wanyu/IteraTeR_full_sent huggingface dataset:
Original:  The direction of the wind is generally parallel to the southern Caribbean Sea margin , however, between May and October the EUZ has more along shore winds that are ~1.7° varying from the along-shore direction and during November until April the direction is more onshore within ±12°.
Revised:  The direction of the wind is generally parallel to the southern Caribbean Sea margin . However, between May and October the EUZ has more along shore winds that are ~1.7° varying from the along-shore direction and during November until April the direction is more onshore within ±12°.
Edit intent: fluency
Original:  Chlorophyll-a Chlorophyll a is used to see the productivity of phytoplankton and therefore zooplankton , amounts of chlorophyll-a increase with higher nutrient concentrations that are found in upwelled water and can therefore be used as a proxy for upwelling systems.
Revised:  Chlorophyll-a Chlorophyll a is used to see the productivity of phytoplankton and therefore zooplankton . Amounts of chlorophyll-a increase with higher nutrient concentrations that are found in upwelled water and can therefore be used as a proxy for upwelling systems.
Edit intent: fluency
Original:  These show a Chlorophyll-a maximum in December and April and a shorter maximum between June and July  . Biological impact Nutrient concentrations that come with the water from the SUW have a strong positive impact on the phytoplankton productivity , it is estimated that up to 95\% of the small pelagic biomass is the southern Caribbean sea is sustained by the primary production that comes with these upwelled waters.
Revised:  These show a Chlorophyll-a maximum in December and April and a shorter maximum between June and July further confirming the upwelling of nutrient rich water . Biological impact Nutrient concentrations that come with the water from the SUW have a strong positive impact on the phytoplankton productivity , it is estimated that up to 95\% of the small pelagic biomass is the southern Caribbean sea is sustained by the primary production that comes with these upwelled waters.
Edit intent: meaning-changed
Original:  These show a Chlorophyll-a maximum in December and April and a shorter maximum between June and July  . Biological impact Nutrient concentrations that come with the water from the SUW have a strong positive impact on the phytoplankton productivity , it is estimated that up to 95\% of the small pelagic biomass is the southern Caribbean sea is sustained by the primary production that comes with these upwelled waters.
Revised:  These show a Chlorophyll-a maximum in December and April and a shorter maximum between June and July . Biological impact Nutrient concentrations that come with the water from the SUW have a strong positive impact on the phytoplankton productivity . It is estimated that up to 95\% of the small pelagic biomass is the southern Caribbean sea is sustained by the primary production that comes with these upwelled waters.
Edit intent: fluency
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 The Caribbean low-level jet (CLLJ) The CLLJ has a core in the western basin (70°W - 80°W, 15°N) and maximum horizontal wind speeds of up to 16 m/s that tops in July and February. The Caribbean low-level jet is an amplification of the large-scale circulation of the North Atlantic subtropical high (NASH). The NASH interacts closely with the trade winds and therefor connects the CLLJ with the tradewinds .
Edit intent: meaning-changed
Original: The Southern Caribbean Upwelling system (SCUS) is a low latitude tropical upwelling system , a system where due to multiple environmental and bathymetric conditions water from the deep sea is forced to the surface layers  .
Revised: The Southern Caribbean Upwelling system (SCUS) is a low latitude tropical upwelling system . Where; due to multiple environmental and bathymetric conditions water from the deep sea is forced to the surface layers .
Edit intent: fluency
Original: The Southern Caribbean Upwelling system (SCUS) is a low latitude tropical upwelling system , a system where due to multiple environmental and bathymetric conditions water from the deep sea is forced to the surface layers  .
Revised: The Southern Caribbean Upwelling system (SCUS) is a low latitude tropical upwelling system , a system where due to multiple environmental and bathymetric conditions water from the deep sea is forced to the surface layers of the ocean .
Edit intent: clarity
Original:  The intensity of the Caribbean low-level jet (further explanation below) and the coastal orientation are determining the timing and spatial variability of this upwelling system. The system is likely to be responsible for a major part in the primary production due to the addition of nutrients that are added to the system through the upwelling. 427x427px |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 too wind (offshET).
