wanyu/IteraTeR_v2 huggingface dataset:
Original:  Respiratory Research 8:63 (free full text article)  External links Information on cabinless plethysmography for lung function testing Information on pulmonary function testing and physician reimbursement Information on plethysmography used in preclinical research
Revised:  Respiratory Research 8:63 (free full text article) External links Information on cabinless plethysmography for pulmonary function testing Information on pulmonary function testing and physician reimbursement Information on plethysmography used in preclinical research
Edit intent: fluency
Original: Ernesto Castro Aldana is a Salvadoran politician who currently serves as the incumbent President of the Legislative Assembly of El Salvador.
Revised: Ernesto Castro Aldana is a Salvadoran politician who is currently the incumbent President of the Legislative Assembly of El Salvador.
Edit intent: clarity
Original:  From 2012 to 2015, Castro served as the Secretary and Private Advisor to the Municipal Mayor of Nuevo Cuscatlán, who was then Nayib Bukele.
Revised:  From 2012 to 2015, Castro was the secretary and private advisor to the municipal mayor of Nuevo Cuscatlán, who was then Nayib Bukele.
Edit intent: fluency
Original:  Castro became the Private Secretary to President Bukele on 1 June 2019.
Revised:  Castro became the private secretary to President Bukele on 1 June 2019.
Edit intent: fluency
Original:  In the 2021 Salvadoran legislative election, Castro was elected as a Deputy to the Legislative Assembly of El Salvador from the department of San Salvador.
Revised:  In the 2021 Salvadoran legislative election, Castro was elected as a deputy to the Legislative Assembly of El Salvador from the department of San Salvador.
Edit intent: fluency
Original: Tides in Marginal Seas Tides are water level variations caused by the gravitational interaction between the moon, the sun and the earth.
Revised: Tides are water level variations caused by the gravitational interaction between the moon, the sun and the earth.
Edit intent: clarity
Original:  Tidal propagation along coasts After entering the continental shelf, a tidal wave quickly faces a boundary in the form of a landmass.
Revised: Internal tide and mixing At the continental shelf the reflection and transmission of the tidal wave can lead to the generation of internal tides on the pycnocline. The surface (i.e. barotropic) tide generates these internal tides where stratified waters are forced upwards over a sloping bottom topography. The internal tide extracts energy from the surface tide and propagates both in shoreward and seaward direction. The shoreward propagating internal waves shoals when reaching shallower water where the wave energy is dissipated. The shoaling of the internal tide drives mixing across the pycnocline, high levels carbon sequestration and sediment resuspension. Furthermore, through nutrient mixing the shoaling of the internal tide has a fundamental control on the functioning of ecosystems on the continental margin. Tidal propagation along coasts After entering the continental shelf, a tidal wave quickly faces a boundary in the form of a landmass.
Edit intent: clarity
Original:  The tidal currents are shown in lower panel of figure 2.
Revised:  The tidal currents ( lower panel of figure 2.
Edit intent: clarity
Original: where is the zonal velocity ( direction), the meriodional velocity ( direction), is time and is the coriolis frequency.
Revised: where is the zonal velocity ( direction), the meridional velocity ( direction), is time and is the coriolis frequency.
Edit intent: fluency
Original: where is the zonal velocity ( direction), the meriodional velocity ( direction), is time and is the coriolis frequency.
Revised: where is the zonal velocity ( direction), the meriodional velocity ( direction), is time and is the Coriolis frequency.
Edit intent: fluency
Original:  On the closed side the reflection happens through the creation of Poincare waves which are not modeled here.
Revised:  On the closed side the reflection happens through the creation of Poincare waves which are not modelled here.
Edit intent: fluency
Original:  The colors are indicated in the color bar, the arrows are scaled velocity vectors.
Revised:  The colours are indicated in the color bar, the arrows are scaled velocity vectors.
Edit intent: fluency
Original:  The colors are indicated in the color bar, the arrows are scaled velocity vectors.
Revised:  The colors are indicated in the colour bar, the arrows are scaled velocity vectors.
Edit intent: fluency
Original:  | 620x620px The expression of tides as a bounded Kelvin wave is well observable in enclosed shelf seas around the world (e.g. the English channel, the North Sea or the Yellow sea).
Revised:  | The expression of tides as a bounded Kelvin wave is well observable in enclosed shelf seas around the world (e.g. the English channel, the North Sea or the Yellow sea).
Edit intent: coherence
Original:  The sea surface height (SSH  ), the tidal elevation, is maximum at the coast and decreases towards the center of the domain.
