the-french-artist/wikipedia_20220301.simple_sentence_embeddings huggingface dataset:
Electronic component 
 connector plug = a device at the end of a fibre-optic or copper cable that receives and contains something.
Asuel 
 Asuel is a municipality, in the new municipality of La Baroche and district Porrentruy in the canton of Jura in Switzerland.
Bressaucourt 
 On 1 January 2013 the former municipality of Bressaucourt merged into the municipality of Fontenais.
South Uist 
 There is a nature reserve and a number of sites of archaeological interest, including the only location in Great Britain where prehistoric mummies have been found.
South Uist 
 The island, in common with the rest of the Hebrides, is one of the last remaining strongholds of the Gaelic language in Scotland.
South Uist 
 In 2006 South Uist, and neighbouring Benbecula and Eriskay were involved in  Scotland's biggest community land buyout to date.
Outer Hebrides 
 The Outer Hebrides, often called the Western Isles, make up an island chain off the west coast of Scotland.
Outer Hebrides 
 The isles form part of the Hebrides, and are separated from the Scottish mainland and from the Inner Hebrides by the stormy waters of the Minch, the Little Minch and the Sea of the Hebrides.
Outer Hebrides 
 Formerly the dominant language of the Islands, Scottish Gaelic remains spoken even though it has now been largely supplanted by English in some parts.
Outer Hebrides 
 Sea transport is crucial and a variety of ferry services operate between the islands and to mainland Britain.
Outer Hebrides 
 The Western Isles became part of the Suðreyjar kingdom of the Norse, who ruled for over 400 years until sovereignty was transferred to Scotland by the Treaty of Perth in 1266.
Outer Hebrides 
 Most of the islands have a bedrock formed from ancient metamorphic rocks and the climate is mild and oceanic.
Outer Hebrides 
 The 15 inhabited islands have a total population of about 26,500 and there are more than 50 substantial uninhabited islands.
Outer Hebrides 
 Much of the archipelago is a protected habitat including both the islands and the surrounding waters.
Outer Hebrides 
 There are 53 Sites of Special Scientific Interest (SSSI) of which the largest are Loch an Duin, North Uist  at  and North Harris, which is  in extent.
Outer Hebrides 
 Loch Druidibeg on South Uist is a National Nature Reserve owned and managed by Scottish Natural Heritage.
Outer Hebrides 
 Historical footnote: Many websites of the Outer Hebrides derive content from the Eolas Virtual Hebrides, website.
Space Shuttle Atlantis 
 It was named after a sailing boat used for ocean research by the Woods Hole Oceanographic Institute.
Hurricane Gordon (2006) 
 Hurricane Gordon was a strong Category 3 hurricane that crossed the Azores as a Category 1 hurricane, making it the first hurricane to directly impact the Azores since 1991.
Hurricane Gordon (2006) 
 It was the eighth tropical storm, third hurricane and first major hurricane of the 2006 Atlantic hurricane season.
Hurricane Gordon (2006) 
 It began as a tropical wave just right behind Florence in the first week of September, which at first was absorbed into the large circulation of then-Tropical Storm Florence.
Hurricane Gordon (2006) 
 As Florence began to organize and move northwest, the wave managed to break from the circulation again and slowly organize in spite of hostile conditions at first.
Hurricane Gordon (2006) 
 On September 10, it had organized enough to be declared Tropical Depression Seven northeast of the Lesser Antilles.
Hurricane Gordon (2006) 
 With Florence far away from the system, conditions became more favorable for development, and it was upgraded to Tropical Storm Gordon on September 11 while moving slowly westward.
Hurricane Gordon (2006) 
 The conditions remained favorable as Gordon steered through a hole in the ridge near the Azores, allowing it to avoid land.
Hurricane Gordon (2006) 
 It continued to strengthen, becoming a hurricane on September 12 and rapidly organizing into a strong Category 2 hurricane less than 24 hours later.
Hurricane Gordon (2006) 
 The quick development continued on September 13, and by that evening, it had strengthened into a major hurricane - the first of 2006 - while maintaining a very small size.
Hurricane Gordon (2006) 
 Gordon would remain a major hurricane for over 24 hours before cooler water began to set in and Gordon gradually weakened, beginning early on September 15.
Hurricane Gordon (2006) 
 The steering currents would also weaken greatly and Gordon became nearly stationary for about 24 hours as well before a trough would come in and push Gordon northeastward.
Hurricane Gordon (2006) 
 By the morning of September 16, Gordon was barely a hurricane and was forecast to weaken over cooler waters.