Edit intent: meaning-changed
Original:  The system is likely to be responsible for a major part in the primary production due to the addition of nutrients that are added to the system through the upwelling. 427x427px |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:  The system is likely to be responsible for a major part in the primary production due to the addition of nutrients that are added to the system through the upwelling. 427x427px |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).
Edit intent: fluency
Original:   For thirty years after 1990, the upwelling has intensified which is producing cooling of the sea surface temperature (SST) in the WUZ, this is in contrast to the general temperature in the Caribbean sea which has shown to increase.
Revised:  General information For thirty years after 1990, the upwelling has intensified which is producing cooling of the sea surface temperature (SST) in the WUZ, this is in contrast to the general temperature in the Caribbean sea which has shown to increase.
Edit intent: coherence
Original:   Under the Caribbean surface waters more saline water is found with values close to those typical for the Subtropical Underwater (SUW) SA(salinity) ~37, Θ ~22 °C.
Revised:  The intensity of the Caribbean low-level jet (further explanation below) and the coastal orientation are determining the timing and spatial variability of this upwelling system. The system is likely to be responsible for a major part in the primary production due to the addition of nutrients that are added to the system through the upwelling. Under the Caribbean surface waters more saline water is found with values close to those typical for the Subtropical Underwater (SUW) SA(salinity) ~37, Θ ~22 °C.
Edit intent: meaning-changed
Original:  Characterization of the SCUS Sinces 1994 variations in upwelling are studied using cycles of satellite SST  . The SST this is used as a proxy for upwelling (explained in more detail below) in this tropical region As well as the dominant winds and chlorophyll a.
Revised:  Characterization of the SCUS Sinces 1994 variations in upwelling are studied using cycles of satellite SST (Sea surface Temperature) . The SST this is used as a proxy for upwelling (explained in more detail below) in this tropical region As well as the dominant winds and chlorophyll a.
Edit intent: meaning-changed
Original:  These are all proxies that are relatively easy to measure and quite easily accessible. 514x514px|Upwelling zones in the Southern Caribbean The Rossby radius  changes the positioning of the upwelling relative to the coastline.
Revised:  These are all proxies that are relatively easy to measure and quite easily accessible. 514x514px|Upwelling zones in the Southern Caribbean shown through SST Data. changes the positioning of the upwelling relative to the coastline.
Edit intent: meaning-changed
Original:  These are all proxies that are relatively easy to measure and quite easily accessible. 514x514px|Upwelling zones in the Southern Caribbean The Rossby radius  changes the positioning of the upwelling relative to the coastline.
Revised:  These are all proxies that are relatively easy to measure and quite easily accessible. 514x514px|Upwelling zones in the Southern Caribbean The Rossby radius Location and source of the SCUS The location of the SCUS is depending on the Rossby radius or R. The rossby radius changes the positioning of the upwelling relative to the coastline.
Edit intent: meaning-changed
Original:  Upwelled waters in the SCUS are consistent in geochemical compositions with the "Subtropical Underwater" , which is a water mass that comes from the central Atlantic and due to its relative dense water properties (SA (salinity) ~37g per kg water, Temperature ~22 °C) lays under the Caribbean surface waters , and is likely to come from this water mass.
Revised:  Upwelled waters in the SCUS are consistent in geochemical compositions with the "Subtropical Underwater" . This is a water mass that comes from the central Atlantic and due to its relative dense water properties (SA (salinity) ~37g per kg water, Temperature ~22 °C) lays under the Caribbean surface waters , and is likely to come from this water mass.
Edit intent: fluency
Original:  Upwelled waters in the SCUS are consistent in geochemical compositions with the "Subtropical Underwater" , which is a water mass that comes from the central Atlantic and due to its relative dense water properties (SA (salinity) ~37g per kg water, Temperature ~22 °C) lays under the Caribbean surface waters , and is likely to come from this water mass.
Revised:  Upwelled waters in the SCUS are consistent in geochemical compositions with the "Subtropical Underwater" , which is a water mass that comes from the central Atlantic and due to its relative dense water properties (SA (salinity) ~37g per kg water, Temperature ~22 °C) lays under the Caribbean surface waters . Because the properties are so similar to the water that is upwelled in the SCUS its likely that the water comes from this water mass.
