wanyu/IteraTeR_v2 huggingface dataset:
Original:  The most widely accepted model is called ‘Stage Theory’ Atkinson–Shiffrin memory model based on the work by Atkinson and Shriffin shown in figure 1.
Revised:  The most widely accepted model is called ‘Stage Theory’ based on the work by Atkinson and Shriffin shown in figure 1.
Edit intent: clarity
Original:  Technologies are compensatory systems that can be used to support cognitive decline and impairment Impairment and thereby improve performance.
Revised:  Technologies are compensatory systems that can be used to support cognitive decline and impairment and thereby improve performance.
Edit intent: fluency
Original:  Listed below are some of the information technologies that have been developed: There are many, more recent theories concerning information processing that differ from the stage theory model, and today, research and study continues to modify existing beliefs in this area of cognitive psychology Cognitive psychology .
Revised:  Listed below are some of the information technologies that have been developed: There are many, more recent theories concerning information processing that differ from the stage theory model, and today, research and study continues to modify existing beliefs in this area of cognitive psychology .
Edit intent: fluency
Original:  Levels of processing Levels-of-processing effect : One of the first alternatives to the stage theory was developed by Craik and Lockhart (1972) and labeled the levels of processing model.
Revised:  Levels of processing : One of the first alternatives to the stage theory was developed by Craik and Lockhart (1972) and labeled the levels of processing model.
Edit intent: clarity
Original:  Dual Coding Theory Dual-coding theory : Another theory in the information processing debate is Paivio’s work in dual coding.
Revised:  Dual Coding Theory : Another theory in the information processing debate is Paivio’s work in dual coding.
Edit intent: fluency
Original:  Schema theory Schema (psychology) , parallel distributed processing, and connectionist models Connectionism : Rumelhart (1980), working in conjunction with others, developed the schema theory of information processing and memory.
Revised:  Schema theory , parallel distributed processing, and connectionist models Connectionism : Rumelhart (1980), working in conjunction with others, developed the schema theory of information processing and memory.
Edit intent: coherence
Original:  Schema theory Schema (psychology) , parallel distributed processing, and connectionist models Connectionism : Rumelhart (1980), working in conjunction with others, developed the schema theory of information processing and memory.
Revised:  Schema theory Schema (psychology) , parallel distributed processing, and connectionist models : Rumelhart (1980), working in conjunction with others, developed the schema theory of information processing and memory.
Edit intent: coherence
Original: There are many, more recent theories concerning information processing that differ from the stage theory model, and today, research and study continues to modify existing beliefs in this area of cognitive psychology.
Revised: There are many, more recent theories concerning information processing that differ from the stage theory model, and today, research and study continue to modify existing beliefs in this area of cognitive psychology.
Edit intent: fluency
Original:  Specifically, the levels of processing theory holds that memory is not three-staged which separates it immediately from the stage theory model.
Revised:  Specifically, the levels of processing theory hold that memory is not three-staged which separates it immediately from the stage theory model.
Edit intent: fluency
Original:  The deep temperature layer along with strong stratification in the salinity gives the conditions for BLT formation  Mignot, J., C.d.B.
Revised:  The deep temperature layer along with strong stratification in the salinity gives the conditions for BLT formation . Mignot, J., C.d.B.
Edit intent: fluency
Original:  Montegut, A. Lazar, and S. Cravatte, Control of salinity on the mixed layer depth in the world ocean: 2. Tropical areas, Journal of Geophysical Research-Oceans, 112 (C10), 2007. . For the western Pacific, the mechanism for BLT formation is different.
Revised:  Montegut, A. Lazar, and S. Cravatte, Control of salinity on the mixed layer depth in the world ocean: 2. Tropical areas, Journal of Geophysical Research-Oceans, 112 (C10), 2007. For the western Pacific, the mechanism for BLT formation is different.
