cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.17632/r99xkp2czc.1
title: MARHYD: Magdalena River Hidrodynamic model in Delft3D. Results of Case 2 (salinity and water level)

description: This database contains output files of MARHYD: the MAgdalena River HYdrodynamic model in Delft3D. Model description: The model domain of MARHYD extends from coordinates 10.9619 °N to 11.2669° N and from 74.7571 °W to 74.8784 °W. This domain includes the last 22 km of the river and estuary before discharging into the Caribbean Sea and 63 km by 37 km of the surrounding coastal region in east-west and north-south directions. In oceanic waters, the model is rectangular, configured on a 150 m x 150 m horizontal resolution near the open boundaries, with a gradual refinement to 50 m x 50 m near the river mouth. In the river and estuary, the model is curvilinear, with 10 horizontal cells in the transversal section, reaching a variable size between 40 m to 100 m. 40 Z-layers represent the water column with a higher resolution close to the surface. Layers of approximately 0.5 m cover the upper 10 m of the water columns, where most of the mixing processes between the river and the ocean occur. The vertical resolution reduces progressively from 10 m depth to the bottom. The boundary conditions of salinity and currents with the Caribbean Sea (at the North, East, and West) were obtained from HYCOM + NODA reanalysis every 6 hours, and wind velocity was obtained from CFSR-NCEP/NCAR reanalysis every 1 hour for the wind stress. The bathymetry was derived from GEBCO, Nautical charts of the Maritime Directorate of Colombia (DIMAR), and high-resolution in-situ measurements. River discharge data were obtained from the nearest upstream hydrological station of the Magdalena River. The model was calibrated and validated using field data of salinity profiles along the river estuary and plume, velocity measurements in the river and estuary, and water level in the estuary for two climatic seasons. Description of simulation case: Case 2 corresponds to a mid-discharge scenario with Q = 6800 m^3/s, equivalent to the 50th percentile of the historical freshwater flow. Water currents, salinity and water level in the open boundaries correspond to the time-average of HYCOM Reanalysis database for the dates between 9th and 29th of November of 2017. Winds are constant with a speed of 11.3 m/s from the Northeast. The full set of input (configuration) files of this simulation can be found in the dataset: Barros, Yennis ; Saavedra, Victor; Álvarez-Silva, Óscar; Cardona, Yuley; Cáceres-Euse, Alejandro; Osorio, Andres F.; Arbeláez, Felipe (2021), “MARHYD: Magdalena River Hydrodynamic model in Delft3D. Database 1 of 5: Inputs”, Mendeley Data, V1, doi: 10.17632/hmhdvg47kg.1 Files description: This dataset includes the salinity and water level results for the entire computational domain every 8 hours during 20 days of simulation. ​ The data are in .nc format. Results of water velocity for this simulation case can be found in the database: MARHYD: Magdalena River Hydrodynamic model in Delft3D. Results of Case 1 (water velocity), doi: 10.17632/7nzrcrvzmk.1
DOI: 10.17632/rk8kzbdz45.1
title: GSB_pyrochlores

description: The data are processed microprobe analyses of pyrochlore-supergroup minerals from the Julianna pegmatitic system in the Góry Sowie Block refered to the manuscript 'Environmental constraints on geochemical evolution of pyrochlore-supergroup minerals in anatectic pegmatites of the Góry Sowie block, SW Poland: A case of the Julianna pegmatitic system at Piława Górna' by A. Pieczka. They include Table 2 (a and b), Table 3 (a and b), ...., Table 7 (a and b) presenting representative compositions (in wt% and in apfu) of the pyrochlores occurring in various bodies of the pegmatite system.
DOI: 10.17632/vxs52f7fcd.1
title: MARHYD: Magdalena River Hydrodynamic model in Delft3D. Results of Case 1 (water velocity)