Edit intent: coherence
Original:  The intensity of the trade winds varies per season ( image 2 shows the WUZ b) and c) in December and d) and e) in February) and explains the variation in upwelling and the measured differences in SST that are mentioned above.
Revised:  The intensity of the trade winds varies per season ( the image of the Seasonal differences shows the WUZ b) and c) in December and d) and e) in February) and explains the variation in upwelling and the measured differences in SST that are mentioned above.
Edit intent: meaning-changed
Original:  Literary sources Burmese chronicles and Buddhist apocryphal literature are now the primary sources of recorded Burmese mythology. The earliest known surviving work mentioning Burmese myths is Zatadawbon Yazawin ("The Royal Horoscopes Chronicle"), first written in the late 13th century by court astrologers. This chronicle relates the cosmogony and mythic origins of the world and Burma according to Buddhist mythology.
Revised:  Name Instructor Course Date
Edit intent: meaning-changed
Original:  Yazawin Kyaw (the Celebrated Chronicle) is the most famous surviving work, which mainly focuses on the mythological and religious matters of Myanmar. It was written in 16th century by Shin Maha Silvamsa and was mainly influenced by Mahavamsa and Dipavamsa, two much older histories. The work claims to be based on the records of the chronicles of the Burmese dynasties, which claimed to be the direct descendants from the Sakya clan of Lord Buddha, thus directly connecting themselves to the solar dynasty.
Revised:  DQ1: Should developing the disaster recovery plan enough to protect the organizational IT infrastructure? If yes or no, explain. No, I believe that a disaster recovery plan alone is insufficient to defend an organization's information technology infrastructure. Aside from the disaster recovery strategy, a company must pay close attention to some other essential factors to safeguard its infrastructure. For example, a disaster recovery strategy on its own is insufficient unless it is supported by appropriately educated and well-informed employees or users on matters concerning disaster recovery plans. It is well acknowledged that for a disaster recovery plan to be effective, it requires the participation of individuals. Competent individuals will be responsible for achieving the aims and objectives of the strategy by controlling how it should function and what effects should impose in ensuring that the infrastructure is secure. They are the people who are in charge of preparing for and reacting against any disaster such as application failure, campus disaster, or data set disaster. Their work also includes updating the strategy and also testing it. Another essential factor to consider is managerial support. The development of a robust risk management strategy by an organization may be successful, but its execution may be unsuccessful. When it comes to putting the strategy into action, effective organizational management is essential to ensure all the needs for disaster recovery Management are met. The absence of managerial support can destroy the entire process because their role is to pass budgetary and other approvals and then evolve into advisory roles allows the owners to get the rest of the company on board with the plan (August 22, 2005,
Edit intent: coherence
Original:   Archaeological sources The discovery of the ancient Pyu civilization in the twentieth century helped to explain some questions about Burmese myths. The excavation of the areas provided archaeological evidence for some of the mythological details about Burmese ancient city states, which had long been considered fictional. For example, Vishnu city and Sri Kshetra were mentioned in Burmese legends, and now the existence of these ancient lost cities has been confirmed. The sites of Hanlin and Taguang have also been excavated .
Revised:  References .
Edit intent: coherence
Original: For a uniformly stratified fluid, the power of the buoyancy frequency is equal to:Therefore, the classical result for the nonpenetrative deepening of the upper mixed layer is: The chimney evolution equation 261x261px |A schematic view of a convective chimney in the stratified fluid As time progresses and the baroclinic instability effects are becoming important, the time evolution of the chimney cannot be described only by the buoyancy forcing.
Revised: For a uniformly stratified fluid, the power of the buoyancy frequency is equal to:Therefore, the classical result for the nonpenetrative deepening of the upper mixed layer is: The chimney evolution equation 304x304px |A schematic view of a convective chimney in the stratified fluid As time progresses and the baroclinic instability effects are becoming important, the time evolution of the chimney cannot be described only by the buoyancy forcing.