Revised:  The sea surface height (SSH ), the tidal elevation, is maximum at the coast and decreases towards the centre of the domain.
Edit intent: fluency
Original:  They are both maximum under the crest and the trough of the waves and decrease towards the center .
Revised:  They are both maximum under the crest and the trough of the waves and decrease towards the centre .
Edit intent: fluency
Original:  The final pattern of  SSH and the tidal currents are made up of the sum of the two Kelvin waves.
Revised:  The final pattern of the SSH and the tidal currents are made up of the sum of the two Kelvin waves.
Edit intent: fluency
Original:  The final pattern of  SSH and the tidal currents are made up of the sum of the two Kelvin waves.
Revised:  The final pattern of SSH and the tidal currents is made up of the sum of the two Kelvin waves.
Edit intent: fluency
Original:  The reflected wave amplitude has decreased and as a result the Amphidromic points shifted towards the top side of the panel .
Revised:  The reflected wave amplitude has decreased and as a result the Amphidromic points shift towards the side of the panel .
Edit intent: clarity
Original:  Channel convergence increases the tidal amplitude and phase seed as the energy of the tidal wave is traveling through a smaller area while bottom friction decrease the amplitude through energy loss.
Revised:  Channel convergence increases the tidal amplitude and phase speed as the energy of the tidal wave is traveling through a smaller area while bottom friction decrease the amplitude through energy loss.
Edit intent: fluency
Original:  and the Eastern Upwelling Zone;
Revised:  And the Eastern Upwelling Zone;
Edit intent: fluency
Original:   Wind 357x357px|Seasonal differences in wind and connected SST the trade winds that blow over the southern Caribbean Sea (also called the low-level jet ) generate northward Ekman transport.
Revised:  Wind 357x357px|Seasonal differences in wind and connected SST the trade winds that blow over the southern Caribbean Sea (also called the low-level jet generate northward Ekman transport.
Edit intent: coherence
Original:  Upwelling over wide and shallow continental shelves can generate resuspension and transport of essential microelements from the benthic boundary layer to the surface   .
Revised:  Upwelling over wide and shallow continental shelves can generate resuspension and transport of essential microelements from the benthic boundary layer to the surface . .
Edit intent: fluency
Original:  386x386px|A comparison between the WUZ and EUZ showing the minimum and maximum values for: Wind speed (W), Turbulence (Turb), alongshore wind speed (alongW), Offshore Ekman transport due too wind (offshET).
Revised:  386x386px|A comparison between the WUZ and EUZ showing the minimum and maximum values for: Wind speed (W), Turbulence (Turb), alongshore wind speed (alongW), Offshore Ekman transport due to wind (offshET).
Edit intent: fluency
Original:  Vertical transport due too Ekman pumping intergrated too 100k offshore (EP100), Sea Surface Temperature (SST), chlorophyll-a(Chl).
Revised:  Vertical transport due to Ekman pumping integrated to 100k offshore (EP100), Sea Surface Temperature (SST), chlorophyll-a(Chl).
Edit intent: fluency
Original:  Wind 357x357px|Seasonal differences in wind and connected SST. b and c show the wind in December and SST that comes with it. d and e show the same in February.
Revised:  Wind 357x357px|Seasonal differences in wind and connected SST. (b) and (c) show the wind in December and SST that comes with it. d and e show the same in February.
Edit intent: coherence
Original:  Wind 357x357px|Seasonal differences in wind and connected SST. b and c show the wind in December and SST that comes with it. d and e show the same in February.
Revised:  Wind 357x357px|Seasonal differences in wind and connected SST. b and c show the wind in December and SST that comes with it. (d) and (e) show the same in February.
Edit intent: coherence
Original: Memory of Mankind on the URL is a time capusle that will go to the moon in 2021 on Astrobotic Technology's Peregrine URL in 2021.
Revised: Memory of Mankind on the Moon is a time capusle that will go to the moon in 2021 on Astrobotic Technology's Peregrine URL in 2021.
Edit intent: fluency
Original: Memory of Mankind on the Moon is a time capusle that will go to the moon in 2021 on Astrobotic Technology's Peregrine URL in 2021.
Revised: Memory of Mankind on the Moon is a time capusle that will go to the moon in 2021 on Astrobotic Technology's Peregrine lander in 2021.
Edit intent: clarity
Original:  It is made in colaberation with Hungarian company Puli Space URL and Memory of Mankind.
Revised:  It is made in colaberation with Hungarian company Puli Space Technologies and Memory of Mankind.
Edit intent: fluency
Original: Finnish Ukranians are Ukranians living in Finland and their offspring. in 2020 5 961 people spoke Ukranian in Finland.
