katrina moved inland diagonally over Mississippi, high winds cut a swath of damage that affected almost the entire state.
Storm history of Hurricane Katrina 
 One half of the storm continued to race northward, affecting the Central United States, and it was last noticeable in the eastern Great Lakes region.
Storm history of Hurricane Katrina 
 On August 31, it was absorbed by a frontal boundary and became a powerful extratropical low, causing 1.97–6.69 inches (50–170 mm) of rain in 12 hours.
Storm history of Hurricane Katrina 
 It also caused gale-force wind gusts from 31 to 61 mph (50 to 98 km/h) in southeastern Quebec and northern New Brunswick.
Storm history of Hurricane Katrina 
 However, the other half of Katrina broke off in the eastern part of the Appalachians, which caused a major tornado outbreak in the area from central Georgia to central Pennsylvania.
Storm history of Hurricane Katrina 
 At 11:00 p.m. EDT on August 31, the center of the remaining storm that was once Katrina was absorbed by another weather system in southeastern Canada.
Troposphere 
 The troposphere is made up of approximately 78% nitrogen, 21% oxygen, and 1% other gases, which include carbon dioxide, methane, neon, krypton, argon, helium, and hydrogen.
Rapid deepening 
 Rapid deepening is a condition that happens when the minimum sea-level atmospheric pressure of a tropical cyclone goes down at lot very quickly.
Rapid deepening 
 The National Weather Service describes rapid deepening as a decrease of 42 millibars in less than 24 hours.
Doppler radar 
 The Doppler effect will shift the received frequency up or down, based on the radial velocity of a target in the beam.
Doppler radar 
 This gives a direct and highly accurate measurement of target velocity, but only the radial velocity.
Doppler radar 
 Doppler radar by itself doesn't measure the azimuthal velocity (how fast it is going in other directions).
Horseshoe crab 
 The long, spiky tail is not used as a weapon or for defense; instead, it is just used for steering and flipping the body over if it gets turned upside down.
Horseshoe crab 
 Atlantic horseshoe crabs, Limulus polyphemus, can be found all over the eastern coast of North America and Mexico.
Horseshoe crab 
 Some of these shells are quite big, as the horseshoe crab can grow up to two feet long and a foot wide.
Horseshoe crab 
 The horseshoe crab population ranges from the Yucatán Peninsula to northern Maine, but they are most commonly found in the mid-Atlantic region between Virginia and New Jersey.
Horseshoe crab 
 Each major estuary along the coast has its own horseshoe crab population, distinguished from one another by size, colour and eye pigment.
Horseshoe crab 
 The Japanese horseshoe crab (Tachypleus tridentatus) is found in the Seto Inland Sea, and is considered an endangered species because of loss of habitat.
Horseshoe crab 
 Two other species occur along the east coast of India: Tachypleus gigas and Carcinoscorpius rotundicauda.
Horseshoe crab 
 The blood of horseshoe crabs contains an enzyme that causes very rapid clotting in response to the presence of infectious bacteria.
Horseshoe crab 
 This response is used by medical and pharmaceutical companies to detect those kinds of bacteria in products, before the products are sold.
Horseshoe crab 
 Horseshoe crabs are relatives of the Eurypterids (sea scorpions), whose first fossils appeared at the same time.
Horseshoe crab 
 They were definitely present in the early Ordovician, 450 million years ago, in a Burgess Shale-type environment.
Horseshoe crab 
 The Atlantic horseshoe crab itself has no fossil record at all, and the genus Limulus goes back only some 20 million years, not 200 million.
Horseshoe crab 
 Because they are famous as so-called "living fossils", the evolutionary record and the genetics of the horsehoe crabs have been studied with interest.
Horseshoe crab 
 The living species in the genus Limulus, are virtually identical to fossil species in a different family that existed 150 mya".
Horseshoe crab 
 Genetic and molecular analysis of Limulus makes it clear that the animal has just as much genetic variability as any normal species.
Atlantic hurricane 
 An Atlantic hurricane is a tropical cyclone that forms in the Atlantic Ocean, usually in the Northern Hemisphere during the summer or autumn, with one-minute maximum sustained winds of at least 74 mph (64 knots, 33 m/s, 119 km/h).
Atlantic hurricane 
 When applied to hurricanes, "Atlantic" generally refers to the entire "Atlantic basin", which includes the North Atlantic Ocean, Caribbean Sea and the Gulf of Mexico.
Atlantic hurricane 
 The United States National Hurricane Center monitors the basin and gives out reports, watches and warnings about tropical weather systems for the Atlantic Basin as one of the Regional Specialized Meteorological Centers for tropical cyclones as defined by the World Meteorological Organization.
Atlantic hurricane 
 On average, 10.1 named storms form each season, with an average of 5.9 becoming hurricanes and 2.5 becoming major hurricanes (Category 3 or greater).
Buras-Triumph, Louisiana 
 Buras-Triumph has become famous as the location where, on August 29, 2005, at 6:10 AM CDT, the eye of Hurricane Katrina made its strongest landfall.
Dry Tortugas 
 They are an unincorporated area of Monroe County, Florida and belong to the Lower Keys Census County Division.
Aventura, Florida 
 The city name is from the Spanish word for "adventure," and was named "Aventura" because that was the name of the original group of condominium developments in the area.
Florida Keys 
 They begin at the southeastern tip of the Florida peninsula, about 15 miles south of Miami, and extend in a gentle arc south-southwest and then westward to Key West, the westernmost of the inhabited islands, and on to the uninhabited Dry Tortugas.
Florida Keys 
 The islands lie along the Florida Straits, dividing the Atlantic Ocean to the east from the Gulf of Mexico to the west, and defining one edge of Florida Bay.
Florida Keys 
 More than 95 percent of the land area is in Monroe County, but a small portion extends northeast into Miami-Dade County, primarily in the city of Islandia, Florida.
Florida Keys 
 As of the 2000 census the population was 79,535, with an average density of 223.66/km² (579.27/sq mi), although much of the population is concentrated in a few areas of much higher density, such as the city of Key West, which has 32% of the entire population of the Keys.
Florida Keys 
 The city of Key West is the county seat of Monroe County, which consists of a section on the mainland which is almost entirely in Everglades National Park, and the Keys islands from Key Largo to the Dry Tortugas.
Climatology 
 Climatology is the study of climate, scientifically defined as weather conditions averaged over a period of time, and is a branch of the atmospheric sciences.
Climatology 
 Basic knowledge of climate can be used within shorter term weather forecasting using analog techniques such as teleconnections and climate indices.
Climatology 
 Climatology News Daily publication with news in all areas of climatology plus free news feeds for webmasters.
Climatology 
 IPCC Intergovernmental Panel on Climate Change: The IPCC assesses the scientific, technical and socio-economic information relevant for the understanding of the risk of human-induced climate change.