Edit intent: fluency
Original:  The length scale of baroclinic eddies, assumed to be set by the Rossby radius of deformation, scale as: 413x413px |The stages and properties of the convection process
Revised:  The length scale of baroclinic eddies, assumed to be set by the Rossby radius of deformation, scale as: 566x566px |The stages and properties of the convection process
Edit intent: meaning-changed
Original: Many of the male minority convicted were co-accused with their wife. Helen, wife of Peter Bradwall  scolded Hugh Welesson and Isabel, his wife , in Middlewichin 1434 , calling Isabel a "child murderer" and Hugh a "skallet [wretched] knave".
Revised: Many of the male minority convicted were co-accused with their wives. In 1434, Helen Bradwall ( wife of Peter Bradwall scolded Hugh Welesson and Isabel, his wife , in Middlewichin 1434 , calling Isabel a "child murderer" and Hugh a "skallet [wretched] knave".
Edit intent: fluency
Original:  Helen, wife of Peter Bradwall  scolded Hugh Welesson and Isabel, his wife , in Middlewichin 1434 , calling Isabel a "child murderer" and Hugh a "skallet [wretched] knave".
Revised:  Helen, wife of Peter Bradwall ), scolded Hugh Welesson and Isabel, his wife , in Middlewichin 1434 , calling Isabel a "child murderer" and Hugh a "skallet [wretched] knave".
Edit intent: fluency
Original:  Helen, wife of Peter Bradwall  scolded Hugh Welesson and Isabel, his wife , in Middlewichin 1434 , calling Isabel a "child murderer" and Hugh a "skallet [wretched] knave".
Revised:  Helen, wife of Peter Bradwall scolded Hugh Welesson and his wife Isabel in Middlewich , calling Isabel a "child murderer" and Hugh a "skallet [wretched] knave".
Edit intent: clarity
Original: Cham dance during Dosmoche festival in Leh Palace The Culture of Ladakh refers to the traditional customs, belief systems, political systems that are followed by Ladakhi people . Ladakh's languages, religions, dance, music, architecture, food, and customs  are similar to neighboring Tibet.
Revised: Cham dance during Dosmoche festival in Leh Palace The culture of Ladakh refers to the traditional customs, belief systems, political systems that are followed by Ladakhi people . Ladakh's languages, religions, dance, music, architecture, food, and customs are similar to neighboring Tibet.
Edit intent: fluency
Original: Cham dance during Dosmoche festival in Leh Palace The Culture of Ladakh refers to the traditional customs, belief systems, political systems that are followed by Ladakhi people . Ladakh's languages, religions, dance, music, architecture, food, and customs  are similar to neighboring Tibet.
Revised: Cham dance during Dosmoche festival in Leh Palace The Culture of Ladakh refers to the traditional customs, belief systems, political systems that are followed by Ladakhi people in India. The languages, religions, dance, music, architecture, food, and customs are similar to neighboring Tibet.
Edit intent: meaning-changed
Original: Cham dance during Dosmoche festival in Leh Palace The Culture of Ladakh refers to the traditional customs, belief systems, political systems that are followed by Ladakhi people . Ladakh's languages, religions, dance, music, architecture, food, and customs  are similar to neighboring Tibet.
Revised: Cham dance during Dosmoche festival in Leh Palace The Culture of Ladakh refers to the traditional customs, belief systems, political systems that are followed by Ladakhi people . Ladakh's languages, religions, dance, music, architecture, food, and customs of the Ladakh region are similar to neighboring Tibet.
Edit intent: meaning-changed
Original:  The popular dances in Ladakh include the Khatok Chenmo, Chaams , etc. . People of Ladakh also celebrate several festivals throughout the year, some of the most famous ones being Hemis Tsechu  Losar.
Revised:  The popular dances in Ladakh include the khatok chenmo, cham , etc. . People of Ladakh also celebrate several festivals throughout the year, some of the most famous ones being Hemis Tsechu Losar.
Edit intent: fluency
Original:  The popular dances in Ladakh include the Khatok Chenmo, Chaams , etc. . People of Ladakh also celebrate several festivals throughout the year, some of the most famous ones being Hemis Tsechu  Losar.
Revised:  The popular dances in Ladakh include the Khatok Chenmo, Chaams , etc. People of Ladakh also celebrate several festivals throughout the year, some of the most famous ones being Hemis Tsechu Losar.
