the-french-artist/wikipedia_20220301.simple_sentence_embeddings huggingface dataset:
Hurricane Florence (2006) 
 Hurricane Florence was the first Atlantic hurricane to produce hurricane force winds on Bermuda since Hurricane Fabian hit the island in September 2003.
Hurricane Florence (2006) 
 The seventh tropical storm and second hurricane of the 2006 Atlantic hurricane season, Florence developed from a tropical wave in the tropical Atlantic Ocean on September 3 and followed the track of a Cape Verde-type hurricane.
Hurricane Florence (2006) 
 Because of unfavorable conditions, the system failed to organize at first, and as a result the storm grew to an unusually large size.
Hurricane Florence (2006) 
 After several days, Florence encountered an area of lesser wind shear and strengthened into a hurricane on September 10.
Hurricane Florence (2006) 
 It passed just west of Bermuda while recurving northeastward, and on September 13 it transitioned into an extratropical cyclone.
Hurricane Florence (2006) 
 Florence produced wind gusts of up to 115 mph (185 km/h) on Bermuda, which caused several power outages and minor damage.
Hurricane Florence (2006) 
 Florence then brought heavy rains across Newfoundland as an extratropical storm, destroying one house and causing minor damage to several others.
Hurricane Florence (2006) 
 On August 31, a second tropical wave exited the coast of Africa at a faster speed than its predecessor.
Hurricane Florence (2006) 
 The two waves interacted, and by September 2 combined to form a large area of disturbed weather across the eastern Atlantic Ocean.
Hurricane Florence (2006) 
 Convection increased within the system, and the large system developed a thick area of convection along with an organized low pressure area.
Hurricane Florence (2006) 
 By late on September 3, the system maintained a large closed circulation and enough convective organization to be named Tropical Depression Six while located about midway between the Lesser Antilles and Africa.
Hurricane Florence (2006) 
 Banding features increased in satellite pictures, though southwesterly wind shear from an upper-level trough to its northeast and the lack of an organized circulation originally prevented strengthening.
Hurricane Florence (2006) 
 Dry air encountered the depression, and as such the depression developed very slowly; forecasters maintained considerable difficulty in determining a center of circulation.
Hurricane Florence (2006) 
 It continued its motion to the west-northwest while tracking around the southern periphery of a deep-layer subtropical ridge to its north.
Hurricane Florence (2006) 
 Though convection remained focused near the outer periphery of the system, the overall organized continued to steadily increase, and it is estimated the depression strengthened into Tropical Storm Florence on September 5 while located about 1120 miles (1800 km) east-northeast of Anguilla.
Hurricane Florence (2006) 
 After reaching tropical storm status, the maximum sustained winds existed for three days between 40 mph (65 km/h) and 50 mph (85 km/h).
Hurricane Florence (2006) 
 This is because of the large size of Florence; the wind field reached 460 miles (745 km) wide with a radius of maximum winds of about 110 miles (170 km).
Hurricane Florence (2006) 
 By September 6, an orgained form of cloud swirls became visible, with thin rainbands developing in the southeast and northwest quadrants.
Hurricane Florence (2006) 
 As a result, hurricane forecasters predicted Florence to quickly develop and reach major hurricane status.
Hurricane Florence (2006) 
 Though convection slowly moved closer to the center of the storm, forecasters could not detect an organized center of circulation late on September 13.
Hurricane Florence (2006) 
 On September 7, convection developed over and to the west of the center for the first time in its duration.
Hurricane Florence (2006) 
 However, Florence failed to strengthen any further with a wind field more than 1035 miles (1670 km) in diameter.
Hurricane Florence (2006) 
 This made it diffficult to forecast the storm, since it tracked through an area of 84° F (29° C) water temperatures, light shear, and a large low-level cyclonic envelop with abundant convection.
Hurricane Florence (2006) 
 By early on September 8, the storm became a stretched out, shapeless cloud pattern not normal for a tropical cyclone.
Hurricane Florence (2006) 
 Later that day, as an anticyclone developed over Florence, the storm began to consolidate around a vorticity center on the western side of the large cyclonic envelope.
Hurricane Florence (2006) 
 Early on September 10, an eye began developing inside a ring of round thick convection over the center, and shortly thereafter Florence reached hurricane status while located about 390 miles (630 km) south of Bermuda.
Hurricane Florence (2006) 
 Hurricane Florence turned to the north and north-northeast through a break in the subtropical ridge.
Hurricane Florence (2006) 
 Though its eyewall was open on the north side, favorable conditions led forecasters to predict Florence passing near Bermuda as a strong Category 2 hurricane.
