the-french-artist/wikipedia_20220301.simple_sentence_embeddings huggingface dataset:
2011 Pacific typhoon season 
 However, the JMA continued to track the remants as a weak tropical depression over the next few days until the system dissipated on August 15.
2011 Pacific typhoon season 
 Late on August 8, the JMA upgraded an area of low pressure to a tropical depression, to the northwest of Minamitorishima.
2011 Pacific typhoon season 
 On August 10, the system was caught in a moderate vertical wind shear and due to cold sea surface temperature, the system dissipated into a remnant low.
2011 Pacific typhoon season 
 Early on August 20, the system developed a broad area of low level circulation center and a good divergence aloft becoming more well defined.
2011 Pacific typhoon season 
 Later that day, the JMA upgraded the system to a tropical depression southeast of the Bonin Islands.
2011 Pacific typhoon season 
 On August 22, the system started interacting with an anticyclone and was exposed to a strong vertical wind shear, prompting the JMA to stop monitoring the system as a tropical depression, as the system dissipated to a remnant low.
2011 Pacific typhoon season 
 However, at midnight, the same day, the remnants regenerated, and the JMA started tracking the system as a tropical depression again, until it last appeared near Okinawa, Japan on August 25, as the system dissipated completely.
2011 Pacific typhoon season 
 Early on August 20, the system became more better organized and developed a low-level circulation center.
2011 Pacific typhoon season 
 The system then turned north and continued to drift north until on August 21, when the JMA upgraded the low pressure area to a tropical depression east of Philippines.
2011 Pacific typhoon season 
 The JTWC also issued a Tropical Cyclone Formation Alert (TCFA) on the system reporting that the system was becoming more well organized.
2011 Pacific typhoon season 
 Later that day, the PAGASA started monitoring the system as a tropical depression and named it Mina.
2011 Pacific typhoon season 
 Late on August 22, the system became more well organized prompting the JTWC to initiate advisories on the system, designating it with 14W. On August 23, the JMA upgraded 14W to a tropical storm, naming it Nanmadol.
2011 Pacific typhoon season 
 Overnight, the system continued to intensify and early on August 24, the JMA upgraded Nanmadol to a severe tropical storm.
2011 Pacific typhoon season 
 Nanmadol continued to drift northeast and made landfall over Gonzaga, Cagayan, Philippines with strong winds of over .
2011 Pacific typhoon season 
 Nanmadol weakened significantly after interacting with land and early on August 28, the JMA downgraded Nanmadol to a severe tropical storm.
2011 Pacific typhoon season 
 Late on August 28, Nanmadol made its second landfall over Taimali in the Taitung County of Taiwan and started weakening.
2011 Pacific typhoon season 
 Landfall weakened the system rapidly prompting the JMA to downgrade Nanmadol to a tropical storm with winds of under .
2011 Pacific typhoon season 
 After its third landfall over Fujian, China, Nanmadol weakened rapidly prompting both the JTWC and the JMA to issue their final warnings on the system.
2011 Pacific typhoon season 
 At least two Filipino fishermen were reported to be missing after Nanmadol's strong winds whipped up large waves.
2011 Pacific typhoon season 
 At midnight that day, the system became sufficiently well organized that the JMA started tracking it as a tropical depression.
2011 Pacific typhoon season 
 On August 23, the system moved into an environment of low wind shear and warm sea surface temperatures prompting the JTWC to issued a TCFA on it.
2011 Pacific typhoon season 
 By August 25, the system grew strong enough that the JMA upgraded it to a tropical storm, naming it Talas.
2011 Pacific typhoon season 
 Over the next few days, Talas continued to drift north very slowly until late on August 29, when the JMA upgraded Talas to a typhoon.
2011 Pacific typhoon season 
 Soon, a subtropical ridge to the west of the storm weakened and the subtropical ridge to the east of the system pushed Talas to the west.
2011 Pacific typhoon season 
 An upper-level cyclone over the system suppressed the convection and kept it from reaching the center.
2011 Pacific typhoon season 
 Convection never managed to consolidate the center and convective banding remained well away from the fully exposed low-level circulation center.
2011 Pacific typhoon season 
 The convective banding continued to expand more and more with the outer rainbands already brushing parts of Japan.
2011 Pacific typhoon season 
 Coastal areas in the nation have already reported gale-force winds several hours before landfall, while the Omega block continued to drive Talas towards the nation.
