wanyu/IteraTeR_v2 huggingface dataset:
Original:  Sea surface height /sea level rise (RADAR altimetry) RADAR altimiters send microwave pulses to the surface to catch the reflection intensity over a short time period and thereby measure the two-way travel time of the signal.
Revised:  Sea surface height /sea level rise (RADAR altimetry) RADAR altimeters send microwave pulses to the surface to catch the reflection intensity over a short time period and thereby measure the two-way travel time of the signal.
Edit intent: clarity
Original:  Sea surface height /sea level rise (RADAR altimetry) RADAR altimiters send microwave pulses to the surface to catch the reflection intensity over a short time period and thereby measure the two-way travel time of the signal.
Revised:  Sea surface height /sea level rise (RADAR altimetry) RADAR altimiters send microwave pulses to the surface and catch the reflection intensity over a short time period and thereby measure the two-way travel time of the signal.
Edit intent: fluency
Original:  Sea surface height /sea level rise (RADAR altimetry) RADAR altimiters send microwave pulses to the surface to catch the reflection intensity over a short time period and thereby measure the two-way travel time of the signal.
Revised:  Sea surface height /sea level rise (RADAR altimetry) RADAR altimiters send microwave pulses to the surface to catch the reflection intensity over a short time period measuring the two-way travel time of the signal.
Edit intent: coherence
Original:  To deduce the sea surface height the distance between the satellite and the surface has to be corrected for dynamical errors and calibrated to the satellites orbit and geoid height at the respective location .
Revised:  To deduce the sea surface height the distance between the satellite and the surface has to be corrected for dynamical errors , the atmospheric conditions and the local geoid height .
Edit intent: clarity
Original: is the height of the satellite above the ocean surface and is the quantity measured by the satellite with cm precision. is the local height difference between the geoid and the reference elipsoid which is in the order of ±100 cm and can be estimated using a time series of ocean altimetry data. is the local height difference due to tidal movements of which the magnitude scales dependent of the time of day. is the local height difference due to atmospheric pressure difference above the surface.
Revised: is the height of the satellite above the ocean surface and is the quantity measured by the satellite with cm precision. is the local height difference between the geoid and the reference ellipsoid which is in the order of ±100 cm and can be estimated using a time series of ocean altimetry data. is the local height difference due to tidal movements of which the magnitude scales dependent of the time of day. is the local height difference due to atmospheric pressure difference above the surface.
Edit intent: fluency
Original:  The altimetry derived dynamical sea surface height can be used in oceanographic research to compute the Sea Surface Height Anomaly (SSHA)  by subtracting the temporal mean of the sea surface height from the current sea surface height with the Mean Sea Surface (MSS) as and the SSHA as . Although the SSHA can show anomalies in surface currents of the ocean  often a measure called the Absolute Dynamic Topography (ADT) is computed using a independent measurement of the geoid height :
Revised:  The altimetry derived dynamical sea surface height can be used in oceanographic research to compute the Sea Surface Height Anomaly (SSHA) by subtracting the temporal mean of the SSH or Mean Sea Surface (MSS) as and the SSHA as . Although the SSHA can show anomalies in surface currents of the ocean often a measure called the Absolute Dynamic Topography (ADT) is computed using a independent measurement of the geoid height :
Edit intent: clarity
Original:  The altimetry derived dynamical sea surface height can be used in oceanographic research to compute the Sea Surface Height Anomaly (SSHA)  by subtracting the temporal mean of the sea surface height from the current sea surface height with the Mean Sea Surface (MSS) as and the SSHA as . Although the SSHA can show anomalies in surface currents of the ocean  often a measure called the Absolute Dynamic Topography (ADT) is computed using a independent measurement of the geoid height :
Revised:  The altimetry derived dynamical sea surface height can be used in oceanographic research to compute the Sea Surface Height Anomaly (SSHA) by subtracting the temporal mean of the sea surface height from the current sea surface height with the Mean Sea Surface (MSS) from the current SSH with so that: Although the SSHA can show anomalies in surface currents of the ocean often a measure called the Absolute Dynamic Topography (ADT) is computed using a independent measurement of the geoid height :
Edit intent: clarity