Hurricane Florence (2006) 
 The inner core of convection became ragged-looking on satellite pictures, and based on reports from Hurricane Hunters it is estimated the hurricane reached peak winds of 90 mph (150 km/h) late on September 10.
Hurricane Florence (2006) 
 Subsequent to further erosion of the eyewall, the hurricane weakened, and on September 11 passed about 60 miles (95 km) west of Bermuda with winds of 85 mph (135 km/h).
Hurricane Florence (2006) 
 The overall cloud pattern became a little bit better organized, and Florence briefly re-strengthened before encountering increased upper-level winds and cooler waters.
Hurricane Florence (2006) 
 Dry air wrapping around the southern half of the cyclone dissipated most of the deep convection by early on September 12.
Hurricane Florence (2006) 
 The cloud shield became asymmetrically displaced to the north of the center, and frontal-like features began to form.
Hurricane Florence (2006) 
 It continued to lose tropical characteristics, and on September 13 Florence turned into an extratropical cyclone about 485 miles (780 km) south-southwest of Cape Race, Newfoundland.
Hurricane Florence (2006) 
 At first, the storm was able to keep hurricane-force winds, as the extratropical remnant passed near Cape Race before turning to the east-northeast, and on September 14 the winds weakened to gale force.
Hurricane Florence (2006) 
 The storm executed a broad cyclonic half-loop to the southwest of Iceland over the subsequent days, and after turning to the west the extratropical remnants of Florence were absorbed to the east of Greenland by a developing extratropical cyclone to its south.
Hurricane Florence (2006) 
 The government of Bermuda gave out a hurricane watch for the island on September 8, which was followed by a tropical storm warning on September 9.
Hurricane Florence (2006) 
 These were replaced by a hurricane warning on September 10, which were given out at the same time with the storm's strengthening to hurricane status.
Hurricane Florence (2006) 
 The government pursaded the potentially impacted citizens to take preparations for the storm, many of whom bought supplies at local hardware stores.
Hurricane Florence (2006) 
 Before Florence approached the storm, officials canceled bus and ferry service, and also closed all schools and government offices on the day of impact.
Hurricane Florence (2006) 
 Hurricane Florence produced strong swells and dangerous surf conditions for the northern Lesser Antilles, U.S. Virgin Islands, Puerto Rico, Hispaniola, and Bermuda.
Hurricane Florence (2006) 
 Later in its duration, the tight pressure gradient between Florence and a high-pressure system over southeastern Canada produced strong winds and rough waves along the East Coast of the United States.
Hurricane Florence (2006) 
 The hurricane also caused strong swells and rough ocean conditions, including rip currents, in the Bahamas and Atlantic Canada.
Hurricane Florence (2006) 
 Passing a short distance west of Bermuda, Hurricane Florence produced strong winds on the island; sustained winds peaked at 82 mph (132 km/h) on St. David's Island at an elevation of 410 feet (48 m), while gusts reached 115 mph (185 km/h) at the Maritime Operations Centre in St. George's Parish at an elevation of 665 feet (78 m).
Hurricane Florence (2006) 
 The winds knocked down trees and power lines, leaving over 25,000 homes and businesses without electricity during the peak of the storm.
Hurricane Florence (2006) 
 The powerful winds damaged ten houses, including destroying the roofs of three, and blew out windows across the island.
Hurricane Florence (2006) 
 During the peak of the storm, police officials advised citizens to remain indoors away from harm, though there were several reports of looting throughout the territory.
Hurricane Florence (2006) 
 Shortly after the storm passed through, BELCO began restoring power, and by six hours after the peak of the storm power had been restored to 7,000 homes and businesses.
Hurricane Florence (2006) 
 The passage of the storm damaged the causeway between St. David's Island and Hamilton Parish, temporarily limiting traffic to one lane in each direction.
Hurricane Florence (2006) 
 As an extratropical storm over Newfoundland, Florence produced powerful winds peaking at 101 mph (163 km/h) and moderate amounts of rainfall of up to 2.6 inches (67 mm).
Hurricane Florence (2006) 
 The hurricane caused flight interruptions at St. John's International Airport and also to the Trans Canada ferry between Newfoundland and Cape Breton Island in eastern Nova Scotia Strong winds destroyed a house in the small Newfoundland village of Francois.
Hurricane Florence (2006) 
 Residents in Francois agreed to rebuild the wrecked home while the family temporarily resided in a summer home of another family.
Hurricane Florence (2006) 
 The winds also caused damage to shingles and sides of homes, while the strong waves damaged roads and boats along the Burin Peninsula.
2006 Nova Scotia tropical storm 
 It formed as an extratropical cyclone, a type of weather system, to the southeast of Nantucket, Massachusetts.