Edit intent: fluency
Original:   Bosc, C., T. Delcroix, and C. Maes, Barrier layer variability in the western Pacific warm pool from 2000 to 2007, Journal of Geophysical Research-Oceans, 114, 2009. . Importance of BLT Prior to El Nino, the warm pool stores heat and is confined to the far western Pacific.
Revised:  . Bosc, C., T. Delcroix, and C. Maes, Barrier layer variability in the western Pacific warm pool from 2000 to 2007, Journal of Geophysical Research-Oceans, 114, 2009. . Importance of BLT Prior to El Nino, the warm pool stores heat and is confined to the far western Pacific.
Edit intent: fluency
Original:   Bosc, C., T. Delcroix, and C. Maes, Barrier layer variability in the western Pacific warm pool from 2000 to 2007, Journal of Geophysical Research-Oceans, 114, 2009. . Importance of BLT Prior to El Nino, the warm pool stores heat and is confined to the far western Pacific.
Revised:  Bosc, C., T. Delcroix, and C. Maes, Barrier layer variability in the western Pacific warm pool from 2000 to 2007, Journal of Geophysical Research-Oceans, 114, 2009. Importance of BLT Prior to El Nino, the warm pool stores heat and is confined to the far western Pacific.
Edit intent: fluency
Original:  Using coupled, atmospheric/ocean models and tuning the mixing to eliminate BLT for one year prior to El Nino, it was shown that the heat buildup associated with BLT is a requirement for big El Nino Maes , C., J. Picaut, and S. Belamari, Importance of the salinity barrier layer for the buildup of El Niño, Journal of Climate, 18 (1), 104-118, 2005..
Revised:  Using coupled, atmospheric/ocean models and tuning the mixing to eliminate BLT for one year prior to El Nino, it was shown that the heat buildup associated with BLT is a requirement for big El NinoMaes , C., J. Picaut, and S. Belamari, Importance of the salinity barrier layer for the buildup of El Niño, Journal of Climate, 18 (1), 104-118, 2005..
Edit intent: fluency
Original:  In addition, the BLT is the key factor in establishing the mean state that is perturbed during El Nino/La Nina Maes, C., and S. Belamari, On the Impact of Salinity Barrier Layer on the Pacific Ocean Mean State and ENSO, Sola, 7, 97-100, 2011. Referenc
Revised:  In addition, the BLT is the key factor in establishing the mean state that is perturbed during El Nino/La Nina Maes, C., and S. Belamari, On the Impact of Salinity Barrier Layer on the Pacific Ocean Mean State and ENSO, Sola, 7, 97-100, 2011. Reference
Edit intent: fluency
Original: Barrier Layer Thickness Barrier Layer Thickness Definition%DIFDELCMD < %DIFDELCMD < %%% The Barrier Layer Thickness (BLT) is a layer of water separating the well-mixed surface layer from the thermocline Sprintall, J., and M. Tomczak, Evidence of the barrier layer in the surface-layer of the tropics, Journal of Geophysical Research-Oceans, 97 (C5), 7305-7316, 1992..
Revised:  Barrier Layer Thickness Definition%DIFDELCMD < %DIFDELCMD < %%% The Barrier Layer Thickness (BLT) is a layer of water separating the well-mixed surface layer from the thermocline Sprintall, J., and M. Tomczak, Evidence of the barrier layer in the surface-layer of the tropics, Journal of Geophysical Research-Oceans, 97 (C5), 7305-7316, 1992..
Edit intent: fluency
Original: Barrier Layer Thickness Barrier Layer Thickness Definition%DIFDELCMD < %DIFDELCMD < %%% The Barrier Layer Thickness (BLT) is a layer of water separating the well-mixed surface layer from the thermocline Sprintall, J., and M. Tomczak, Evidence of the barrier layer in the surface-layer of the tropics, Journal of Geophysical Research-Oceans, 97 (C5), 7305-7316, 1992..