description: This database contains output files of MARHYD: the MAgdalena River HYdrodynamic model in Delft3D. Model description: The model domain of MARHYD extends from coordinates 10.9619 °N to 11.2669° N and from 74.7571 °W to 74.8784 °W. This domain includes the last 22 km of the river and estuary before discharging into the Caribbean Sea and 63 km by 37 km of the surrounding coastal region in east-west and north-south directions. In oceanic waters, the model is rectangular, configured on a 150 m x 150 m horizontal resolution near the open boundaries, with a gradual refinement to 50 m x 50 m near the river mouth. In the river and estuary, the model is curvilinear, with 10 horizontal cells in the transversal section, reaching a variable size between 40 m to 100 m. 40 Z-layers represent the water column with a higher resolution close to the surface. Layers of approximately 0.5 m cover the upper 10 m of the water columns, where most of the mixing processes between the river and the ocean occur. The vertical resolution reduces progressively from 10 m depth to the bottom. The boundary conditions of salinity and currents with the Caribbean Sea (at the North, East, and West) were obtained from HYCOM + NODA reanalysis every 6 hours, and wind velocity was obtained from CFSR-NCEP/NCAR reanalysis every 1 hour for the wind stress. The bathymetry was derived from GEBCO, Nautical charts of the Maritime Directorate of Colombia (DIMAR), and high-resolution in-situ measurements. River discharge data were obtained from the nearest upstream hydrological station of the Magdalena River. The model was calibrated and validated using field data of salinity profiles along the river estuary and plume, velocity measurements in the river and estuary, and water level in the estuary for two climatic seasons. Description of simulation case: Case 1 corresponds to a low-discharge scenario with Q = 3400 m^3/s, equivalent to the 10th percentile of the historical freshwater flow. Water currents, salinity and water level in the open boundaries correspond to the time-average of HYCOM Reanalysis database for the days between 9 and 29 of November of 2017. Winds are constant with a speed of 10.5 m/s from the Northeast. The full set of input (configuration) files of this simulation can be found in the dataset: Barros, Yennis ; Saavedra, Victor; Álvarez-Silva, Óscar; Cardona, Yuley; Cáceres-Euse, Alejandro; Osorio, Andres F.; Arbeláez, Felipe (2021), “MARHYD: Magdalena River Hydrodynamic model in Delft3D. Database 1 of 5: Inputs”, Mendeley Data, V1, doi: 10.17632/hmhdvg47kg.1 Files description: This dataset includes the salinity and water level results for the whole computational domain every 8 hours during 20 days of simulation. ​ The data are in .nc format. Results of water velocity for this simulation can be found in the database: MARHYD: Magdalena River Hydrodynamic model in Delft3D. Results of Case 1 (salinity and water level), doi: 10.17632/zhtwsdzr6c.1
DOI: 10.17632/7nzrcrvzmk.1
title: MARHYD: Magdalena River Hydrodynamic model in Delft3D. Results of Case 2 (water velocity)

description: This database contains output files of MARHYD: the MAgdalena River HYdrodynamic model in Delft3D. Model description: The model domain of MARHYD extends from coordinates 10.9619 °N to 11.2669° N and from 74.7571 °W to 74.8784 °W. This domain includes the last 22 km of the river and estuary before discharging into the Caribbean Sea and 63 km by 37 km of the surrounding coastal region in east-west and north-south directions. In oceanic waters, the model is rectangular, configured on a 150 m x 150 m horizontal resolution near the open boundaries, with a gradual refinement to 50 m x 50 m near the river mouth. In the river and estuary, the model is curvilinear, with 10 horizontal cells in the transversal section, reaching a variable size between 40 m to 100 m. 40 Z-layers represent the water column with a higher resolution close to the surface. Layers of approximately 0.5 m cover the upper 10 m of the water columns, where most of the mixing processes between the river and the ocean occur. The vertical resolution reduces progressively from 10 m depth to the bottom. The boundary conditions of salinity and currents with the Caribbean Sea (at the North, East, and West) were obtained from HYCOM + NODA reanalysis every 6 hours, and wind velocity was obtained from CFSR-NCEP/NCAR reanalysis every 1 hour for the wind stress. The bathymetry was derived from GEBCO, Nautical charts of the Maritime Directorate of Colombia (DIMAR), and high-resolution in-situ measurements. River discharge data were obtained from the nearest upstream hydrological station of the Magdalena River. The model was calibrated and validated using field data of salinity profiles along the river estuary and plume, velocity measurements in the river and estuary, and water level in the estuary for two climatic seasons. Description of simulation case: Case 2 corresponds to a low-discharge scenario with Q = 6800 m^3/s, equivalent to the 50th percentile of the historical freshwater flow. Water currents, salinity and water level in the open boundaries correspond to the time-average of HYCOM Reanalysis database for the dates between 9th and 29th of November of 2017. Winds are constant with a speed of 11.3 m/s from the Northeast. The full set of input (configuration) files of this simulation can be found in the dataset: Barros, Yennis ; Saavedra, Victor; Álvarez-Silva, Óscar; Cardona, Yuley; Cáceres-Euse, Alejandro; Osorio, Andres F.; Arbeláez, Felipe (2021), “MARHYD: Magdalena River Hydrodynamic model in Delft3D. Database 1 of 5: Inputs”, Mendeley Data, V1, doi: 10.17632/hmhdvg47kg.1 Files description: This dataset includes the water velocity results for the entire computational domain, every 8 hours during 20 days of simulation. ​ The data are in .nc format. Results of salinity and water level for this simulation case can be found in the database: MARHYD: Magdalena River Hydrodynamic model in Delft3D. Results of Case 2 (salinity and water level), doi: 10.17632/r99xkp2czc.1
DOI: 10.17632/zhtwsdzr6c.1
title: MARHYD: Magdalena River Hidrodynamic model in Delft3D. Results of Case 1 (salinity and water level)