2011 Pacific typhoon season 
 Land interaction weakened Talas, prompting the JMA to downgrade Talas from a typhoon to a severe tropical storm with winds of under .
2011 Pacific typhoon season 
 After landfall, Talas accelerated north at over  and its central convection became significantly eroded and was displaced to the northeast as Talas was exposed to a very strong wind shear of over  that made the LLCC very distorted and difficult to pin-point.
2011 Pacific typhoon season 
 Talas was embedded in a baroclinic zone and the JTWC anticipated an extratropical transition, which prompted them to issue their final warning on the system.
2011 Pacific typhoon season 
 On September 5, the JMA issued their final warning on the system, reporting that Talas has become extratropical on the Sea of Japan.
2011 Pacific typhoon season 
 Soon, the system developed a well-defined but partially exposed low-level circulation center (LLCC), prompting the JTWC to issue a tropical cyclone formation alert.
2011 Pacific typhoon season 
 On September 3, the central convection around the LLCC deepened with favorable equatoward outflow prompting the JTWC to initiate advisories on the system, designating it with 16W. Soon, 16W accelerated north at over  with its LLCC being being consolidated by convection.
2011 Pacific typhoon season 
 Also, data from an ASCAT scatterometer pass revealed that the LLCC was tightly wrapped with  winds prompting the JTWC to upgrade 16W to a tropical storm.
2011 Pacific typhoon season 
 An Aqua microwave imagery depicted that the LLCC remained partially exposed though consolidated with deep central convection.
2011 Pacific typhoon season 
 Albeit in an area of moderate vertical wind shear, an anticyclone enhanced northeastward outflow while a tropical upper tropospheric trough (TUTT cell) suppressed the outflow towards the west.
2011 Pacific typhoon season 
 As 16W continued to accelerate north at a staggering , convective banding became fragmented and detached behind the main area of central convection.
2011 Pacific typhoon season 
 However, the outflow to the southeast of the storm remained favorable and 16W continued to strengthen, prompting the JMA upgraded the system to a tropical storm, naming it Noru.
2011 Pacific typhoon season 
 Late on September 4, Noru's LLCC that remained partially exposed since formation unexpectedly became elongated and started weakening.
2011 Pacific typhoon season 
 However, data from an ASCAT scatterometer pass depicted that the LLCC had an expansive area of strong tropical storm force winds along the eastern and northern peripheries.
2011 Pacific typhoon season 
 Soon, the convective banding, which was already fragmented started becoming disorganized causing Noru to start weakening.
2011 Pacific typhoon season 
 The TUTT cell moved over Noru snuffing outflow in all directions and sheared the remnant central convection, prompting the JTWC to downgrade Noru to a tropical depression.
2011 Pacific typhoon season 
 However, data from an scatterometer pass depicted that Noru had winds of over  near the center, prompting the JTWC to reupgrade the system to a tropical storm.
2011 Pacific typhoon season 
 On September 5, Noru started to appear like a hybrid system, primarily showing subtropical characteristics.
2011 Pacific typhoon season 
 The JTWC added that Noru was undergoing an extratropical transition and would become an extratropical cyclone within 24 hours.
2011 Pacific typhoon season 
 Noru continued to transition into an extratropical cyclone with a broadening LLCC and weaker winds at the core, being embedded in an upper-level trough that suppressed the formation of convection within the LLCC.
2011 Pacific typhoon season 
 With the extratropical transition well underway, Noru drifted into an area of low sea surface temperatures and started weakening, prompting the JTWC to downgrade Noru to a tropical depression.
2011 Pacific typhoon season 
 On September 6, Noru finished the extratropical transition becoming an extratropical cyclone east-southeast of Hokkaido, Japan, prompting the JMA and the JTWC to issue their final warning on the system.
2011 Pacific typhoon season 
 Over the next two days, the system drifted north and developed a well defined LLCC with organized convective banding, prompting the JMA to upgrade the low pressure area to a tropical depression.
2011 Pacific typhoon season 
 On September 7, convection consolidated the low-level circulation center very well with tightly curved banding wrapped into it.
2011 Pacific typhoon season 
 Also, high sea-surface temperatures and very low wind shear caused the system to undergo rapid deepening, prior to which, the JMA upgraded the system to a tropical storm and named it Kulap.
2011 Pacific typhoon season 
 However, the system stopped strengthening soon after as the LLCC became partially exposed and the convection was displaced to the south.
2011 Pacific typhoon season 
 Kulap remained small in size and dry air entering from the western periphery kept it from strengthening further.