Revised: Barrier Layer Thickness %DIFDELCMD < %DIFDELCMD < %%% The Barrier Layer Thickness (BLT) is a layer of water separating the well-mixed surface layer from the thermocline Sprintall, J., and M. Tomczak, Evidence of the barrier layer in the surface-layer of the tropics, Journal of Geophysical Research-Oceans, 97 (C5), 7305-7316, 1992..
Edit intent: fluency
Original:  A more precise definition would be the difference between mixed layer depth (MLD) calculated from temperature minus the mixed layer depth calculated using density.
Revised:  The thickness of the layer is defined as the difference between mixed layer depth (MLD) calculated from temperature minus the mixed layer depth calculated using density.
Edit intent: clarity
Original:  Importance of BLT
Revised:  Significance of BLT
Edit intent: fluency
Original:  Prior to the abundant subsurface salinity available from Argo, this was the main methodology for calculating the oceanic MLD.
Revised:  Prior to the subsurface salinity available from Argo, this was the main methodology for calculating the oceanic MLD.
Edit intent: clarity
Original:  More recently, a density criterion has been used to define the MLD . The density-derived MLD is defined as the depth where the density increases from the surface value due to a prescribed temperature decrease of 0.2oC from the surface value while maintaining constant surface salinity value.
Revised:  More recently, a density criterion has been used to define the MLD , defined as the depth where the density increases from the surface value due to a prescribed temperature decrease of 0.2oC from the surface value while maintaining constant surface salinity value.
Edit intent: clarity
Original:  Using data from the ship of opportunity and Tropical Atmosphere – Ocean (TAO) moorings in the western Pacific, the east and west migration of the warm pool was tracked over 1992-2000 using sea surface salinity (SSS), sea surface temperature (SST), currents, and subsurface data from Conductivity, temperature , depth taken on various research cruises <ref> Delcroix, T., and M.
Revised:  Using data from ship of opportunity and Tropical Atmosphere – Ocean (TAO) moorings in the western Pacific, the east and west migration of the warm pool was tracked over 1992-2000 using sea surface salinity (SSS), sea surface temperature (SST), currents, and subsurface data from Conductivity, temperature , depth taken on various research cruises <ref> Delcroix, T., and M.
Edit intent: fluency
Original:  Using data from the ship of opportunity and Tropical Atmosphere – Ocean (TAO) moorings in the western Pacific, the east and west migration of the warm pool was tracked over 1992-2000 using sea surface salinity (SSS), sea surface temperature (SST), currents, and subsurface data from Conductivity, temperature , depth taken on various research cruises <ref> Delcroix, T., and M.
Revised:  Using data from the ship of opportunity and Tropical Atmosphere – Ocean (TAO) moorings in the western Pacific, the east and west migration of the warm pool was tracked over 1992-2000 using sea surface salinity (SSS), sea surface temperature (SST), currents, and subsurface data on conductivity as a function of temperature and depth taken on various research cruises <ref> Delcroix, T., and M.
Edit intent: clarity
Original:  Using data from the ship of opportunity and Tropical Atmosphere – Ocean (TAO) moorings in the western Pacific, the east and west migration of the warm pool was tracked over 1992-2000 using sea surface salinity (SSS), sea surface temperature (SST), currents, and subsurface data from Conductivity, temperature , depth taken on various research cruises <ref> Delcroix, T., and M.
Revised:  Using data from the ship of opportunity and Tropical Atmosphere – Ocean (TAO) moorings in the western Pacific, the east and west migration of the warm pool was tracked over 1992-2000 using sea surface salinity (SSS), sea surface temperature (SST), currents, and subsurface data from Conductivity, temperature , depth taken on various research cruises Delcroix, T., and M.
Edit intent: coherence
Original:  <\ref> . This work showed that during westward flow, the BLT in the western Pacific along the equator (138oE-145oE, 2oN-2oS) was between 18 m – 35 m corresponding with warm SST and serving as an efficient storage mechanism for heat.
Revised:  . This work showed that during westward flow, the BLT in the western Pacific along the equator (138oE-145oE, 2oN-2oS) was between 18 m – 35 m corresponding with warm SST and serving as an efficient storage mechanism for heat.