2006 Nova Scotia tropical storm 
 It turned into a tropical storm on July 17, when an area of thunderstorms formed near the center of the cyclone.
2006 Nova Scotia tropical storm 
 The northern weather system was about 290 miles (470 km) to the south-southeast of Cape Cod, Massachusetts.
2006 Nova Scotia tropical storm 
 It turned into a tropical depression on July 17, when it was about 240 miles (390 km) to the southeast of Nantucket, Massachusetts.
2006 Nova Scotia tropical storm 
 The storm moved to the northwest northeastward, and it moved into an area that was good for strengthening.
2006 Nova Scotia tropical storm 
 Every year, the National Hurricane Center checks to make sure they did not miss any storms during the past tropical storm season.
2006 Nova Scotia tropical storm 
 It is guessed that the storm became a tropical cyclone at 39.1º N. This was the farthest north that any Atlantic storm in July became a tropical cyclone.
Cape Hatteras 
 It is the point that protrudes the farthest to the southeast along the northeast-to-southwest line of the Atlantic coast of North America, making it a key point for navigation along the eastern seaboard.
Tropical Storm Alberto (1988) 
 Tropical Storm Alberto (also known as Hurricane Alberto) became a tropical storm farther north than any other Atlantic tropical cyclone.
Tropical Storm Alberto (1988) 
 Tropical Storm Alberto continued to move quickly, and struck the western area of Nova Scotia late on August 7.
Tropical Storm Beryl (2006) 
 Developing from a tropical disturbance on July 18, it tracked generally northward, and strengthened to attain peak winds of 60 mph (95 km/h) under generally favorable conditions.
Tropical Storm Beryl (2006) 
 The extratropical remnants continued northeastward through Nova Scotia, and on July 22 it merged with an approaching cold front.
Tropical Storm Beryl (2006) 
 In Massachusetts, its impact was limited to light rainfall and gusty winds, with no reported damage.
Tropical Storm Beryl (2006) 
 Beryl later produced moderate rainfall and gusty winds across Atlantic Canada, resulting in some localized power outages though little damage.
Tropical Storm Beryl (2006) 
 A cold front moved off the East Coast of the United States on July 16 and stalled off the coast of North Carolina.
Tropical Storm Beryl (2006) 
 It slowly decayed into a surface low pressure trough, and developed into two disturbances; one was centered 290 miles (490 km) south-southeast of Cape Cod and another was located 200 miles (320 km) south of Cape Hatteras, North Carolina.
Tropical Storm Beryl (2006) 
 The first low quickly organized into an unnamed tropical storm, and the other area stayed broad and disorganized.
Tropical Storm Beryl (2006) 
 However, by July 18, the system became much better organized with improved banding features, and the area developed into Tropical Depression Two while located 220 miles (355 km) south-southeast of Cape Hatteras.
Tropical Storm Beryl (2006) 
 The depression moved slowly to the north-northwest through a break in the subtropical ridge, and as convective banding features became more visible the system strengthened into Tropical Storm Beryl.
Tropical Storm Beryl (2006) 
 Throughout much of its duration, the storm tracked through an environment with light vertical wind shear and well-established upper-level outflow.
Tropical Storm Beryl (2006) 
 Shortly after becoming a tropical storm, the low-level circulation of Beryl became exposed with limited deep convection, though deep convection re-developed the following morning.
Tropical Storm Beryl (2006) 
 Outflow continued to improve, and with warm sea surface temperatures Beryl slowly strengthened further to reach peak winds of 60 mph (95 km/h) early on July 20 while located about 120 miles (190 km) east of Nags Head, North Carolina.
Tropical Storm Beryl (2006) 
 Beryl maintained peak winds for about 18 hours as it paralleled the Mid-Atlantic and New Jersey coasts, during which an eye-like feature developed in the center of the convection.
Tropical Storm Beryl (2006) 
 Steering winds ahead of an approaching mid-level trough caused Beryl to speed up northeastward, and early on July 21 the center of the storm crossed the island of Nantucket.
Tropical Storm Beryl (2006) 
 The convection diminished as it moved through progressively colder waters, and shortly after 1200 UTC on July 21 Beryl became an extratropical cyclone a short distance east of Cape Cod.
Tropical Storm Beryl (2006) 
 Hours later, it made landfall in southwestern Nova Scotia, and on July 22 the extratropical remnants of Beryl merged with an approaching cold front over Newfoundland.
Tropical Storm Beryl (2006) 
 Forecasters originally predicted Beryl to brush the Carolinas; as such, a tropical storm watch was issued for the eastern coast of North Carolina from Cape Lookout northward to Currituck Beach Lighthouse.