2011 Pacific typhoon season 
 On September 8, Kulap moved into the east-northeast periphery of the Philippine Area of Responsibility (PAR) prompting the PAGASA to start issuing advisories on the system, naming it Nonoy.
2011 Pacific typhoon season 
 However, Kulap quickly accelerated north and exited the PAR on the same evening, prompting the PAGASA to issued their final advisory on the system.
2011 Pacific typhoon season 
 After increasing wind shear caused further weakening, the JTWC downgraded Kulap to a tropical depression late on September 8.
2011 Pacific typhoon season 
 Early on September 10, the JMA too downgraded Kulap to a tropical depression, and continued to track Kulap's remnants as a tropical depression until it finally dissipated early on September 11.
2011 Pacific typhoon season 
 Early on September 8, a cluster of thunderstorms came together as a low pressure area with imporoving outflow and a developing low-level circulation center (LLCC).
2011 Pacific typhoon season 
 Later that day, the JMA upgraded the low pressure area to a tropical depression north-northeast of the Northern Mariana Islands.
2011 Pacific typhoon season 
 Over the next two days, the system gradually drifted west and intensified slightly, prompting the JTWC to issue a Tropical Cyclone Formation Alert (TCFA) on it.
2011 Pacific typhoon season 
 Convection gradually consolidated the LLCC and the JTWC initiated advisories on the system on September 11, designating it with 18W. The next day, the depression drifted into the Philippine Area of Responsibility (PAR) and the PAGASA initiated advisories on the depression, naming it Onyok.
2011 Pacific typhoon season 
 In an advisory, the JTWC reported that there were at-least two more vortices associated with the system, that caused an abrupt, erratic movement.
2011 Pacific typhoon season 
 However, being in an area of warm sea surface temperatures and low vertical wind shear, the depression continued to strengthen and on September 13, the JMA upgraded the depression to a tropical storm and named it Roke.
2011 Pacific typhoon season 
 On September 17, Roke developed a small, deep convective eye promoting the JMA to upgrade Roke to a severe tropical storm with winds of over .
2011 Pacific typhoon season 
 Between September 19 and 20, Roke underwent Explosive intensification, a more extreme case of rapid deepening that involves a tropical cyclone deepening at a rate of at least 2.5 mbar per hour for a minimum of 12 hours.
2011 Pacific typhoon season 
 Soon Roke started weakening as cloud tops started getting warmed up and eye diameter started to decrease.
2011 Pacific typhoon season 
 However, the system still maintained a near radial outflow and the convective structure continued to remain organized that kept Roke from dissipating rapidly.
2011 Pacific typhoon season 
 Although Roke entered a de-intensification phase, it still had plenty of strength that posed a great threat to regions of Japan.
2011 Pacific typhoon season 
 Being about  southwest of Yokosuka, Kanagawa, the typhoon accelerated north-northwestward at about  with winds of over  (1-min sustained) being a Category 3 typhoon on the SSHS.
2011 Pacific typhoon season 
 Also, land interaction severely weakened the storm to a minimal Category 1 typhoon with winds of under  (1-min sustained).
2011 Pacific typhoon season 
 Only six hours later, the storm further weakened and accelerated northeastward at about  with rapidly dissipating deep convection completely sheared to the northeast of the LLCC.
2011 Pacific typhoon season 
 The system gradually drifted north and steadily intensified until the next day when the JMA upgraded the system to a tropical depression.
2011 Pacific typhoon season 
 Later on September 14, the JTWC issued a Tropical Cyclone Formation Alert (TCFA) on the system reporting that the system could intensify into a tropical storm within 24 hours from then.
2011 Pacific typhoon season 
 Convection rapidly consolidated the center with persistent, deep convection around the northeastern periphery, prompting the JTWC to initiate advisories on the system, designating it with 19W. Soon, the JMA also initiated advisories on the system, upgrading it to Tropical Storm Sonca.
2011 Pacific typhoon season 
 In the begging, Sonca seemed to have intensified rapidly since formation, however, soon the storm weakened back to a minimal tropical storm because of dry air entering the LLCC that caused it to elongate and weaken.
2011 Pacific typhoon season 
 However, that was not for too long as vigorous convection persisted over the well defined LLCC with tightly curved banding wrapped in, Sonca continued to strengthen gradually and the JTWC reported winds of at-least  near the center.