Edit intent: coherence
Original: == Barrier layer thickness (BLT) The thickness of the  layer is defined as the difference between mixed layer depth (MLD) calculated from temperature minus the mixed layer depth calculated using density.
Revised:  Barrier layer thickness (BLT) The thickness of the layer is defined as the difference between mixed layer depth (MLD) calculated from temperature minus the mixed layer depth calculated using density.
Edit intent: coherence
Original: == Barrier layer thickness (BLT) The thickness of the  layer is defined as the difference between mixed layer depth (MLD) calculated from temperature minus the mixed layer depth calculated using density.
Revised: == Barrier layer thickness (BLT) The thickness of the barrier layer is defined as the difference between mixed layer depth (MLD) calculated from temperature minus the mixed layer depth calculated using density.
Edit intent: fluency
Original:  The clo value is also similar in magnitude to the R value: 1 clo = 0.155 K·m²·W⁻¹ ≈ 0.88 R (where R means ft2·°F·hr/Btu) This is the amount of insulation that allows a person at rest to maintain thermal equilibrium in an environment at 21°C (70°F) in a normally ventilated room (0.1 m/s air movement).
Revised:  1 clo = 0.155 K·m²·W⁻¹ ≈ 0.88 R (where R means ft2·°F·hr/Btu) This is the amount of insulation that allows a person at rest to maintain thermal equilibrium in an environment at 21°C (70°F) in a normally ventilated room (0.1 m/s air movement).
Edit intent: clarity
Original:  Table 1 - Typical Insulation for Clothing Ensembles Ensemble Description Icl (clo)
Revised: + Table 1 - Typical Insulation for Clothing Ensembles Ensemble Description Icl (clo)
Edit intent: fluency
Original:  Table 1 - Typical Insulation for Clothing Ensembles Ensemble Description Icl (clo)
Revised:  Table 1 Ensemble Description Icl (clo)
Edit intent: clarity
Original:  Table 1 - Typical Insulation for Clothing Ensembles Ensemble Description Icl (clo)
Revised:  Table 1 - Typical Insulation for Clothing Ensembles – Typical insulation for clothing ensembles Ensemble description Icl (clo)
Edit intent: fluency
Original:  sandals 0.54 Knee-length skirt, long-sleeved shirt, full slip, panty hose 0.67 Knee-length skirt, long-sleeved shirt, half slip, panty hose, long-sleeved sweater 1.10 Knee-length skirt, long-sleeved shirt, half slip, panty hose, suit jacket 1.04 Ankle-length skirt, long-sleeved shirt, suit jacket, panty hose 1.10 Long-sleeved coveralls, T-shirt 0.72 Overalls, long-sleeved shirt, T-shirt 0.89 Insulated coveralls, long-sleeved thermal underwear, long underwear bottoms 1.37  Table 2 -
Revised:  sandals 0.54 Knee-length skirt, long-sleeved shirt, full slip, panty hose 0.67 Knee-length skirt, long-sleeved shirt, half slip, panty hose, long-sleeved sweater 1.10 Knee-length skirt, long-sleeved shirt, half slip, panty hose, suit jacket 1.04 Ankle-length skirt, long-sleeved shirt, suit jacket, panty hose 1.10 Long-sleeved coveralls, T-shirt 0.72 Overalls, long-sleeved shirt, T-shirt 0.89 Insulated coveralls, long-sleeved thermal underwear, long underwear bottoms 1.37 + Table 2 -
Edit intent: clarity
Original:  Garment Insulation Garment Description Icl (clo)
Revised:  Garment Insulation – Garment insulation Garment description Icl (clo)
Edit intent: coherence
Original:  Garment Description Icl (clo)
Revised:  Garment description Icl (clo)
Edit intent: fluency
Original:  Underwear Dress and Skirts Bra 0.01 Skirt (thin)
Revised:  Underwear Dresses and skirts Bra 0.01 Skirt (thin)