description: This database contains output files of MARHYD: the MAgdalena River HYdrodynamic model in Delft3D. Model description: The model domain of MARHYD extends from coordinates 10.9619 °N to 11.2669° N and from 74.7571 °W to 74.8784 °W. This domain includes the last 22 km of the river and estuary before discharging into the Caribbean Sea and 63 km by 37 km of the surrounding coastal region in east-west and north-south directions. In oceanic waters, the model is rectangular, configured on a 150 m x 150 m horizontal resolution near the open boundaries, with a gradual refinement to 50 m x 50 m near the river mouth. In the river and estuary, the model is curvilinear, with 10 horizontal cells in the transversal section, reaching a variable size between 40 m to 100 m. 40 Z-layers represent the water column with a higher resolution close to the surface. Layers of approximately 0.5 m cover the upper 10 m of the water columns, where most of the mixing processes between the river and the ocean occur. The vertical resolution reduces progressively from 10 m depth to the bottom. The boundary conditions of salinity and currents with the Caribbean Sea (at the North, East, and West) were obtained from HYCOM + NODA reanalysis every 6 hours, and wind velocity was obtained from CFSR-NCEP/NCAR reanalysis every 1 hour for the wind stress. The bathymetry was derived from GEBCO, Nautical charts of the Maritime Directorate of Colombia (DIMAR), and high-resolution in-situ measurements. River discharge data were obtained from the nearest upstream hydrological station of the Magdalena River. The model was calibrated and validated using field data of salinity profiles along the river estuary and plume, velocity measurements in the river and estuary, and water level in the estuary for two climatic seasons. Description of simulation case: Case 1 corresponds to a low-discharge scenario with Q = 3400 m^3/s, equivalent to the 10th percentile of the historical freshwater flow. Water currents, salinity and water level in the open boundaries correspond to the time-average of HYCOM Reanalysis database for the days between 9 and 29 of November of 2017. Winds are constant with a speed of 10.5 m/s from the Northeast. The full set of input (configuration) files of this simulation can be found in the dataset: Barros, Yennis ; Saavedra, Victor; Álvarez-Silva, Óscar; Cardona, Yuley; Cáceres-Euse, Alejandro; Osorio, Andres F.; Arbeláez, Felipe (2021), “MARHYD: Magdalena River Hydrodynamic model in Delft3D. Database 1 of 5: Inputs”, Mendeley Data, V1, doi: 10.17632/hmhdvg47kg.1 Files description: This dataset includes the salinity and water level results for the whole computational domain every 8 hours during 20 days of simulation. ​ The data is in .nc format. Results of water velocity for this simulation can be found in the database: MARHYD: Magdalena River Hydrodynamic model in Delft3D. Results of Case 1 (water velocity), doi: 10.17632/vxs52f7fcd.1
DOI: 10.5281/zenodo.4906457
title: [Dataset] A Particle-In-Cell Code Comparison for Ion Acceleration: EPOCH, LSP, and WarpX

