cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.5281/zenodo.8422666
title: SUPERYACHT_2019_Rrs

description: Archimedes Yacht surface hyperspectral remote sensing reflectance (Rrs) 2019 Hyperspectral remote sensing reflectance data collected on Archimedes Yacht in the Atlantic and Mediterranean Sea in 2019. Time stamp is in UTC. Ocean-colour sensors mounted on satellites can view the entire ocean over a period of a few days. However, to calibrate these sensors and validate the data, satellite observations must be compared with accurate and reliable in situ measurements, collected at the ocean surface. There are many regions of the ocean where these in situ measurements are rarely collected. Ocean-colour sensors can be mounted on research vessels and ships of opportunity. In this project, an ocean-colour sensor (Seabird HyperSAS Solar Tracker) was mounted on a yacht that visits remote regions of the planet where few observations have been collected. This project aims to process this data to a level for use by the scientific community for scientific applications, such as satellite validation.
DOI: 10.5281/zenodo.8422649
title: Dataset for Article: Numerical investigation of a graphene-on-semiconductor device for optical monitoring of cell electrophysiology

description: Matlab scripts used in the preparation of data and figures for the publication "Numerical investigation of a graphene-on-semiconductor device for optical monitoring of cell electrophysiology" in iScience
DOI: 10.5281/zenodo.8422648
title: Dataset for Article: Numerical investigation of a graphene-on-semiconductor device for optical monitoring of cell electrophysiology

description: Matlab scripts used in the preparation of data and figures for the publication "Numerical investigation of a graphene-on-semiconductor device for optical monitoring of cell electrophysiology" in iScience
DOI: 10.5281/zenodo.8422675
title: SUPERYACHT_2020_Rrs

description: Archimedes Yacht surface hyperspectral remote sensing reflectance (Rrs) 2020 Hyperspectral remote sensing reflectance data collected on Archimedes Yacht in the Atlantic, Pacific and Southern Ocean in 2020. Time stamp is in UTC. Ocean-colour sensors mounted on satellites can view the entire ocean over a period of a few days. However, to calibrate these sensors and validate the data, satellite observations must be compared with accurate and reliable in situ measurements, collected at the ocean surface. There are many regions of the ocean where these in situ measurements are rarely collected. Ocean-colour sensors can be mounted on research vessels and ships of opportunity. In this project, an ocean-colour sensor (Seabird HyperSAS Solar Tracker) was mounted on a yacht that visits remote regions of the planet where few observations have been collected. This project aims to process this data to a level for use by the scientific community for scientific applications, such as satellite validation.
DOI: 10.5281/zenodo.8422674
title: SUPERYACHT_2020_Rrs

description: Archimedes Yacht surface hyperspectral remote sensing reflectance (Rrs) 2020 Hyperspectral remote sensing reflectance data collected on Archimedes Yacht in the Atlantic, Pacific and Southern Ocean in 2020. Time stamp is in UTC. Ocean-colour sensors mounted on satellites can view the entire ocean over a period of a few days. However, to calibrate these sensors and validate the data, satellite observations must be compared with accurate and reliable in situ measurements, collected at the ocean surface. There are many regions of the ocean where these in situ measurements are rarely collected. Ocean-colour sensors can be mounted on research vessels and ships of opportunity. In this project, an ocean-colour sensor (Seabird HyperSAS Solar Tracker) was mounted on a yacht that visits remote regions of the planet where few observations have been collected. This project aims to process this data to a level for use by the scientific community for scientific applications, such as satellite validation.
DOI: 10.5281/zenodo.8422703
title: TumourMethData Transcript Counts

description: RNA-Seq Kallisto transcript counts for TumourMethData
DOI: 10.5281/zenodo.8422702
title: TumourMethData Transcript Counts

description: RNA-Seq Kallisto transcript counts for TumourMethData
DOI: 10.25345/c5kp7v250
title: MassIVE MSV000093068 - Identification of PIP5K1a-associated proteins in human Th17 cells by IP-MS
title: human Th17 cells generated in vitro from naive T cells + anti-CD3+IL-23+IL1b for 5 days, then immunopreciptation performed with anti-PIP5K1a or IgG controls and submitted to MSBioworks for LC-MS analysis. 3 individual experiments with 3 unique donors.
DOI: 10.5281/zenodo.8403807
title: 3D printed models are an accurate, cost-effective, and reproducible tool for quantifying terrestrial thermal environments

description: Dataset used in Alujević et al. 2023. 3D printed models are an accurate, cost-effective, and reproducible tool for quantifying terrestrial thermal environments.
DOI: 10.5281/zenodo.8403806
title: 3D printed models are an accurate, cost-effective, and reproducible tool for quantifying terrestrial thermal environments

description: Dataset used in Alujević et al. 2023. 3D printed models are an accurate, cost-effective, and reproducible tool for quantifying terrestrial thermal environments.
DOI: 10.18739/a2kp7ts45
title: Seasonal soil active layer measurements from a Circumpolar Active Layer monitoring (CALM) grid, (R-32) Talnakh (Norilsk), Central Siberia. 2005-2020.