Tropical Storm Beryl (2006) 
 When a more northeastward track became apparent, a tropical storm watch was issued about 33 hours before moving ashore from Woods Hole to Plymouth, Massachusetts, including Cape Cod, Nantucket, and Martha's Vineyard.
Tropical Storm Beryl (2006) 
 About 22 hours before landfall, the National Hurricane Center replaced the watch with a tropical storm warning for the same area, and also issued a tropical storm watch from Woods Hole, Massachusetts westward to New Haven, Connecticut and for the eastern portion of Long Island from east of Fire Island to Port Jefferson.
Tropical Storm Beryl (2006) 
 Expecting for the storm, the Massachusetts Emergency Management Agency was activated as a trial run for the hurricane season.
Tropical Storm Beryl (2006) 
 Local Red Cross chapters were opened, as well, with two volunteer teams placed on standby to assist.
Tropical Storm Beryl (2006) 
 Across southeastern Massachusetts, police departments maintained extra staff in preparation for any potential problems from the storm.
Tropical Storm Beryl (2006) 
 Many fishermen secured their boats, while some business owners boarded up windows to prevent storm damage.
Tropical Storm Beryl (2006) 
 Several days prior to the passage of Beryl through Atlantic Canada, the Canadian Hurricane Centre issued gale warnings for the coastal waters off of Nova Scotia and Newfoundland.
Tropical Storm Beryl (2006) 
 In anticipation of heavy rainfall, the agency also issued heavy rainfall warnings for western Nova Scotia, including Halifax.
Tropical Storm Beryl (2006) 
 The storm caused high waves along the East Coast of the United States, with 19 foot seas (5.97 m) in the open ocean.
Tropical Storm Beryl (2006) 
 Waves along the southern coast of Nantucket reached 10 feet in height as the storm approached the island, resulting in four people being rescued by lifeguards from rip currents.
Tropical Storm Beryl (2006) 
 Winds across southeastern Massachusetts were fairly light, with no sustained tropical storm force winds and wind gusts peaking at 44 mph; unofficially gusts reached 51 mph.
Tropical Storm Beryl (2006) 
 Beryl dropped moderate precipitation just offshore, though the maximum precipitation total in the United States was only 0.97 inches (24.6 mm) on Nantucket.
Tropical Storm Beryl (2006) 
 Overall impact was minor; there were no reported power outages, deaths, injuries, or maritime emergencies in association with the storm.
Tropical Storm Beryl (2006) 
 The remnants of Beryl dropped moderate precipitation in Atlantic Canada, officially peaking at 2.8 inches (71 mm) in Scotts Bay, Nova Scotia with an unofficially higher total of 3.5 inches (88 mm); in some locations 1 inch of rain fell in an hour.
Tropical Storm Beryl (2006) 
 Moderate winds were reported along its path, which peaked at 60 mph (96 km/h) in southern Nova Scotia.
1991 Halloween Nor'easter 
 The 1991 Halloween Nor’easter, also known as the Perfect Storm, was an atypical nor’easter which was extratropical, absorbed one hurricane, and ultimately evolved into a small hurricane late in its life cycle.
1991 Halloween Nor'easter 
 The unnamed hurricane of 1991 was the last tropical cyclone of the 1991 Atlantic hurricane season, and its 4 hurricane.
Nor'easter 
 A Nor'easter is called that because the winds in a Nor'easter come from the northeast, especially in the coastal areas of the Northeastern United States and Atlantic Canada.
Nor'easter 
 More specifically, it is a low pressure area whose center of rotation is just off the East Coast and whose leading winds in the left forward quadrant rotate onto land from the northeast.
Nor'easter 
 Nor'easters also can cause coastal flooding, coastal erosion, hurricane force winds, and heavy snow.
Nor'easter 
 Nor'easters can occur at any time of the year but are mostly known for their presence in the winter.
Nor'easter 
 Nor'easters can be devastating and damaging, especially in the winter months, when most damage and deaths are from the cold.
Nor'easter 
 Nor'easters thrive on the converging air masses; that is, the polar cold air mass and the warmer ocean water of the Gulf Stream.
Cape Lookout (North Carolina) 
 Cape Lookout is southern point of the South Core Banks, one of the natural barrier islands on the Atlantic coast of North Carolina, USA.
Cape Lookout (North Carolina) 
 Cape Lookout stands at 34°36'19"N, 76°32'10"W, and is part of Carteret County, 11 miles southeast of Beaufort, NC.