Edit intent: fluency
Original:  0.17 Shirts and Blouses Single-breasted (thin)
Revised:  0.17 Shirts and blouses Single-breasted (thin)
Edit intent: fluency
Original:  0.18 Trousers and Coveralls Sleeveless long gown (thin) 0.20 Short shorts 0.06 Short-sleeve hospital gown 0.31 Walking shorts 0.08 Short-sleeve short robe (thin) 0.34 Straight trousers (thin) 0.15 Short-sleeve pajamas (thin) 0.42 Straight trousers (thick) 0.24 Long-sleeve long gown (thick) 0.46 Sweatpants 0.28 Long-sleeve short wrap robe (thick) 0.48 Overalls 0.30 Long-sleeve pajamas (thick) 0.57 Coveralls 0.49 Long-sleeve long wrap robe (thick) 0.69
Revised:  0.18 Trousers and coveralls Sleeveless long gown (thin) 0.20 Short shorts 0.06 Short-sleeve hospital gown 0.31 Walking shorts 0.08 Short-sleeve short robe (thin) 0.34 Straight trousers (thin) 0.15 Short-sleeve pajamas (thin) 0.42 Straight trousers (thick) 0.24 Long-sleeve long gown (thick) 0.46 Sweatpants 0.28 Long-sleeve short wrap robe (thick) 0.48 Overalls 0.30 Long-sleeve pajamas (thick) 0.57 Coveralls 0.49 Long-sleeve long wrap robe (thick) 0.69
Edit intent: fluency
Original: stopping the wind from penetrating and replacing the layer of warm air close to the body;
Edit intent: coherence
Original:  Mechanisms of insulation There are three kinds of heat transfer: conduction (exchange of heat through contact), convection (movement of fluids), and radiation.
Revised: Thermophysiological comfort Thermophysiological comfort is the capacity of the clothing material that makes the balance of moisture and heat between the body and the environment. It is a property of textile materials that creates ease by maintaining moisture and thermal levels in a human's resting and active states. The selection of textile material significantly affects the comfort of the wearer. Different textile fiber holds individual properties that suit in different environments. Natural fibers breathable and absorbs moisture, and synthetic fibers are hydrophobic; they repel moisture and do not allow air to pass. Different environments demand a diverse selection of clothing materials. Hence the appropriate choice is important.The major determinants that influence Thermophysiological comfort are the permeable construction, heat, and moisture transfer rate. Mechanisms of insulation There are three kinds of heat transfer: conduction (exchange of heat through contact), convection (movement of fluids), and radiation.
Edit intent: coherence
Original:  It is a direct antecedent of the Emirate of Nejd and Hasa.
Revised:  It was the direct antecedent of the Emirate of Nejd and Hasa.
Edit intent: fluency
Original:  Pp. 40. was the first iteration of the third Saudi state from 1902 to 1913.J. A. Hammerton.
Revised:  Pp. 40. was the first iteration of the Third Saudi State from 1902 to 1913.J. A. Hammerton.
Edit intent: fluency
Original: The Emirate of Nejd and Hasa  from 1913 to 1921.
Revised: The Emirate of Nejd and Hasa existed from 1913 to 1921.
Edit intent: clarity
Original: The Emirate of Nejd and Hasa  existed from 1913 to 1921.
Revised: The Emirate of Nejd and Hasa was a state that existed from 1913 to 1921.
Edit intent: clarity
Original:  It is a direct antecedent of the Sultanate of Nejd.
Revised:  It was the direct antecedent of the Sultanate of Nejd.
Edit intent: fluency
Original: The Emirate of Nejd and Hasa was  second iteration of the Third Saudi State from 1913 to 1921.
Revised: The Emirate of Nejd and Hasa was the second iteration of the Third Saudi State from 1913 to 1921.