Original:  The altimetry derived dynamical sea surface height can be used in oceanographic research to compute the Sea Surface Height Anomaly (SSHA)  by subtracting the temporal mean of the sea surface height from the current sea surface height with the Mean Sea Surface (MSS) as and the SSHA as . Although the SSHA can show anomalies in surface currents of the ocean  often a measure called the Absolute Dynamic Topography (ADT) is computed using a independent measurement of the geoid height :
Revised:  The altimetry derived dynamical sea surface height can be used in oceanographic research to compute the Sea Surface Height Anomaly (SSHA) by subtracting the temporal mean of the sea surface height from the current sea surface height with the Mean Sea Surface (MSS) as and the SSHA as . Although the SSHA can show anomalies in surface currents of the ocean , often a measure called the Absolute Dynamic Topography (ADT) is computed using a independent measurement of the geoid height :
Edit intent: fluency
Original:  The altimetry derived dynamical sea surface height can be used in oceanographic research to compute the Sea Surface Height Anomaly (SSHA)  by subtracting the temporal mean of the sea surface height from the current sea surface height with the Mean Sea Surface (MSS) as and the SSHA as . Although the SSHA can show anomalies in surface currents of the ocean  often a measure called the Absolute Dynamic Topography (ADT) is computed using a independent measurement of the geoid height :
Revised:  The altimetry derived dynamical sea surface height can be used in oceanographic research to compute the Sea Surface Height Anomaly (SSHA) by subtracting the temporal mean of the sea surface height from the current sea surface height with the Mean Sea Surface (MSS) as and the SSHA as . Although the SSHA can show anomalies in surface currents of the ocean often a measure called the Absolute Dynamic Topography (ADT) is computed using a independent measurement of the geoid height 
Edit intent: fluency
Original:  With trend analysis over the entire ocean altimetry time period (since the   launch of TOPEX/ Poseidon in 1992 ) researchers have deducted a global mean sea level trend indicating a rise in global sea level.
Revised:  With trend analysis over the entire ocean altimetry time period (since the launch of TOPEX/ POSEIDON in 1992 ) researchers have deducted a global mean sea level trend indicating a rise in global sea level.
Edit intent: fluency
Original: Remote sensing  is a widely used observational technique in oceanography as it enables researchers to acquire data of a location without physically measuring at that location.
Revised: Remote sensing in oceanography is a widely used observational technique in oceanography as it enables researchers to acquire data of a location without physically measuring at that location.
Edit intent: fluency
Original: Remote sensing  is a widely used observational technique in oceanography as it enables researchers to acquire data of a location without physically measuring at that location.
Revised: Remote sensing is a widely used observational technique which enables researchers to acquire data of a location without physically measuring at that location.
Edit intent: clarity
Original: Remote sensing in oceanography is a widely used observational technique  which enables researchers to acquire data of a location without physically measuring at that location.
Revised: Remote sensing in oceanography is a widely used observational technique . which enables researchers to acquire data of a location without physically measuring at that location.
Edit intent: fluency
Original:  Algal blooms are used to study internal wave structures, up-welling and river outflows, which all bring nutrients to surface waters, since they are correlated with algae concentration . Pollution often coincides with high nutrient waters, making algal blooms good indicators for the severity and impact of water pollution .
Revised:  Algal blooms are used to study internal wave structures, up-welling and river outflows, which all bring nutrients to surface waters, since they are correlated with algae concentration . Pollution often coincides with high nutrient waters, making algal blooms good indicators for the severity and impact of water pollution 
Edit intent: fluency
Original: Remote sensing in oceanography is a widely used observational technique . which enables researchers to acquire data of a location without physically measuring at that location.
Revised: Remote sensing in oceanography is a widely used observational technique which enables researchers to acquire data of a location without physically measuring at that location.
Edit intent: fluency
Original: Dzianis Urad (, also know as Denis Urad;
Revised: Dzianis Urad (, also known as Denis Urad;
Edit intent: fluency
Original:  The Experiential dining trend is primarily driven by Millennial and Generation Z diners  
Revised:  The Experiential dining trend is primarily driven by Millennial and Generation Z diners . 