New Haven, Connecticut 
 New Haven is the second largest city in Connecticut, after Bridgeport, with a population of 129,779 at the 2010 United States Census. "
New Haven, Connecticut 
 New Haven" may also refer to the wider Greater New Haven area, which has nearly 600,000 inhabitants in the immediate area.
Martha's Vineyard 
 Martha's Vineyard (and the smaller Chappaquiddick Island nearby) is an island off the southern coast of Cape Cod, both forming a part of the Outer Lands region.
Martha's Vineyard 
 With a land area of 87.48 square miles (231.75 km²), Martha's Vineyard is the 57th largest island in the United States.
Martha's Vineyard 
 It is located in the U.S. state of Massachusetts, in Dukes County, which also includes Cuttyhunk and the other Elizabeth Islands, as well as the island of Nomans Land.
Woods Hole, Massachusetts 
 Woods Hole is a census-designated place and village within the town of Falmouth in Barnstable County, Massachusetts, at the extreme southwest corner of Cape Cod, near Martha's Vineyard and the Elizabeth Islands.
Carcinogen 
 The carcinogens in them are caused by the radiation they release, such as gamma rays or alpha particles.
Carcinogen 
 How much of a carcinogen a radiation is depends on the type of radiation, the type of exposure to it and its penetration.
Carcinogen 
 Marie Curie, one of the pioneers of radioactivity, died of a cancer that was caused by the radiation she was exposed to during her experiments.
Carcinogen 
 Higher-energy radiation, including ultraviolet radiation, usually is carcinogenic, if a person is exposed to it long enough.
Carcinogen 
 Recent research has shown that when food is cooked at high temperatures, carcinogens may be formed in very small amounts.
Carcinogen 
 Pre-cooking meats in a microwave oven for 2-3 minutes before broiling shortens the time on the hot pan.
Carcinogen 
 Certain kinds of foods, like potato chips and French fries, may have higher levels of carcinogens than others.
Port Jefferson, New York 
 The Incorporated Village of Port Jefferson is in the town of Brookhaven in Suffolk County, New York.
Fairchild Republic A-10 Thunderbolt II 
 It is designed to drop bombs, fire rockets, missiles, and its 30 mm Gatling Gun at enemies on the ground (like tanks).
Fairchild Republic A-10 Thunderbolt II 
 The A-10 is also used as a CAS (close air support) aircraft, which involves flying slowly over a target area and destroying any targets in that area.
Fairchild Republic A-10 Thunderbolt II 
 The A-10 is 53 feet, 4 inches (16.16 meters) long, 14 feet, 8 inches (4.42 meters) high, has a wingspan of 57 feet, 6 inches (17.42 meters), can go 420 miles per hour, and can weigh 51,000 pounds (22,950 kilograms) at heaviest.
Fairchild Republic A-10 Thunderbolt II 
 It can also carry radar-jamming pods so it cannot be seen on radar, and chaff, which can confuse missiles fired at the A-10.
Fairchild Republic A-10 Thunderbolt II 
 While the A-10 has a lot of room on its wings to carry bombs and missiles, its main weapon is the gun, called the GAU-8 Avenger.
Fairchild Republic A-10 Thunderbolt II 
 It is a very long and heavy gun called a Gatling cannon, since it is a both an autocannon (fires large bullets very fast) and Gatling gun (has more than one barrel, which spin while being shot) The Avenger is so big that the A-10 had to be built around it, which created the joke that the A-10 does not have a gun attached like other warplanes, but it is the Avenger that has a plane attached.
Fairchild Republic A-10 Thunderbolt II 
 Other American planes instead use the smaller Vulcan, which is also a Gatling cannon but with a smaller bullet.
Fairchild Republic A-10 Thunderbolt II 
 Because the Avenger fires such big bullets (artillery shells 3 cm wide, which also explode) at such a high rate of fire (up to 40 every second) many believe it can destroy any target very easily, even tanks with thick armour such as the M1 Abrams.
Fairchild Republic A-10 Thunderbolt II 
 The bullet can go through thin metal on a car or truck, but it cannot penetrate the thick metal covering a tank.
Fairchild Republic A-10 Thunderbolt II 
 If an A-10 manages to shoot there, then it is bad for the tank, but if it shoots the front or side where the metal is thicker, then the tank will not be damaged.
Fairchild Republic A-10 Thunderbolt II 
 After trying other procedures, she turned off the hydraulics and flew the aircraft in manual reversion.
Fire Island, New York 
 Fire Island is a barrier island, approximately 31 miles (49.5 km) long and varying between approximately 0.1 mile (0.16 km) to 0.5 mile (0.8 km) wide, in Suffolk County on the southern side of Long Island in the U.S. state of New York, running approximately WSW to ENE.