description: The Circumpolar Active Layer Monitoring (CALM) program represents the only coordinated program providing collection, standardization, open access, and dissemination of active-layer data world-wide. Widespread, systematic changes in the thickness of the active layer could have profound effects on the flux of greenhouse gases, on the human infrastructure in cold regions, and on landscape and hydrologic processes. It is therefore critical that observational and analytical procedures continue over decadal periods to assess trends and detect cumulative, long-term changes. This dataset contains active-layer observations conducted by the CALM program since the 1990s, supported by a series of National Science Foundation (NSF) awards. CALM program is an integral part of the Global Terrestrial Network for Permafrost. CALM 2020 data are significantly reduced due to pandemic-related travel restrictions. Available 2020 data are limited in terms of extent, and observations were not as controlled as previous years in terms of measurement timing or method, and therefore should be treated with caution.
DOI: 10.5517/ccdc.csd.cc24mwnb
title: CCDC 1985322: Experimental Crystal Structure Determination

description: Related Article: Yu Hao, Zi-Hao Li, Peng-Fei Lian, Quan-Zhe Li, Yuan She, Zhi-Gang Ma, Shu-Yu Zhang|2023|Org.Lett.|25|6913|doi:10.1021/acs.orglett.3c02690
description: An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
DOI: 10.5517/ccdc.csd.cc2brzdh
title: CCDC 2167997: Experimental Crystal Structure Determination

description: Related Article: Emmanouil Broumidis, Christopher G. Thomson, Brendan Gallagher, Lia Sotorríos, Kenneth G. McKendrick, Stuart A. Macgregor, Martin J. Paterson, Janet E. Lovett, Gareth O. Lloyd, Georgina M. Rosair, Andreas S. Kalogirou, Panayiotis A. Koutentis, Filipe Vilela|2023|Org.Lett.|25|6907|doi:10.1021/acs.orglett.3c02673
description: An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
DOI: 10.5517/ccdc.csd.cc2brzhl
title: CCDC 2168000: Experimental Crystal Structure Determination

description: Related Article: Emmanouil Broumidis, Christopher G. Thomson, Brendan Gallagher, Lia Sotorríos, Kenneth G. McKendrick, Stuart A. Macgregor, Martin J. Paterson, Janet E. Lovett, Gareth O. Lloyd, Georgina M. Rosair, Andreas S. Kalogirou, Panayiotis A. Koutentis, Filipe Vilela|2023|Org.Lett.|25|6907|doi:10.1021/acs.orglett.3c02673
description: An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
DOI: 10.5517/ccdc.csd.cc2bs4kv
title: CCDC 2168157: Experimental Crystal Structure Determination

description: Related Article: Emmanouil Broumidis, Christopher G. Thomson, Brendan Gallagher, Lia Sotorríos, Kenneth G. McKendrick, Stuart A. Macgregor, Martin J. Paterson, Janet E. Lovett, Gareth O. Lloyd, Georgina M. Rosair, Andreas S. Kalogirou, Panayiotis A. Koutentis, Filipe Vilela|2023|Org.Lett.|25|6907|doi:10.1021/acs.orglett.3c02673
description: An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
DOI: 10.18739/a27s7hs3w
title: Thaw depth measurements from the Circumpolar Active Layer Monitoring (CALM) project for site 'Cape Chukochi, alas, Kolyma' (R13 B), North East Siberia, Russia from 2000-2018

description: The primary goal of the Circumpolar Active Layer Monitoring (CALM) program is to observe the response of the active layer and near-surface permafrost to climate change over long (multi-decadal) time scales. The CALM observational network, established in the 1990s, observes the long-term response of the active layer and near-surface permafrost to changes and variations in climate at more than 200 sites in both hemispheres. CALM currently has participants from 15 countries. Majority of sites measure active-layer thickness on grids ranging from 1 hecatre to 1 square kilometer, and observe soil temperatures. Most sites in the CALM network are located in Arctic and Subarctic lowlands. Southern Hemisphere component (CALM-South) is being organized and currently includes sites in Antarctic and South America. The broader impacts of this project are derived from the hypothesis that widespread, systematic changes in the thickness of the active layer could have profound effects on the flux of greenhouse gases, on the human infrastructure in cold regions, and on landscape processes. It is therefore critical that observational and analytical procedures continue over decadal periods to assess trends and detect cumulative, long-term changes. The CALM program began in 1991. It was initially affiliated with the International Tundra Experiment and has been supported independently and continuously since 1998 through grants from the United States National Science Foundation (NSF). CALM is funded by the NSF Award 1304555 (Polar Programs). This dataset and metadata record was automatically generated from a web crawl of the original project page https://www2.gwu.edu/~calm/data/north.htm at the request of project coordinators. More information about this site and others in the project can be found at https://www2.gwu.edu/~calm/data/north.htm and also http://gtnpdatabase.org/activelayers.
DOI: 10.18739/a2cj87k71
title: Thaw depth measurements from the Circumpolar Active Layer Monitoring (CALM) project for site 'Deadhorse' (U6), Alaska North Slope, United States (Alaska) from 1996-2018