Edit intent: fluency
Original:  The Experiential dining trend is primarily driven by Millennial and Generation Z diners.
Revised:  The experiential dining trend is primarily driven by Millennial and Generation Z diners.
Edit intent: fluency
Original:  A unique experience provided by a restaurant or food truck may include dining in darkness, in  high places, or in outdoor settings.
Revised:  A unique experience provided by a restaurant or food truck may include dining in darkness, in a large space, in high places, or in outdoor settings.
Edit intent: clarity
Original: 2000 born Category:Beauty Pageant Participants Category:Beauty Pageant Winners Category:Beauty pageant contestants Category:Beauty pageant contestant stubs Category:Model stubs Category:Asian beauty pageant contestant stubs Category: Models (profession) Category:Indian models Category:Models from Bangalore Category:Female models from Bangalore Category:Female models from Karnataka Category:Indian female models Category:Beauty pageant contestants from India Category:Indian beauty pageant winne
Revised: 2000 births Category:Beauty Pageant Participants Category:Beauty Pageant Winners Category:Beauty pageant contestants Category:Beauty pageant contestant stubs Category:Model stubs Category:Asian beauty pageant contestant stubs Category: Models (profession) Category:Indian models Category:Models from Bangalore Category:Female models from Bangalore Category:Female models from Karnataka Category:Indian female models Category:Beauty pageant contestants from India Category:Indian beauty pageant winne
Edit intent: fluency
Original: 2000 born Category:Beauty Pageant Participants Category:Beauty Pageant Winners Category:Beauty pageant contestants Category:Beauty pageant contestant stubs Category:Model stubs Category:Asian beauty pageant contestant stubs Category: Models (profession) Category:Indian models Category:Models from Bangalore Category:Female models from Bangalore Category:Female models from Karnataka Category:Indian female models Category:Beauty pageant contestants from India Category:Indian beauty pageant winne
Revised: 2000 born Category:Beauty pageant contestants Category:Beauty pageant contestant stubs Category:Model stubs Category:Asian beauty pageant contestant stubs Category: Models (profession) Category:Indian models Category:Models from Bangalore Category:Female models from Bangalore Category:Female models from Karnataka Category:Indian female models Category:Beauty pageant contestants from India Category:Indian beauty pageant winne
Edit intent: clarity
Original: 2000 born Category:Beauty Pageant Participants Category:Beauty Pageant Winners Category:Beauty pageant contestants Category:Beauty pageant contestant stubs Category:Model stubs Category:Asian beauty pageant contestant stubs Category: Models (profession) Category:Indian models Category:Models from Bangalore Category:Female models from Bangalore Category:Female models from Karnataka Category:Indian female models Category:Beauty pageant contestants from India Category:Indian beauty pageant winne
Revised: 2000 born Category:Beauty Pageant Participants Category:Beauty Pageant Winners Category:Beauty pageant contestants Category:Beauty pageant contestant stubs Category:Model stubs Category:Asian beauty pageant contestant stubs Category: Indian models Category:Female models from Bangalore Category:Female models from Karnataka Category:Indian female models Category:Beauty pageant contestants from India Category:Indian beauty pageant winne
Edit intent: clarity
Original: Early life Josita joined St Mary ’ s School, and then continued her schooling at St.
Revised: Early life Josita joined St Mary ' s School, and then continued her schooling at St.
Edit intent: fluency
Original: Actresses in Tamil cinema Category:Living people Category:Actresses in Tulu cinema Category:Konkani people Category:2000 births Category:Beauty pageant contestants Category:Beauty pageant contestant stubs Category:Model stubs Category:Asian beauty pageant contestant stubs Category:Indian models Category:Female models from Bangalore Category:Female models from Karnataka Category:Indian female models Category:Beauty pageant contestants from India Category:Indian beauty pageant winne
Revised: Actresses in Tamil cinema Category:Living people Category:Actresses in Tulu cinema Category:Konkani people Category:2000 births Category:Beauty pageant contestants Category:Indian models Category:Female models from Bangalore Category:Female models from Karnataka Category:Indian female models Category:Beauty pageant contestants from India Category:Indian beauty pageant winne
Edit intent: clarity
Original:  She also played a cameo role in popular television show Yeh rishta kya kehlata hai on Star Plus.