description: Here we share simulation results comparing three Particle-In-Cell (PIC) codes: <br> - EPOCH (using the normal random seed and 20 additional runs with different seeds),<br> - LSP (using both explicit and implicit modes labeled LSP_E and LSP_I), <br> - WarpX Notes:<br> - Since the previous upload, the WarpX particle energy distributions have been updated to include the virtual (py) momenta<br> - LSP makes calculations using a virtual dimension of 1 cm while the other codes use 1 meter<br> - See the corresponding manuscript for full problem description and context Explanation of Folders/Files:<br> -&gt; Energy_Diagnostics<br> - This directory has files containing field and particle energy information for each code<br> - Various file formats are used, see headers for information on data format<br> - As mentioned above LSP uses a different convention for the virtual dimension size, so the outputs must be multiplied by 100 for comparison <br> <br> -&gt; Particle_Spectra<br> - This directory contains calculated energy distributions of forward going particles for the various runs. <br> - The file number multiplied by 10 fs gives the simulation time (e.g. 30_Spectrum.dat is 300 fs)<br> - In the files, the first column is the energy bin (MeV), the second is total ion charge (C), and third is electron charge (C)<br> - As mentioned above LSP uses a different convention for the virtual dimension size, so the outputs must be multiplied by 100 for comparison<br> <br> -&gt;Simulation_Input_Files<br> - EPOCH and WarpX simulation input decks (input files) are included here <br> - LSP is a commercial code. If you have access to the code and are interested in the input files, please contact us. <br> <br> -&gt; EPOCH_20_Runs_Density_Map<br> - An array of the simulation space denoting whether at least one of the 20 additional EPOCH simulations had non-zero ion density for the corresponding plot step (every 10 fs)<br>
DOI: 10.5281/zenodo.4651296
title: [Dataset] A Particle-In-Cell Code Comparison for Ion Acceleration: EPOCH, LSP, and WarpX

description: Here we share simulation results comparing three Particle-In-Cell (PIC) codes: <br> - EPOCH (using the normal random seed and 20 additional runs with different seeds),<br> - LSP (using both explicit and implicit modes labeled LSP_E and LSP_I), <br> - WarpX Notes:<br> - Since the previous upload, the WarpX particle energy distributions have been updated to include the virtual (py) momenta<br> - LSP makes calculations using a virtual dimension of 1 cm while the other codes use 1 meter<br> - See the corresponding manuscript for full problem description and context Explanation of Folders/Files:<br> -&gt; Energy_Diagnostics<br> - This directory has files containing field and particle energy information for each code<br> - Various file formats are used, see headers for information on data format<br> - As mentioned above LSP uses a different convention for the virtual dimension size, so the outputs must be multiplied by 100 for comparison <br> <br> -&gt; Particle_Spectra<br> - This directory contains calculated energy distributions of forward going particles for the various runs. <br> - The file number multiplied by 10 fs gives the simulation time (e.g. 30_Spectrum.dat is 300 fs)<br> - In the files, the first column is the energy bin (MeV), the second is total ion charge (C), and third is electron charge (C)<br> - As mentioned above LSP uses a different convention for the virtual dimension size, so the outputs must be multiplied by 100 for comparison<br> <br> -&gt;Simulation_Input_Files<br> - EPOCH and WarpX simulation input decks (input files) are included here <br> - LSP is a commercial code. If you have access to the code and are interested in the input files, please contact us. <br> <br> -&gt; EPOCH_20_Runs_Density_Map<br> - An array of the simulation space denoting whether at least one of the 20 additional EPOCH simulations had non-zero ion density for the corresponding plot step (every 10 fs)<br>
DOI: 10.15468/xuzjgv
title: Redescriptions of Neanthes Kinberg, 1865 (Annelida: Errantia: Nereididae) species from worldwide regions

description: This dataset contains the digitized treatments in Plazi based on the original journal article Villalobos-Guerrero, Tulio F., Kara, Jyothi, Idris, Izwandy (2021): Redescriptions of Neanthes Kinberg, 1865 (Annelida: Errantia: Nereididae) species from worldwide regions. European Journal of Taxonomy 760 (1): 101-135, DOI: https://doi.org/10.5852/ejt.2021.760.1443, URL: http://zoobank.org/917481ff-7c89-4b0f-8c91-77e616271ecc
DOI: 10.25345/c5483n
title: MassIVE MSV000087866 - Interactive effects Clavibacter michiganensis subsp. michiganensis and Pseudomonas entomophila strain 23S in-culture secretome
title: This research aims at studying the responses of Clavibacter michiganensis subsp. michiganensis (Cmm) to Pseudomonas entomophila strain 23S when grown as pure culture and as mixed culture. The secretome of the cultures were analysed using LC-MS/MS.
DOI: 10.15468/zxjhbw
title: The first Pan-Podocnemididae turtle egg from the Presidente Prudente Formation (Late Cretaceous, Bauru Group), Brazil

description: This dataset contains the digitized treatments in Plazi based on the original journal article Marsola, Júlio C. De A., Grellet-Tinner, Gerald, Montefeltro, Felipe C., Langer, Max C. (2014): The first Pan-Podocnemididae turtle egg from the Presidente Prudente Formation (Late Cretaceous, Bauru Group), Brazil. Zootaxa 3872 (2): 187-194, DOI: http://dx.doi.org/10.11646/zootaxa.3872.2.5
DOI: 10.5281/zenodo.5122589
title: Raw dataset

description: Raw dataset: Effect of exposure to traumatic events on the development of post-traumatic disorder symptoms in municipal police officers
DOI: 10.34808/qv8z-c216
title: Bibliometric data for a research study on scientific productivity of Polish technical universities (Koszalin University of Technology 2016-2020) retrieved by InCites benchmarking tool.