Revised: Finnish Ukrainians are Ukrainians living in Finland and their offspring. in 2020 5 961 people spoke Ukranian in Finland.
Edit intent: style
Original: Finnish Ukranians are Ukranians living in Finland and their offspring. in 2020 5 961 people spoke Ukranian in Finland.
Revised: Finnish Ukranians are Ukranians living in Finland and their offspring. in 2020 5 961 people spoke Ukrainian in Finland.
Edit intent: fluency
Original:  Most Ukranians live in Helsinki, Tampere, Jyväskylä, Turku, Oulu and Salo.
Revised:  Most Ukrainians live in Helsinki, Tampere, Jyväskylä, Turku, Oulu and Salo.
Edit intent: fluency
Original:  There is a Finnish-Ukranian organization in Finland created in 1997.
Revised:  There is a Finnish-Ukrainian organization in Finland created in 1997.
Edit intent: fluency
Original:  History Since June 1918 about 60 Ukranians lived in Finland.
Revised:  History Since June 1918 about 60 Ukrainians lived in Finland.
Edit intent: fluency
Original:  However the amount of Ukranians in Finland for almost 70 years was unknown untill 1992.
Revised:  However the amount of Ukrainians in Finland for almost 70 years was unknown untill 1992.
Edit intent: fluency
Original:  However the amount of Ukranians in Finland for almost 70 years was unknown untill 1992.
Revised:  However the amount of Ukranians in Finland for almost 70 years was unknown until 1992.
Edit intent: fluency
Original: Kyrre was killed in mysterious circumstances . in November 1960 at his summer villa in Gladsaxe near Copenhagen.
Revised: Kyrre was killed in mysterious circumstances in November 1960 at his summer villa in Gladsaxe near Copenhagen.
Edit intent: fluency
Original:  ISBN 951-23-0844-4. fi After the  Moscow armistice in 1944, Kyrre set up a secret radio station in the attic of his Helvar radio factory in Pitäjänmäki, Helsinki, to send reports from German agents operating in Finland to Germany.
Revised:  ISBN 951-23-0844-4. fi After the armistice After the Moscow armistice in 1944, Kyrre set up a secret radio station in the attic of his Helvar radio factory in Pitäjänmäki, Helsinki, to send reports from German agents operating in Finland to Germany.
Edit intent: fluency
Original: Thoralf Kyrre (1913 - 27 November 1960 in Copenhagen, Denmark) was a Danish engineer who was involved in the Pro-German resistance movement in Finland in 1944-1945.
Revised: Thoralf Kyrre (1913 – 27 November 1960 in Copenhagen, Denmark) was a Danish engineer who was involved in the Pro-German resistance movement in Finland in 1944-1945.
Edit intent: fluency
Original: Thoralf Kyrre (1913 - 27 November 1960 in Copenhagen, Denmark) was a Danish engineer who was involved in the Pro-German resistance movement in Finland in 1944-1945.
Revised: Thoralf Kyrre (1913 - 27 November 1960 in Copenhagen, Denmark) was a Danish engineer who was involved in the Pro-German resistance movement in Finland in 1944–1945.
Edit intent: fluency
Original:  During the Continuation War  Kyrre worked for the secret police ValPo led by Arno Anthoni;
Revised:  During the Continuation War , Kyrre worked for the secret police ValPo led by Arno Anthoni;
Edit intent: fluency
Original:  Lars Westerlund) Kansallisarkisto, Helsinki 2011, Kyrrestä ss. 287-291 Poikonen was later caught and sentenced in August 1946 to two and a half years imprisonment, but Kyrre hid in Finland for ten months and on 25 january 1946 crossed the Tornio river to Sweden.
Revised:  Lars Westerlund) Kansallisarkisto, Helsinki 2011, Kyrrestä ss. 287-291 Poikonen was later caught and sentenced in August 1946 to two and a half years imprisonment, but Kyrre hid in Finland for ten months and on 25 January 1946 crossed the Tornio river to Sweden.
Edit intent: fluency
Original:  The letter wished for “ a rapid collapse of your department ” . Petter Forsström, Director of Lohjan Kalkkitehdas Oy served as the funder of the getaway and was also involved in the planning of the getaways.
Revised:  The letter wished for " a rapid collapse of your department ” . Petter Forsström, Director of Lohjan Kalkkitehdas Oy served as the funder of the getaway and was also involved in the planning of the getaways.
Edit intent: fluency
Original:  The letter wished for “ a rapid collapse of your department ” . Petter Forsström, Director of Lohjan Kalkkitehdas Oy served as the funder of the getaway and was also involved in the planning of the getaways.