Revised:  She also played a cameo role in popular television show Yeh Rishta Kya Kehlata Hai on Star Plus.
Edit intent: fluency
Original:  The turbulent and dynamic nature of the ocean makes it that the current loop sometimes closes onto itself and separates (" sheds ") from the current.
Revised:  The turbulent and dynamic nature of the ocean causes the current loop sometimes closes onto itself and separates (" sheds ") from the current.
Edit intent: clarity
Original:  The turbulent and dynamic nature of the ocean makes it that the current loop sometimes closes onto itself and separates (" sheds ") from the current.
Revised:  The turbulent and dynamic nature of the ocean makes it that the current loop to sometimes close onto itself and separates (" sheds ") from the current.
Edit intent: fluency
Original:  The turbulent and dynamic nature of the ocean makes it that the current loop sometimes closes onto itself and separates (" sheds ") from the current.
Revised:  The turbulent and dynamic nature of the ocean makes it that the current loop sometimes closes onto itself and separate (" sheds ") from the current.
Edit intent: fluency
Original:  The turbulent and dynamic nature of the ocean makes it that the current loop sometimes closes onto itself and separates (" sheds ") from the current.
Revised:  The turbulent and dynamic nature of the ocean makes it that the current loop sometimes closes onto itself and separates (" shed ") from the current.
Edit intent: fluency
Original:  When exactly a ring is shed, is often unclear and  process behind it is still an active topic of research.
Revised:  When exactly a ring is shed, is often unclear and the process behind it is still an active topic of research.
Edit intent: fluency
Original:  The topography of the ocean floor and incoming eddies from upstream regions could play a role in the sheddingof the rings .
Revised:  The topography of the ocean floor and incoming eddies from upstream regions could play a role in ring shedding .
Edit intent: clarity
Original:  Other research indicates that the procress of ring shedding is driven by barotropic instabilities.
Revised:  Other research indicates that ring shedding is driven by barotropic instabilities.
Edit intent: clarity
Original:  Characteristics and Observation The process of ring shedding was first described by Fuglisteri in 1972, who observed rings in the Gulf Stream.
Revised:  Characteristics and observation The process of ring shedding was first described by Fuglisteri in 1972, who observed rings in the Gulf Stream.
Edit intent: fluency
Original:  Typically, the rings have a diameter between 100 and 400 kilometers , a depth of up to 1500 meters and a temperature anomaly of a few degrees Celsius.
Revised:  Typically, the rings have a diameter of , a depth of up to 1500 meters and a temperature anomaly of a few degrees Celsius.
Edit intent: clarity
Original:  Typically, the rings have a diameter between 100 and 400 kilometers , a depth of up to 1500 meters and a temperature anomaly of a few degrees Celsius.
Revised:  Typically, the rings have a diameter between 100 and 400 kilometers , a depth of up to , and a temperature anomaly of a few degrees Celsius.
Edit intent: clarity
Original:  The rings drift slowly ( 0-5 kilometers per day) until they either decay or are reabsorbed by the current.
Revised:  The rings drift slowly ( per day) until they either decay or are reabsorbed by the current.
Edit intent: clarity
Original:  However, under the surface the colder water temperatures persist longer and deeper and can in that way be measured and observed using vertical ocean profiles of temperature and salinity.
Revised:  However, under the surface the colder water temperatures persist longer and deeper , allowing measurement and observation using vertical ocean profiles of temperature and salinity.
Edit intent: clarity
Original:  The observed current ring was a warm core, anticyclonic ring with a diameter of about 150 kilometer and detached from the Kuroshio in the Luzon Strait.
Revised:  The observed current ring was a warm core, anticyclonic ring with a diameter of about and detached from the Kuroshio in the Luzon Strait.
Edit intent: clarity
Original:  The ring had a current speed of about 1 m/s near the surface.
Revised:  The ring had a current speed of about near the surface.
Edit intent: clarity
Original:  The ring had positive temperature anomalies up until a depth of 1 kilometer . Gulf Stream In the Gulf Stream ring shedding takes place at two locations: in the Gulf of Mexico and along the eastern coast of the United States.