2011 Pacific typhoon season 
 As Sonca continued to strengthen, and the JMA upgraded it to a severe tropical storm on September 17.
2011 Pacific typhoon season 
 Later that day, Sonca developed a large  ragged eye with deep convective banding tightly wrapped into it.
2011 Pacific typhoon season 
 On September 18, Sonca reached a peak intensity of  (1-min mean) and  (10-min mean) and soon the convection around the northern periphery started weakening.
2011 Pacific typhoon season 
 Being embedded in a baroclinic zone with low sea surface temperatures, Sonca started its extratropical transition late on September 19.
2011 Pacific typhoon season 
 The transition took place relatively fast because of a frontal boundary and the JTWC reported that Sonca became extratropical early on September 20, while the JMA did the same later in the evening.
2011 Pacific typhoon season 
 Early on September 14, the JMA started monitoring a cluster of thunderstorms to the southeast of Taiwan as a tropical depression.
2011 Pacific typhoon season 
 But because of the land interaction, the system could not be empowered and the JMA stopped tracking the depression late on September 15, as the system dissipated.
2011 Pacific typhoon season 
 The low gradually drifted west and became more well organized prompting the JTWC to issue a Tropical Cyclone Formation Alert (TCFA) on it.
2011 Pacific typhoon season 
 Later, the LLCC became well organized with flaring deep convection developing around it, so the JMA started monitoring the low as a tropical depression.
2011 Pacific typhoon season 
 Later on September 23, the JTWC also initiated advisories on the system designating it with 20W. Early on September 24, the JMA further upgraded 20W to a tropical storm and named it Nesat.
2011 Pacific typhoon season 
 Nesat continued to drift west with expanding deep convection around the entire system and consolidating convection around the LLCC.
2011 Pacific typhoon season 
 The mid-level warm anomaly near the system continued to intensify and convective banding near the LLCC became more and more tighter.
2011 Pacific typhoon season 
 On the evening of September 21, at almost the same time when Nesat was first seen, another low pressure area persisted far south of Hong Kong.
2011 Pacific typhoon season 
 The low slowly drifted north and strengthened slowly until on September 24, when the JMA upgraded the system to a tropical depression east of Vietnam.
2011 Pacific typhoon season 
 Later that day, the JTWC issued a Tropical Cyclone Formation Alert stating that the low could develop into a tropical cyclone.
2011 Pacific typhoon season 
 On September 26, the Japan Meteorological Agency (JMA) started to monitor a weak tropical depression.
2011 Pacific typhoon season 
 However less than 3 hours later, the JTWC designated it as Tropical Depression 22W. JMA reported that the depression had become a tropical storm and named it Nalgae.
2011 Pacific typhoon season 
 Nalgae developed a microwave eye like feature and well defined convective banding in all the quadrants.
2011 Pacific typhoon season 
 Nalgae quickly intensified on September 30, and became a category 4 super typhoon early on October 1.
2011 Pacific typhoon season 
 Due to land interaction and colder sea surface temperature in the South China Sea, the JMA downgraded Nalgae to a severe tropical storm on October 2.
2011 Pacific typhoon season 
 At least 18 people were killed by the storm and another 7 were reported as missing as of October 11.
2011 Pacific typhoon season 
 On October 7, the JTWC started monitoring a tropical disturbance about 750 km (465 mi) to the south of Hagåtña, Guam.
2011 Pacific typhoon season 
 Early on October 10, the JTWC upgraded the system to a tropical depression called 23W. The PAGASA also upgraded it to a tropical depression and named it Ramon.
2011 Pacific typhoon season 
 After passing Palau on December 15, both the JTWC and the JMA upgraded the system to a tropical storm.
2011 Pacific typhoon season 
 Within the Northwestern Pacific Ocean, there are two separate agencies who assign names to tropical cyclones which often results in a cyclone having two names.
2011 Pacific typhoon season 
 The Japan Meteorological Agency names tropical cyclones should they be judged to have 10-minute sustained windspeeds of 65 km/h, (40 mph), to the north of the equator between the 180° and 100°E. Whilst the Philippine Atmospheric, Geophysical and Astronomical Services Administration assigns names to tropical cyclones which move into or form as a tropical depression in their area of responsibility between 135°E and 115°E and between 5°N-25°N even if the cyclone has had a name assigned to it by the Japan Meteorological Agency.
2011 Pacific typhoon season 
 Tropical Cyclones are named from the following lists by the Regional Specialized Meteorological Centre in Tokyo, Japan, once they reach tropical storm strength.