description: The primary goal of the Circumpolar Active Layer Monitoring (CALM) program is to observe the response of the active layer and near-surface permafrost to climate change over long (multi-decadal) time scales. The CALM observational network, established in the 1990s, observes the long-term response of the active layer and near-surface permafrost to changes and variations in climate at more than 200 sites in both hemispheres. CALM currently has participants from 15 countries. Majority of sites measure active-layer thickness on grids ranging from 1 hecatre to 1 square kilometer, and observe soil temperatures. Most sites in the CALM network are located in Arctic and Subarctic lowlands. Southern Hemisphere component (CALM-South) is being organized and currently includes sites in Antarctic and South America. The broader impacts of this project are derived from the hypothesis that widespread, systematic changes in the thickness of the active layer could have profound effects on the flux of greenhouse gases, on the human infrastructure in cold regions, and on landscape processes. It is therefore critical that observational and analytical procedures continue over decadal periods to assess trends and detect cumulative, long-term changes. The CALM program began in 1991. It was initially affiliated with the International Tundra Experiment and has been supported independently and continuously since 1998 through grants from the United States National Science Foundation (NSF). CALM is funded by the NSF Award 1304555 (Polar Programs). This dataset and metadata record was automatically generated from a web crawl of the original project page https://www2.gwu.edu/~calm/data/north.htm at the request of project coordinators. More information about this site and others in the project can be found at https://www2.gwu.edu/~calm/data/north.htm and also http://gtnpdatabase.org/activelayers.
DOI: 10.18739/a2h98zd1d
title: Thaw depth measurements from the Circumpolar Active Layer Monitoring (CALM) project for site '56 Mile' (U31), Alaska North Slope, United States (Alaska) from 1996-2018

description: The primary goal of the Circumpolar Active Layer Monitoring (CALM) program is to observe the response of the active layer and near-surface permafrost to climate change over long (multi-decadal) time scales. The CALM observational network, established in the 1990s, observes the long-term response of the active layer and near-surface permafrost to changes and variations in climate at more than 200 sites in both hemispheres. CALM currently has participants from 15 countries. Majority of sites measure active-layer thickness on grids ranging from 1 hecatre to 1 square kilometer, and observe soil temperatures. Most sites in the CALM network are located in Arctic and Subarctic lowlands. Southern Hemisphere component (CALM-South) is being organized and currently includes sites in Antarctic and South America. The broader impacts of this project are derived from the hypothesis that widespread, systematic changes in the thickness of the active layer could have profound effects on the flux of greenhouse gases, on the human infrastructure in cold regions, and on landscape processes. It is therefore critical that observational and analytical procedures continue over decadal periods to assess trends and detect cumulative, long-term changes. The CALM program began in 1991. It was initially affiliated with the International Tundra Experiment and has been supported independently and continuously since 1998 through grants from the United States National Science Foundation (NSF). CALM is funded by the NSF Award 1304555 (Polar Programs). This dataset and metadata record was automatically generated from a web crawl of the original project page https://www2.gwu.edu/~calm/data/north.htm at the request of project coordinators. More information about this site and others in the project can be found at https://www2.gwu.edu/~calm/data/north.htm and also http://gtnpdatabase.org/activelayers.
DOI: 10.48331/scielo.r7ofpq/veciag
title: PPT_SciELO25_SciELO South Africa_final.pdf

description: :unav
DOI: 10.48331/scielo.r7ofpq
title: Presentations of the National Coordinations - SciELO South Africa

description: Presentation by Louise van Heerden in the Presentations of the National Coordinations panel of the SciELO 25 Years Week. Event page: https://25.scielo.org/en
DOI: 10.18739/a2n29p65j
title: Thaw depth measurements from the Circumpolar Active Layer Monitoring (CALM) project for site 'Ivotuk 1 km grid' (U26), Alaska North Slope, United States (Alaska) from 2000-2018