Revised:  The ring had positive temperature anomalies up until a depth of . Gulf Stream In the Gulf Stream ring shedding takes place at two locations: in the Gulf of Mexico and along the eastern coast of the United States.
Edit intent: clarity
Original:  At the point of retroflection, ring shedding takes place, resulting in both warm core anticyclonic and cold core cyclonic rings.
Revised:  At the point of retroflection, ring shedding results in both warm core anticyclonic and cold core cyclonic rings.
Edit intent: clarity
Original:  These rings can have diameters up to 400 kilometers and reach depths of 1500 meters .
Revised:  These rings can have diameters up to and reach depths of 1500 meters .
Edit intent: clarity
Original:  These rings can have diameters up to 400 kilometers and reach depths of 1500 meters .
Revised:  These rings can have diameters up to 400 kilometers and reach depths of .
Edit intent: clarity
Original:  Here only warm core, anticyclonic rings with a diameter of typically between 100 and 200 kilometers are formed.
Revised:  Here only warm core, anticyclonic rings with a diameter of typically are formed.
Edit intent: clarity
Original:  Agulhas current The Agulhas current flows alongside the coast of southeast Africa until it retroflects right at the tip of South-Africa.
Revised:  Agulhas current The Agulhas current flows alongside the coast of southeast Africa until it retroflects at the tip of South-Africa.
Edit intent: coherence
Original:  In this retroflection region , ring shedding takes place. . The formed rings are warm core and anticyclonic, with a frequency of 4-6 rings per year.
Revised:  In this retroflection region . The rings are warm core and anticyclonic, with a frequency of 4-6 rings per year.
Edit intent: clarity
Original:  The water from the Agulhas rings can be up to 5 degrees Celsius warmer than the water in the Southern Atlantic.
Revised:  The water from the Agulhas rings can be up to warmer than the water in the Southern Atlantic.
Edit intent: clarity
Original:  The rings from the Agulhas current transport about 5 Sverdrup to the Atlantic Ocean and play an important role in the thermohaline circulationin that way .
Revised:  The rings from the Agulhas current transport about 5 Sverdrup to the Atlantic Ocean , thereby playing an important role in the thermohaline circulationin that way .
Edit intent: clarity
Original:  The rings from the Agulhas current transport about 5 Sverdrup to the Atlantic Ocean and play an important role in the thermohaline circulationin that way .
Revised:  The rings from the Agulhas current transport about 5 Sverdrup to the Atlantic Ocean and play an important role in thermohaline circulation .
Edit intent: clarity
Original:  The exact reason for the shedding of rings in the Agulhas retroflection region is still unsure .
Revised:  The exact cause of ring shedding in the Agulhas retroflection region is still unsure .
Edit intent: clarity
Original:  The exact reason for the shedding of rings in the Agulhas retroflection region is still unsure .
Revised:  The exact reason for the shedding of rings in the Agulhas retroflection region is still unclear .
Edit intent: clarity
Original:  One possible explanation is that the shedding of the rings occurs because of incoming eddies from upstream regions , another possible explanation is that the ring shedding is caused by barotropic instabilities in the Agulhas retroflection region  Thermohalince circulation Ring shedding might play an important role in the thermohaline circulation, depending on the location.
Revised:  One possible cause is incoming eddies from upstream regions , another possible explanation is that the ring shedding is caused by barotropic instabilities in the Agulhas retroflection region Thermohalince circulation Ring shedding might play an important role in the thermohaline circulation, depending on the location.
Edit intent: clarity
Original:  One possible explanation is that the shedding of the rings occurs because of incoming eddies from upstream regions , another possible explanation is that the ring shedding is caused by barotropic instabilities in the Agulhas retroflection region  Thermohalince circulation Ring shedding might play an important role in the thermohaline circulation, depending on the location.
Revised:  One possible explanation is that the shedding of the rings occurs because of incoming eddies from upstream regions . A second proposed explanation is that the ring shedding is caused by barotropic instabilities in the Agulhas retroflection region Thermohalince circulation Ring shedding might play an important role in the thermohaline circulation, depending on the location.
Edit intent: clarity