Edit intent: fluency
Original:  The popular dances in Ladakh include the Khatok Chenmo, Chaams , etc. . People of Ladakh also celebrate several festivals throughout the year, some of the most famous ones being Hemis Tsechu  Losar.
Revised:  The popular dances in Ladakh include the Khatok Chenmo, Chaams , etc. . People of Ladakh also celebrate several festivals throughout the year, some of the most famous ones being Hemis Tsechu and Losar.
Edit intent: fluency
Original:  Ashton noted that he grew up as a gay teen in the 1980s, in a daunting time when homophobia was widespread  , and that he was constantly told which toys to play with.
Revised:  Ashton noted that he grew up as a gay teen in the 1980s, in a daunting time when homophobia was widespread at the height of the HIV/AIDS crisis , and that he was constantly told which toys to play with.
Edit intent: meaning-changed
Original:  Background In 1999, Zoravka Matišić, a Croatian Indologist studying Sanskrit in India, chanced upon historical records that Croatians once lived in Gandaulim, a village set amidst sylvan surroundings just about 3 km from Old Goa.
Revised:  Background In 1999, Zoravka Matišić, a Croatian Indologist studying Sanskrit in India, claimed.that she had found historical records that Croatians once lived in Gandaulim, a village set amidst sylvan surroundings just about 3 km from Old Goa.
Edit intent: clarity
Original:  At the Rua de Ourém archives, she came upon an artistic sketch of the entrance of the Gaudelupchar fort and from the Bishop's Palace she came to know the location of the site of her search.
Revised:  At the Rua de Ourém archives, she came upon an artistic sketch of the entrance of the Gaudelupchar fort and from the Bishop's Palace she decided that was the location of the site of her search.
Edit intent: clarity
Original:  Moments of ecstasy awaited her at Gandaulim when she saw that the church of São Braz, a small chapel built in June 1541 and elevated to a parish church in 1563 by Archbishop D Frei Alexio de Menezes (1595-1607).
Revised:  She visited Gandaulim and saw that the church of São Braz, a small chapel built in June 1541 and elevated to a parish church in 1563 by Archbishop D Frei Alexio de Menezes (1595-1607).
Edit intent: clarity
Original: %DIFDELCMD < %DIFDELCMD < %%% However, most Dubrovniker merchants arrived in Portuguese Goa sometime between 1530 - 1535 AD. They founded their colony of São Braz - named after their patron St. Blaise, on the Konkan Coast in Goa, India. At its peak, the colony had around 12 000 residents.
Revised: %DIFDELCMD < %DIFDELCMD < %%% 
Edit intent: coherence
Original: %DIFDELCMD < %DIFDELCMD < %%% Decline Sao Braz was a thriving colony until the 1570s when trade between the Croatians and Indians declined. As the trade slowed down settlers started to move on from the area. The plague that destroyed Old Goa also had the people of Gandaulim fleeing for their life across the river to the islands of StEstevam and Cumbarjua. The Portuguese had also lost their monopoly over the spice trade to the British and Dutch and Goa was no longer the dominant trading port. The last straw was the great earthquake of 1667 which destroyed Dubrovnik and its prosperity. After the earthquake it no longer had the financial or military power to trade with India or establish any presence here.
Revised: %DIFDELCMD < %DIFDELCMD < %%% 
Edit intent: meaning-changed
Original:  When it was built around 1563 CE, The Church of Sao Braz was  the replica of the original Church of St. Blaise in Dubrovnik, which was destroyed in the earthquake of 1667 CE.
Revised:  When it was built around 1563 , the Church of Sao Braz was the replica of the original Church of St. Blaise in Dubrovnik, which was destroyed in the earthquake of 1667 CE.
Edit intent: fluency
Original:  When it was built around 1563 CE, The Church of Sao Braz was  the replica of the original Church of St. Blaise in Dubrovnik, which was destroyed in the earthquake of 1667 CE.
Revised:  When it was built around 1563 CE, The Church of Sao Braz was allegedly the replica of the original Church of St. Blaise in Dubrovnik, which was destroyed in the earthquake of 1667 CE.
Edit intent: clarity