description: This dataset was created for the purpose of research on scientific productivity at Polish technical universities.The raw data was retrieved in July 2021 by the InCites benchmarking tool in xlsx format and will be used to create the research profiles of the universities and underlying data of journals articles. The most common definition of research productivity (interchangeable with academic productivity or scientific productivity)  states as research productivity are the number of publications per researchers. However, a more extended definition of scientific productivity, connecting quantity and quality approach involves producing quality research represented by publishing academic papers in reputable international journals, citing these papers, gaining research funding (e.g. national and international grants), and collaborating in scientific teams.
The dataset prepared for the scientific profile of Koszalin University of Technology consists records from 2016-2020: Number of Web of Science Documents, Times Cited, % Docs Cited, Rank, Category Normalized Citation Impact, International Collaborations, All Open Access Documents, % International Collaborations, Documents in JIF Journals, Documents in Q1 Journals, Documents in Q2 Journals, Documents in Q3 Journals, Documents in Q4 Journals.
DOI: 10.5281/zenodo.5122588
title: Raw dataset

description: Raw dataset: Effect of exposure to traumatic events on the development of post-traumatic disorder symptoms in municipal police officers
DOI: 10.34808/96fp-2202
title: Bibliometric data for a research study on scientific productivity of Polish technical universities (Gdańsk University of Technology 2016-2020) retrieved by InCites benchmarking tool.

description: This dataset was created for the purpose of research on scientific productivity at Polish technical universities.The raw data was retrieved in July 2021 by the InCites benchmarking tool in xlsx format and will be used to create the research profiles of the universities and underlying data of journals articles. The most common definition of research productivity (interchangeable with academic productivity or scientific productivity)  states as research productivity are the number of publications per researchers. However, a more extended definition of scientific productivity, connecting quantity and quality approach involves producing quality research represented by publishing academic papers in reputable international journals, citing these papers, gaining research funding (e.g. national and international grants), and collaborating in scientific teams.
The dataset prepared for the scientific profile of Gdańsk University of Technology consists records from 2016-2020: Number of Web of Science Documents, Times Cited, % Docs Cited, Rank, Category Normalized Citation Impact, International Collaborations, All Open Access Documents, % International Collaborations, Documents in JIF Journals, Documents in Q1 Journals, Documents in Q2 Journals, Documents in Q3 Journals, Documents in Q4 Journals.
DOI: 10.5281/zenodo.5122883
title: PJM East

description: PJM Interconnection LLC (PJM) is a regional transmission organization (RTO) in the United States. It is part of the Eastern Interconnection grid operating an electric transmission system serving all or parts of Delaware, Illinois, Indiana, Kentucky, Maryland, Michigan, New Jersey, North Carolina, Ohio, Pennsylvania, Tennessee, Virginia, West Virginia, and the District of Columbia. The hourly power consumption data comes from PJM's website and are in megawatts (MW). The regions have changed over the years so data may only appear for certain dates per region.
DOI: 10.5281/zenodo.5122882
title: PJM East

description: PJM Interconnection LLC (PJM) is a regional transmission organization (RTO) in the United States. It is part of the Eastern Interconnection grid operating an electric transmission system serving all or parts of Delaware, Illinois, Indiana, Kentucky, Maryland, Michigan, New Jersey, North Carolina, Ohio, Pennsylvania, Tennessee, Virginia, West Virginia, and the District of Columbia. The hourly power consumption data comes from PJM's website and are in megawatts (MW). The regions have changed over the years so data may only appear for certain dates per region.
DOI: 10.15468/g5q6zc
title: The status of Crossopalpus obscuripes (Adams), a new junior synonym of Crossopalpus aenescens (Wiedemann) (Diptera: Hybotidae: Tachydromiinae)

description: This dataset contains the digitized treatments in Plazi based on the original journal article Cumming, Jeffrey M., Sinclair, Bradley J. (2014): The status of Crossopalpus obscuripes (Adams), a new junior synonym of Crossopalpus aenescens (Wiedemann) (Diptera: Hybotidae: Tachydromiinae). Zootaxa 3872 (4): 398-400, DOI: http://dx.doi.org/10.11646/zootaxa.3872.4.8