Hurricane Gordon (2006) 
 However, that did not happen, and Gordon actually strengthened a little bit while moving northeastward and became better organized.
Hurricane Gordon (2006) 
 That trend continued for over 48 hours, and Gordon increased in strength slowly, becoming a Category 2 hurricane.
Hurricane Gordon (2006) 
 While the forecast constantly showed a weakening trend, the resiliency suddenly meant that the Azores were threatened by Gordon.
Hurricane Gordon (2006) 
 Gordon reached its secondary peak of 105 mph (165 km/h) on the morning of September 19, before weakening again.
Hurricane Gordon (2006) 
 The remnants of Gordon then began to interact with a large Atlantic low pressure area to the west of Ireland and an associated weather front extending south.
Hurricane Gordon (2006) 
 It tracked towards the north-west of the Iberian Peninsula and then on September 21 turned northwards towards south-west Britain and Ireland.
Hurricane Gordon (2006) 
 With the onset of Gordon expected, all nine Azores Islands were placed on red alert by the Portuguese government, and residents were asked to take emergency precautions.
Hurricane Gordon (2006) 
 Residents were warned to stay indoors, close doors and windows, clear storm sewers and move livestock to safe areas.
Hurricane Gordon (2006) 
 Forecasters warned of winds as high as 105 mph (170 km/h), along with heavy rain and waves of up to 12 metres (40 ft) high lashing coastal areas.
Hurricane Gordon (2006) 
 In Spain, the region of Galicia was placed on red alert - the highest level - by authorities who were expecting the extratropical remnants of Gordon.
Hurricane Gordon (2006) 
 11 other regions of Spain, including as far east as Madrid and as far south as Andalusia, received lower levels of warning.
Hurricane Gordon (2006) 
 Stormy conditions caused by the remnants of Gordon were expected to affect the 2006 Ryder Cup in Straffan, County Kildare, Ireland, starting fears that the event may be greatly interrupted and delayed.
Hurricane Gordon (2006) 
 Strong gusts and heavy rain associated with another system had already caused some damages, resulting both teams to delay their second practice rounds.
Hurricane Gordon (2006) 
 This led to concerns about the possible state of the course by the time the tournament proper was expected to start on September 22, leading to the possibility of further interruptions and possible changing of the normal rules.
Hurricane Gordon (2006) 
 On September 19 it was reported that the remnants of Gordon would cause high winds and rainfall in parts of the United Kingdom.
Hurricane Gordon (2006) 
 The UK Met Office stated that a "period of very windy weather" with "exceptionally severe gales" was expected for much of Northern Ireland and Scotland.
Hurricane Gordon (2006) 
 Northern Ireland was expected to receive the worst of the storm, with severe gales as high as 80 mph expected.
Hurricane Gordon (2006) 
 There were also warnings of localised flooding, with up to two inches (50 mm) of rain expected to fall.
Hurricane Gordon (2006) 
 There were only reports of toppled trees and power lines, knocking out power to some communities, particularly on Santa Maria Island.
Hurricane Gordon (2006) 
 Gordon hit the northwestern province of Galicia while as a strengthening extratropical storm early on September 21.
Hurricane Gordon (2006) 
 On September 20, practice rounds for the Ryder Cup were temporarily delayed due to high winds, but Meteorological Office charts showed these to be associated with a different Atlantic low pressure area rather than effects of Gordon itself.
Hurricane Gordon (2006) 
 The remnants of Gordon caused stormy conditions late on September 21, with 1,500 homes losing power.
Hurricane Gordon (2006) 
 The worst affected areas were on the east coast between Drogheda and Wexford and in the south around Cork and Limerick.
Hurricane Gordon (2006) 
 Earlier on the 21st, a woman attending the Ryder Cup in County Kildare was injured after a tree branch fell near a golf buggy in which she was travelling.
Hurricane Gordon (2006) 
 However, the gates opened at 06:00 on September 22 as originally planned and the tournament's first day went ahead without major disruption.
Hurricane Gordon (2006) 
 A gust of 81 mph (130 km/h) was recorded and power lines were hit, leaving more than 1,000 homes without power in Truro, Cornwall.
Hurricane Gordon (2006) 
 In Devon, the rail line between Exeter and Plymouth was damaged by high surf at Dawlish, causing disruption to services.
Hurricane Gordon (2006) 
 Fallen trees caused widespread disruption: in County Down, several people had to be rescued from their vehicles after trees had fallen on them; flooding was also reported at Rostrevor.