2011 Pacific typhoon season 
 Each of the 14 nations or territories submitted 10 names, which are used in alphabetical order, by the English name of the country.
2011 Pacific typhoon season 
 The Philippine Atmospheric, Geophysical and Astronomical Services Administration uses its own naming scheme for tropical cyclones in their area of responsibility.
2011 Pacific typhoon season 
 PAGASA assigns names to tropical depressions that form within their area of responsibility and any tropical cyclone that might move into their area of responsibility.
2011 Pacific typhoon season 
 Should the list of names for a given year prove to be insufficient, names are taken from an auxiliary list, the first 10 of which are published each year before the season starts.
2011 Pacific typhoon season 
 During their 2012 annual session the ESCAP/WMO Typhoon Committee said that the name Washi would be retired from its naming lists.
2011 Pacific typhoon season 
 The Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) said that the names Bebeng, Juaning, Mina, Pedring were retired from PAGASA's list of local names after they each caused over 1 billion PHP in damages to the Philippines during 2011.
2011 Pacific typhoon season 
 The name Sendong was also retired from the list after it caused over 300 deaths, when it made landfall on the Philippines during December 2011.
2011 Pacific typhoon season 
 This table lists all the storms that developed in the western Pacific Ocean to the west of the International Date Line during the 2011 season.
2011 Pacific typhoon season 
 Broadly speaking, the ACE is a measure of the power of a typhoon multiplied by the length of time it existed, so storms that last a long time, as well as particularly strong typhoons, have high ACEs.
2011 Pacific typhoon season 
 ACE is calculated for only full advisories on specifically tropical systems reaching or exceeding wind speeds of 34 knots (63 km/h, 39 mph), or tropical storm strength.
2011 Pacific typhoon season 
 Later the JMA reexamines the data, and produces a final report on each storm, which can lead to the ACE for a storm being revised either upward or downward.
Pretty Fly for a Rabbi 
 "Pretty Fly for a Rabbi" (also called "Pretty Fly (For a Rabbi)" in Australia) is a song by "Weird Al" Yankovic.
You're Pitiful 
 "You're Pitiful" is a parody of "You're Beautiful" by James Blunt by parody musician "Weird Al" Yankovic.
You're Pitiful 
 Blunt's record label did not want Yankovic to release the song, so he put it on his website for a free download.
Stage (geology) 
 Technically, a stage is a succession of rock strata laid down in a single age on the geologic timescale, which usually represents millions of years of sedimentation or deposition.
Red beds 
 The term red beds usually refers to strata of reddish-colored sedimentary rocks such as sandstone, siltstone or shale that were deposited in hot climates under oxidizing conditions.
Red beds 
 Although they have been deposited throughout the Phanerozoic, they are most commonly associated with rocks deposited during the Devonian, Permian and Triassic periods.
Red beds 
 Red beds have economic significance since many of them contain reservoirs of petroleum and natural gas.
Red beds 
 Secondary red beds are linked to the uplift, erosion and surface weathering of previously deposited sediments and require conditions similar to primary red beds for their formation.
Red beds 
 "In modern times red beds are often found in low-latitude tropical climates, and they are always associated with oxidising conditions... the redbeds may be associated with rain forests or places where the rainfall is high but confined to monsoonal periods... A good model for red bed-producing conditions today is the Amazon basin.
Titanosaurus 
 Titanosaurus  was a genus of sauropod dinosaur, first described by Lydekker in 1877 from fragments, but not confirmed by later research.
Titanosaurus 
 Titanosaurus has traditionally been treated as a "wastebasket taxon" for poorly preserved sauropod remains.
First Minister and deputy First Minister 
 The First Minister and the deputy First Minister (Irish: Céad-Aire agus an leas-Chéad-Aire, Ulster Scots: Heid Männystèr an tha Heid Männystèr depute), (FM/dFM for short), are jobs in the Northern Ireland Government.
First Minister and deputy First Minister 
 The two positions are a diarchy, meaning they have equal power; both are nominated and appointed by members of the Northern Ireland Assembly.
First Minister and deputy First Minister 
 Before however, the incumbents were Peter Robinson of the Democratic Unionist Party as First Minister and Martin McGuinness of Sinn Féin as deputy First Minister.
First Minister and deputy First Minister 
 Members of the Northern Ireland Assembly are divided into two groups, Nationalists and Unionists (although there are also some independent or "Other" members).