Revised:  The letter wished for “ a rapid collapse of your department " . Petter Forsström, Director of Lohjan Kalkkitehdas Oy served as the funder of the getaway and was also involved in the planning of the getaways.
Edit intent: fluency
Original:  The letter wished for “ a rapid collapse of your department ” . Petter Forsström, Director of Lohjan Kalkkitehdas Oy served as the funder of the getaway and was also involved in the planning of the getaways.
Revised:  The letter wished for “ a rapid collapse of your department ” . Petter Forsström, Director of , served as the funder of the getaway and was also involved in the planning of the getaways.
Edit intent: clarity
Original: Valpo arrested Kyrre and Poikonen after the Helvar radio station was discovered on January 23 , 1945.
Revised: Valpo arrested Kyrre and Poikonen after the Helvar radio station was discovered on 23 , 1945.
Edit intent: clarity
Original:  Pohjonen 2000, 25 On March 16 , 1945 , they managed to escape with the help of the sympathetic Valpo detective Urho Gunnar Rantala.
Revised:  Pohjonen 2000, 25 On 16 , 1945 , they managed to escape with the help of the sympathetic Valpo detective Urho Gunnar Rantala.
Edit intent: clarity
Original:  Pohjonen 2000, 25 On March 16 , 1945 , they managed to escape with the help of the sympathetic Valpo detective Urho Gunnar Rantala.
Revised:  Pohjonen 2000, 25 On March 16 , 1945 they managed to escape with the help of the sympathetic Valpo detective Urho Gunnar Rantala.
Edit intent: fluency
Original:  On December 6 , 1948 , he sent a mocking letter to Valpo.
Revised:  On 6 , 1948 , he sent a mocking letter to Valpo.
Edit intent: style
Original:  On December 6 , 1948 , he sent a mocking letter to Valpo.
Revised:  On December 6 , 1948 he sent a mocking letter to Valpo.
Edit intent: fluency
Original:  Being clandestinely infiltrated by RPF Inkotanyi soldiers, the Interahamwe was secretly used by RPF of Kagame since 1992 until the end of the genocide.
Edit intent: coherence
Original: Geoconservation in the UK In the late 1970s, the former Nature Conservancy Council initiated the Geological Conservation Review (GCR), a comprehensive assessment of the key geological and geomorphological sites within England, Scotland and Wales, a task which was largely completed by 1990.
Revised: In the UK In the late 1970s, the former Nature Conservancy Council initiated the Geological Conservation Review (GCR), a comprehensive assessment of the key geological and geomorphological sites within England, Scotland and Wales, a task which was largely completed by 1990.
Edit intent: fluency
Original:  Originally referred to as Regionally important geological sites, the term 'Local Geological Sites' (or LoGS) is now in use for them in England and 'Local Geodiversity Sites' in Scotland whilst in Wales they are referred to as 'Regionally Important Geodiversity Sites (or RIGS).
Revised:  Originally referred to as regionally important geological sites, the term 'Local Geological Sites' (or LoGS) is now in use for them in England and 'Local Geodiversity Sites' in Scotland whilst in Wales they are referred to as 'Regionally Important Geodiversity Sites (or RIGS).
Edit intent: fluency
Original:  Over 3000 sites across Britain were identified and many are now designated as SSSIs thus providing them with statutory protection.
Revised:  Over 3000 sites across Britain were identified and many are now designated as sites of special scientific interest (SSSIs), thus providing them with statutory protection.
Edit intent: clarity
Original:  Originally referred to as regionally important geological sites, the term 'Local Geological Sites' (or LoGS) is now in use for them in England and 'Local Geodiversity Sites' in Scotland  whilst in Wales  they are referred to as 'Regionally Important Geodiversity Sites  (or RIGS).
Revised:  Originally referred to as regionally important geological sites, the term 'Local Geological Sites' (or LoGS) is now in use for them in England and 'Local Geodiversity Sites' in Scotland , whilst in Wales they are referred to as 'Regionally Important Geodiversity Sites (or RIGS).
Edit intent: fluency
Original:  Originally referred to as regionally important geological sites, the term 'Local Geological Sites' (or LoGS) is now in use for them in England and 'Local Geodiversity Sites' in Scotland  whilst in Wales  they are referred to as 'Regionally Important Geodiversity Sites  (or RIGS).
Revised:  Originally referred to as regionally important geological sites, the term 'Local Geological Sites' (or LoGS) is now in use for them in England and 'Local Geodiversity Sites' in Scotland whilst in Wales , they are referred to as 'Regionally Important Geodiversity Sites (or RIGS).