Hurricane Gordon (2006) 
 Several roads across the province were blocked by fallen trees, including the M1 motorway and the main roads from Derry to Belfast and Coleraine.
Hurricane Gordon (2006) 
 Lorries on the A715 road were forced to park on the roadside overnight due to dangerous driving conditions.
Hurricane Gordon (2006) 
 One positive effect from the extratropical remnants of Gordon was observed in Newquay, Cornwall, where large waves and swells up to 2.5 m (8 ft) high made for excellent surf conditions.
Tropical Storm Debby (2006) 
 After passing near the Cape Verde islands, Debby moved generally northwestward for much of its life, reaching a peak intensity of 50 mph (85 km/h).
Tropical Storm Debby (2006) 
 Strong wind shear weakened the storm, and Debby dissipated on August 27 over the northern Atlantic Ocean.
Tropical Storm Debby (2006) 
 Early in its life, Debby was forecasted to pass through the southern Cape Verde islands as a tropical storm, possibly causing life-threatening flooding.
Tropical Storm Debby (2006) 
 Most computer models consistently predicted Debby to move to the northwest throughout its lifetime, though intensity was more of a problem for forecasters.
Tropical Storm Debby (2006) 
 The National Hurricane Center continually predicted Debby to strengthen into hurricane status, though strong vertical shear eventually prevented the storm from becoming a hurricane.
Tropical Storm Debby (2006) 
 A strong tropical wave moved off the coast of Africa late on August 20, and almost convective banding and a broad circulation.
Tropical Storm Debby (2006) 
 A large area of low pressure formed within the wave the next day while located 260 miles southeast of the Cape Verde islands.
Tropical Storm Debby (2006) 
 Though convection decreased early on August 21, the area of low pressure stayed well-organized and the system developed into Tropical Depression Four late on August 21.
Tropical Storm Debby (2006) 
 Water temperatures remained warm enough for development, while upper level shear was minimal as the depression moved west-northwestward because of a ridge of high pressure to its north.
Tropical Storm Debby (2006) 
 Original predictions by the National Hurricane Center also forecasted a turn to the northwest based computer model predictions, as quoted by forecaster James Franklin, "The models have also been excellently wrong thus far".
Tropical Storm Debby (2006) 
 In spite of a decrease in convection shortly after forming, the large depression remained well organized, with a 575 mile wide wind field.
Tropical Storm Debby (2006) 
 On August 22, as it passed 140 miles (225 km) miles to south of the Cape Verde islands, deep convection developed over the center of circulation, and early on August 23 the depression strengthened into Tropical Storm Debby about 300 miles southwest of Cape Verde.
Tropical Storm Debby (2006) 
 Banding features continued to organize as the system slowly strengthened, and on August 23 Debby reached its peak intensity of 50 mph over the open waters of the Atlantic Ocean.
Tropical Storm Debby (2006) 
 Forecasters predicted Debby to continue to strengthen to reach hurricane status, while its projected path placed the storm in an area of warm water temperatures and moderate upper level shear.
Tropical Storm Debby (2006) 
 Shortly after reaching its peak intensity, Debby encountered an area of dry air, and as a result weakened.
Tropical Storm Debby (2006) 
 The low level circulation detached itself from the dying convection while the system as a whole continued west-northwestward.
Tropical Storm Debby (2006) 
 Southerly wind shear displaced the convection to the north of the center, and Debby weakened to a weak tropical storm on August 25.
Tropical Storm Debby (2006) 
 The center of the storm became asymmetric and elongated, and on August 26 Debby weakened to a tropical depression.
Tropical Storm Debby (2006) 
 The low turned to the north and north-northeast ahead of an approaching trough, and on August 28 the low dissipated.
Tropical Storm Debby (2006) 
 The government of the Cape Verde islands gave out tropical storm warnings at the same time with the issuance of the first advisory on Tropical Depression Four, meaning tropical storm conditions were expected in the area within 24 hours.
Tropical Storm Debby (2006) 
 The National Hurricane Center stated that heavy rainfall, possibly as high as 10 inches in mountainous areas, would be possible in the territory, possibly causing life-threatening flash floods and mudslides.
Tropical Storm Debby (2006) 
 However, because of a reformation further to the south, tropical storm warnings were discontinued as the depression passed away from the area.
Tropical Storm Debby (2006) 
 While passing around 115 miles to the southwest of the southwestern most islands, the depression produced a 35 mph wind gust at Fogo and some rainfall, though no damage was reported.
Tropical Storm Debby (2006) 
 Though the storm was forecasted to remain far away from the Gulf of Mexico, investors tracking the storm caused the price of crude oil to rise 60 cents a barrel due to the possible impact to oil installations.