Edit intent: fluency
Original:   Former Arab states Category:Ottoman Arabia Nejd Category:History of Nejd Category:History of Saudi Arabia Category:Najd Category: 1920s in Saudi Arabia Category: 1930s in Saudi Arabia Category: States and territories established in 1902 Category:States and territories disestablished in 1921 Category:1902 establishments in Asia Category:1921 disestablishments in As
Revised:  1902 establishments in Asia Category:1921 disestablishments in Asia Category: Former Arab states Category:Ottoman Arabia Nejd Category:History of Nejd Category:History of Saudi Arabia Category:Najd Category: 1920s in Saudi Arabia Category: 1930s in Saudi Arabia Category: States and territories established in 1902 Category:States and territories disestablished in 1921 Category:1902 establishments in Asia Category:1921 disestablishments in As
Edit intent: fluency
Original:   Former Arab states Category:Ottoman Arabia Nejd Category:History of Nejd Category:History of Saudi Arabia Category:Najd Category: 1920s in Saudi Arabia Category: 1930s in Saudi Arabia Category: States and territories established in 1902 Category:States and territories disestablished in 1921 Category:1902 establishments in Asia Category:1921 disestablishments in As
Revised:  Former Arab states Nejd Category:History of Nejd Category:History of Saudi Arabia Category:Najd Category: 1920s in Saudi Arabia Category: 1930s in Saudi Arabia Category: States and territories established in 1902 Category:States and territories disestablished in 1921 Category:1902 establishments in Asia Category:1921 disestablishments in As
Edit intent: clarity
Original:   Former Arab states Category:Ottoman Arabia Nejd Category:History of Nejd Category:History of Saudi Arabia Category:Najd Category: 1920s in Saudi Arabia Category: 1930s in Saudi Arabia Category: States and territories established in 1902 Category:States and territories disestablished in 1921 Category:1902 establishments in Asia Category:1921 disestablishments in As
Revised:  Former Arab states Category:Ottoman Arabia Nejd Category:History of Nejd Category:History of Saudi Arabia Category:Najd Category: Ottoman Arabia Category: 1930s in Saudi Arabia Category: States and territories established in 1902 Category:States and territories disestablished in 1921 Category:1902 establishments in Asia Category:1921 disestablishments in As
Edit intent: fluency
Original:   Former Arab states Category:Ottoman Arabia Nejd Category:History of Nejd Category:History of Saudi Arabia Category:Najd Category: 1920s in Saudi Arabia Category: 1930s in Saudi Arabia Category: States and territories established in 1902 Category:States and territories disestablished in 1921 Category:1902 establishments in Asia Category:1921 disestablishments in As
Revised:  Former Arab states Category:Ottoman Arabia Nejd Category:History of Nejd Category:History of Saudi Arabia Category:Najd Category: 1920s in Saudi Arabia Category: States and territories established in 1902 Category:States and territories disestablished in 1921 Category:1902 establishments in Asia Category:1921 disestablishments in As
Edit intent: clarity
Original:   Former Arab states Category:Ottoman Arabia Nejd Category:History of Nejd Category:History of Saudi Arabia Category:Najd Category: 1920s in Saudi Arabia Category: 1930s in Saudi Arabia Category: States and territories established in 1902 Category:States and territories disestablished in 1921 Category:1902 establishments in Asia Category:1921 disestablishments in As
Revised:  Former Arab states Category:Ottoman Arabia Nejd Category:History of Nejd Category:History of Saudi Arabia Category:Najd Category: 1920s in Saudi Arabia Category: 1930s in Saudi Arabia Category: States and territories established in 1902 Category:States and territories disestablished in 19
Edit intent: coherence
Original:  Furthermore, by combining the usefulness  of event-related potentials with eye movement monitoring, researchers are able to correlate fixations during readings with word recognition in the brain in real-time.
Revised:  Furthermore, by combining the usefulness the of event-related potentials with eye movement monitoring, researchers are able to correlate fixations during readings with word recognition in the brain in real-time.
Edit intent: fluency