Edit intent: fluency
Original:  Originally referred to as regionally important geological sites, the term 'Local Geological Sites' (or LoGS) is now in use for them in England and 'Local Geodiversity Sites' in Scotland  whilst in Wales  they are referred to as 'Regionally Important Geodiversity Sites  (or RIGS).
Revised:  Originally referred to as regionally important geological sites, the term 'Local Geological Sites' (or LoGS) is now in use for them in England and 'Local Geodiversity Sites' in Scotland whilst in Wales they are referred to as 'Regionally Important Geodiversity Sites ' (or RIGS).
Edit intent: fluency
Original: Conditions that predispose a region to convection The ocean convection exists under certain conditions .
Revised: Convection exists under certain conditions .
Edit intent: clarity
Original:  Thus, the most preferred regions are open oceans which are adjacent to boundaries, where either dry and cold winds or ice surfaces blow over water, inducing large latent heat and moisture fluxes.
Revised:  This may be observed in oceans which are adjacent to boundaries, where either dry and cold winds or ice surfaces blow over water, inducing large latent heat and moisture fluxes.
Edit intent: clarity
Original:  Also, the ocean convection depends on the weakness of the stratification under the surface mixed layer.
Revised:  Ocean convection depends on the weakness of the stratification under the surface mixed layer.
Edit intent: clarity
Original:  Also, the ocean convection depends on the weakness of the stratification under the surface mixed layer.
Revised:  Also, the ocean convection depends on the weakness of stratification under the surface mixed layer.
Edit intent: fluency
Original:  Lastly, these stratified water layers must rise, near to the surface resulting in their direct exposition to intense surface forcing.
Revised:  These stratified water layers must rise, near to the surface resulting in their direct exposition to intense surface forcing.
Edit intent: coherence
Original:  Major convection sites Deep convection is observed in the subpolar North Atlantic (the Greenland Sea and the Labrador Sea), in  Weddell Sea in the southern hemisphere as well as in the northwestern Mediterranean.
Revised:  Major convection sites Deep convection is observed in the subpolar North Atlantic (the Greenland Sea and the Labrador Sea), in the Weddell Sea in the southern hemisphere as well as in the northwestern Mediterranean.
Edit intent: fluency
Original:  The Greenland Sea has common aspects with the Labrador Sea but also differs because of the important role of ice in preconditioning during the months November until February.
Revised:  The Greenland Sea differs from the Labrador Sea but also differs because of the important role of ice in preconditioning during the months November until February.
Edit intent: clarity
Original:  The Greenland Sea has common aspects with the Labrador Sea but also differs because of the important role of ice in preconditioning during the months November until February.
Revised:  The Greenland Sea has common aspects with the Labrador Sea because of the important role of ice in preconditioning during the months November until February.
Edit intent: coherence
Original:  In the north-western Mediterranean Sea, the deep convection occurs in winter, when the water undergoes the necessary preconditioning with air-sea fluxes inducing buoyancy losses at the surface.
Revised:  In the northwestern Mediterranean Sea, the deep convection occurs in winter, when the water undergoes the necessary preconditioning with air-sea fluxes inducing buoyancy losses at the surface.
Edit intent: fluency
Original:  In the north-western Mediterranean Sea, the deep convection occurs in winter, when the water undergoes the necessary preconditioning with air-sea fluxes inducing buoyancy losses at the surface.
Revised:  In the north-western Mediterranean Sea, deep convection occurs in winter, when the water undergoes the necessary preconditioning with air-sea fluxes inducing buoyancy losses at the surface.
Edit intent: clarity
Original:  Phases of convection The ocean convection is distinguished in three phases: preconditioning, deep convection and lateral exchange and spreading.
Revised:  Phases of convection Ocean convection is distinguished in three phases: preconditioning, deep convection and lateral exchange and spreading.
Edit intent: clarity
Original:  Phases of convection The ocean convection is distinguished in three phases: preconditioning, deep convection and lateral exchange and spreading.
Revised:  Phases of convection The ocean convection is distinguished by three phases: preconditioning, deep convection and lateral exchange and spreading.
Edit intent: fluency
Original:  Cooling events lead to the second phase, namely deep convection, in which a part of the fluid column may overturn in numerous plumes that distribute the dense surface water in the vertical axis.
Revised:  Cooling events lead to the second phase, deep convection, in which a part of the fluid column may overturn in numerous plumes that distribute the dense surface water in the vertical axis.
Edit intent: clarity