Fogo, Cape Verde 
 It is the most prominent of the group, rising to nearly 3,000 m (10,000 ft) above sea level at Pico do Fogo.
Hurricane Isaac (2006) 
 It reached peak strength of Category 1 just before striking Newfoundland, where it produced tropical storm-force winds.
Hurricane Isaac (2006) 
 Isaac followed the path of the three previous storms in the Atlantic basin, Florence, Gordon, and Helene.
Hurricane Isaac (2006) 
 Intensification was partly suppressed by high wind shear and by cool sea surface temperatures in the wake of Hurricanes Gordon and Helene.
Hurricane Isaac (2006) 
 Isaac reached tropical storm strength on September 28 and entered an area of low wind shear, allowing it to strengthen into an 85 mph (137 km/h) hurricane.
Hurricane Isaac (2006) 
 Its intensity nearly matched forecasts made with the Statistical Hurricane Intensity Prediction Scheme (SHIPS).
Hurricane Isaac (2006) 
 Two days later, it merged with a newly formed baroclinic low off the east coast of the United States.
Hurricane Isaac (2006) 
 Isaac was the second storm to affect Newfoundland during the season, the other being Hurricane Florence.
Hurricane Isaac (2006) 
 An area of disturbed weather began interacting with the tropical wave as deep convection increased on September 23.
Hurricane Isaac (2006) 
 The convection began to organize, and weather agencies to release the first Dvorak numbers on the system.
Hurricane Isaac (2006) 
 The SHIPS models predicted that the system would become a hurricane with maximum sustained winds of 88 knots (150 km/h) after 120 hours.
Hurricane Isaac (2006) 
 However, the system was slow to organize and a Tropical Cyclone Formation Advisory was not issued by the National Hurricane Center (NHC) until four days later.
Hurricane Isaac (2006) 
 The NHC, however, decided the convection was too ephemeral to justify classification as a tropical depression and the TCFA was discontinued.
Hurricane Isaac (2006) 
 Three days later, on September 27 another TCFA was issued, announcing the formation of the ninth tropical depression of the Atlantic season.
Hurricane Isaac (2006) 
 The depression strengthened into Tropical Storm Isaac on September 28, just twelve hours after the cyclone's formation.
Hurricane Isaac (2006) 
 Deep convection was slow to form that day since the system remained over cold waters that had upwelled in the wake of Hurricanes Gordon and Helene.
Hurricane Isaac (2006) 
 The next day, the cyclone moved west-northwestward and started gaining subtropical characteristics while its convection deepened.
Hurricane Isaac (2006) 
 Vertical shear weakened as the system moved away from the cold, upwelling waters and the core of Isaac started re-developing.
Hurricane Isaac (2006) 
 Isaac continued strengthening a little bit during the next day near Bermuda, reaching its peak intensity with sustained winds of 85 mph (135 km/h) and minimum central pressure of 985 mbar.
Hurricane Isaac (2006) 
 Isaac encountered cooler waters as it approached Newfoundland on October 1, and weakened into a tropical storm on October 2.
Hurricane Isaac (2006) 
 Isaac made landfall on the Avalon Peninsula as a weak tropical storm on October 2 and maintained tropical cyclonic structure and deep convection.
Hurricane Isaac (2006) 
 Soon after, Isaac turned into an extratropical storm and merged with a larger extratropical system on October 3 off the Avalon Peninsula.
Hurricane Isaac (2006) 
 On October 2, a ship called the Elektra (call sign SIWB) reported winds of  while it was located about  to the east of the center of the storm.
Hurricane Isaac (2006) 
 Since the storm was moving so quickly, it did not drop much rainfall; precipitation usually amounted to below .
Baroclinic 
 A baroclinic atmosphere is one for which the density depends on both the temperature and the pressure; contrast this with barotropic atmosphere, for which the density depends only on the pressure.
Baroclinic 
 In atmospheric terms, the barotropic zones of the Earth are generally found in the central latitudes, or tropics, whereas the baroclinic areas are generally found in the mid-latitude/polar regions.
Foreign Office of Germany 
 The traditional name of the ministry handling Germany's foreign affairs is the Foreign Office or AA ().
Foreign Office of Germany 
 The Foreign Office handles contact between Germany and other countries or international organisations such as the United Nations.
Foreign Office of Germany 
 This included trying to get a permanent seat in the Security Council of the United Nations as part of the proposed 2005 UN reforms.