description: The primary goal of the Circumpolar Active Layer Monitoring (CALM) program is to observe the response of the active layer and near-surface permafrost to climate change over long (multi-decadal) time scales. The CALM observational network, established in the 1990s, observes the long-term response of the active layer and near-surface permafrost to changes and variations in climate at more than 200 sites in both hemispheres. CALM currently has participants from 15 countries. Majority of sites measure active-layer thickness on grids ranging from 1 hecatre to 1 square kilometer, and observe soil temperatures. Most sites in the CALM network are located in Arctic and Subarctic lowlands. Southern Hemisphere component (CALM-South) is being organized and currently includes sites in Antarctic and South America. The broader impacts of this project are derived from the hypothesis that widespread, systematic changes in the thickness of the active layer could have profound effects on the flux of greenhouse gases, on the human infrastructure in cold regions, and on landscape processes. It is therefore critical that observational and analytical procedures continue over decadal periods to assess trends and detect cumulative, long-term changes. The CALM program began in 1991. It was initially affiliated with the International Tundra Experiment and has been supported independently and continuously since 1998 through grants from the United States National Science Foundation (NSF). CALM is funded by the NSF Award 1304555 (Polar Programs). This dataset and metadata record was automatically generated from a web crawl of the original project page https://www2.gwu.edu/~calm/data/north.htm at the request of project coordinators. More information about this site and others in the project can be found at https://www2.gwu.edu/~calm/data/north.htm and also http://gtnpdatabase.org/activelayers.
DOI: 10.18739/a2rr1pm66
title: Thaw depth measurements from the Circumpolar Active Layer Monitoring (CALM) project for site 'Urengoy Gas Field GP5' (R50a), West Siberia, Russia from 2008-2018

description: The primary goal of the Circumpolar Active Layer Monitoring (CALM) program is to observe the response of the active layer and near-surface permafrost to climate change over long (multi-decadal) time scales. The CALM observational network, established in the 1990s, observes the long-term response of the active layer and near-surface permafrost to changes and variations in climate at more than 200 sites in both hemispheres. CALM currently has participants from 15 countries. Majority of sites measure active-layer thickness on grids ranging from 1 hecatre to 1 square kilometer, and observe soil temperatures. Most sites in the CALM network are located in Arctic and Subarctic lowlands. Southern Hemisphere component (CALM-South) is being organized and currently includes sites in Antarctic and South America. The broader impacts of this project are derived from the hypothesis that widespread, systematic changes in the thickness of the active layer could have profound effects on the flux of greenhouse gases, on the human infrastructure in cold regions, and on landscape processes. It is therefore critical that observational and analytical procedures continue over decadal periods to assess trends and detect cumulative, long-term changes. The CALM program began in 1991. It was initially affiliated with the International Tundra Experiment and has been supported independently and continuously since 1998 through grants from the United States National Science Foundation (NSF). CALM is funded by the NSF Award 1304555 (Polar Programs). This dataset and metadata record was automatically generated from a web crawl of the original project page https://www2.gwu.edu/~calm/data/north.htm at the request of project coordinators. More information about this site and others in the project can be found at https://www2.gwu.edu/~calm/data/north.htm and also http://gtnpdatabase.org/activelayers.
DOI: 10.18739/a2wh2df0z
title: Thaw depth measurements from the Circumpolar Active Layer Monitoring (CALM) project for site 'Allaiha (Indigirka basin)' (R31), North East Siberia, Russia from 2004-2018

description: The primary goal of the Circumpolar Active Layer Monitoring (CALM) program is to observe the response of the active layer and near-surface permafrost to climate change over long (multi-decadal) time scales. The CALM observational network, established in the 1990s, observes the long-term response of the active layer and near-surface permafrost to changes and variations in climate at more than 200 sites in both hemispheres. CALM currently has participants from 15 countries. Majority of sites measure active-layer thickness on grids ranging from 1 hecatre to 1 square kilometer, and observe soil temperatures. Most sites in the CALM network are located in Arctic and Subarctic lowlands. Southern Hemisphere component (CALM-South) is being organized and currently includes sites in Antarctic and South America. The broader impacts of this project are derived from the hypothesis that widespread, systematic changes in the thickness of the active layer could have profound effects on the flux of greenhouse gases, on the human infrastructure in cold regions, and on landscape processes. It is therefore critical that observational and analytical procedures continue over decadal periods to assess trends and detect cumulative, long-term changes. The CALM program began in 1991. It was initially affiliated with the International Tundra Experiment and has been supported independently and continuously since 1998 through grants from the United States National Science Foundation (NSF). CALM is funded by the NSF Award 1304555 (Polar Programs). This dataset and metadata record was automatically generated from a web crawl of the original project page https://www2.gwu.edu/~calm/data/north.htm at the request of project coordinators. More information about this site and others in the project can be found at https://www2.gwu.edu/~calm/data/north.htm and also http://gtnpdatabase.org/activelayers.