Foreign Office of Germany 
 The big old building in the Werderschen Markt became the Reichbanks headquarters in 1940 and from 1959 the central committee headquarters of the SED.
Foreign Office of Germany 
 There are German embassies and consulates or consulates-general in most capitals of the world as well as in larger towns of the countries.
Foreign Office of Germany 
 The Berlin headquarters job is to coordinate German diplomacy, and study the information passed on from the embassies, permanent representations and consulates.
Foreign Office of Germany 
 The Foreign Office has 145 embassies, 59 consulates general, twelve permanent representations (at international organisations) and ten offices abroad.
Foreign Office of Germany 
 There are also three "German Information Centres (GIC)" with the job of giving information about Germany and the German language.
Foreign Office of Germany 
 The Bonn office also arranges communications for the Foreign Minister and the Chancellorwhen they are abroad.
Foreign Office of Germany 
 This is because the Foreign Office does not publish the qualifications of its top diplomats anymore.
Foreign Office of Germany 
 They stopped after terrorists used the information to attack the German embassy in Stockholm in 1975 and the RAF murdered diplomat Gerold von Braunmühl in 1986.
Foreign Office of Germany 
 However the German federal states kept a considerable degree of independence in their own foreign policy.
Foreign Office of Germany 
 The head of this department was a permanent secretary who was also the permanent representative of the German Chancellor in the Foreign Office at the same time.
Foreign Office of Germany 
 The second department was responsible for trade, traffic, consulates, national law, civil law, the art and science, the private matters of Germans abroad, also, justice, police and Post Office, emigration, ship matters.
Foreign Office of Germany 
 The permanent secretary no longerThe minister had the sole responsibility for the foreign policy now.
Foreign Office of Germany 
 Gustav Stresemann was the most famous foreign minister of this time, and moulded German foreign policy just like Bismarck had done during the empire.
Foreign Office of Germany 
 However, there was some resistance, especially from people like Adam von Trott zu Solz and Ulrich von Hassell.
Foreign Office of Germany 
 The Foreign Office wrote a formal letter about the Jews and foreign policy in 1939: It said that giving the Jews a homeland in Palestine was dangerous to world peace.
Foreign Office of Germany 
 This note is a big reason why the second set of Nuremberg Trials included officials from the Foreign Office.
Foreign Office of Germany 
 This meant that there was no need for a Foreign Office until 1951, when the new Germany got more control overs its own affairs.
Foreign Office of Germany 
 in fact More ex party members were in charge parts of the Foreign Office than there were party members doing the same type of job during the Third Reich.
Foreign Office of Germany 
 Since 1966 the Foreign Minister has often been the leader of the smaller coalition partner in coalition governments.
Foreign Office of Germany 
 Konrad Adenauer as the first Foreign Secretary of the Federal Republic of Germany and Helmut Schmidt, after FDP had left coalition and cabinet.
Burin Peninsula 
 The Burin Peninsula is a Canadian peninsula found on the south coast of the island of Newfoundland in the province of Newfoundland and Labrador.
Bonavista Peninsula 
 The Bonavista Peninsula is a large peninsula on the east coast of the island of Newfoundland in the Canadian province of Newfoundland and Labrador.
Districts of Switzerland 
 Some are called Ämter (Lucerne), Amtsbezirke (Bern), district (in French) or distretto (Tessin and part of Graubünden).
Districts of Switzerland 
 Canton of Uri is not divided into districts: the municipality is the next lowest unit of government.
Districts of Switzerland 
 The Canton of Schwyz is divided into six districts and 30 municipalities, although the districts Einsiedeln, Küssnacht and Gersau simply comprise the municipality of the same name.
Districts of Switzerland 
 Canton of Glarus is not divided into districts: the municipality is the next lower unit of government.
Districts of Switzerland 
 From 2005, Solothurn's ten districts are combined in pairs into five electoral districts, called Amtei.
Districts of Switzerland 
 Feuerschaugemeinde is a special-purpose municipality for firefighting, energy and water for the town Appenzell.
Districts of Switzerland 
 Broye-Vully (which will combine the districts of Avenches and Payerne, and part of the districts of Moudon and Oron)
Districts of Switzerland 
 Gros-de-Vaud (which will combine the district of Echallens, and part of the districts of Cossonay, Moudon, and Oron)
Cape Race 
 Cape Race is a point of land at the southeastern tip of the Avalon Peninsula, on the island of Newfoundland, Canada.
Cape Race 
 The Cape appeared on early sixteenth century maps as Cape Raso, and may derive from a cape of the same name at the mouth of the Tagus River in Portugal.