cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.880089
title: Soil temperature and volumetric soil moisture at Bayelva Station in 1998 (level 2)
DOI: 10.1594/pangaea.942858
title: Basic measurements of radiation at station Abashiri (2021-10)
DOI: 10.1594/pangaea.880078
title: Snow height at Bayelva Station in 2007 (level 2)
DOI: 10.1594/pangaea.880079
title: Snow height at Bayelva Station in 2008 (level 2)
DOI: 10.1594/pangaea.880092
title: Soil temperature and volumetric soil moisture at Bayelva Station in 2001 (level 2)
DOI: 10.1594/pangaea.905233
title: Soil data at station Samoylov (2002-2018, level 1, version 201908), link to archive

description: This is an updated version of this data: https://doi.pangaea.de/10.1594/PANGAEA.891140, please use and cite the updated version!
DOI: 10.1594/pangaea.825418
title: (Figure 4) Age and Calcium/Titanium ratio of sediment core GeoB10709-6
DOI: 10.1594/pangaea.881827
title: Meteorological observations at Bayelva Station in 2010 (level 1)
DOI: 10.1594/pangaea.880085
title: Snow height at Bayelva Station in 2014 (level 2)
DOI: 10.1594/pangaea.880105
title: Soil temperature and volumetric soil moisture at Bayelva Station in 2013 (level 2)
DOI: 10.1594/pangaea.880086
title: Snow height at Bayelva Station in 2015 (level 2)
DOI: 10.1594/pangaea.825414
title: (Figure 4) Age and Calcium/Titanium ratio of sediment core GeoB10703-5
DOI: 10.1594/pangaea.881829
title: Meteorological observations at Bayelva Station in 2012 (level 1)
DOI: 10.1594/pangaea.825415
title: (Figure 4) Age and Calcium/Titanium ratio of sediment core GeoB10704-5
DOI: 10.1594/pangaea.881832
title: Meteorological observations at Bayelva Station in 2015 (level 1)
DOI: 10.1594/pangaea.947047
title: Meteorologic data at station Samoylov (2019)

description: Understanding permafrost processes and changes requires long-term observational datasets. This dataset is a continuation of the dataset available from the long-term observational site Samoylov, located in the Lena River Delta, Siberia (72.37°N, 126.48°E). The location is characterized by a cold, dry tundra climate with mean annual air temperature of -11.7°C (using years with complete data between 1998 and 2017). The monthly mean temperatures over this period varied between 9.4°C in the warmest month (July) and -31.7°C in the coldest month (February). The average summer rainfall (June-October) was 145.2 mm. This dataset adds recent years to the observations of meteorological parameters, energy balance, and subsurface observations which have been recorded since 1998. The instrumentation, calibration, processing and data quality control is explained in Boike et al. (2019). The data provide observations of temporally variable parameters that mitigate energy fluxes between permafrost and atmosphere, such as snow depth, snow temperature, liquid precipitation, water level, air temperature, relative humidity, wind speed and direction, atmospheric pressure and radiation fluxes. The observations are suitable for use in integrating, calibrating and testing permafrost as a component in Earth System Models. The resulting quality-controlled dataset is unique in the Arctic and serves as a baseline for future studies.
DOI: 10.1594/pangaea.891141
title: Soil data at station Samoylov (2002-2018, level 2, version 1), link to archive

description: This is an outdated version of the data, please use and cite this data instead: https://doi.pangaea.de/10.1594/PANGAEA.905234
DOI: 10.1594/pangaea.881815
title: Meteorological observations at Bayelva Station in 1998 (level 1)
DOI: 10.1594/pangaea.881817
title: Meteorological observations at Bayelva Station in 2000 (level 1)
DOI: 10.1594/pangaea.881818
title: Meteorological observations at Bayelva Station in 2001 (level 1)
DOI: 10.1594/pangaea.882060
title: Soil data at station Bayelva (1998-2017, level 1, version 1), link to archive
DOI: 10.1594/pangaea.934644
title: Basic measurements of radiation at station Abashiri (2021-04)
DOI: 10.1594/pangaea.881831
title: Meteorological observations at Bayelva Station in 2014 (level 1)
DOI: 10.1594/pangaea.881821
title: Meteorological observations at Bayelva Station in 2004 (level 1)
DOI: 10.1594/pangaea.881825
title: Meteorological observations at Bayelva Station in 2008 (level 1)
DOI: 10.1594/pangaea.880087
title: Snow height at Bayelva Station in 2016 (level 2)
DOI: 10.1594/pangaea.935446
title: Basic measurements of radiation at station Abashiri (2021-06)
DOI: 10.1594/pangaea.881823
title: Meteorological observations at Bayelva Station in 2006 (level 1)
DOI: 10.1594/pangaea.937869
title: Basic measurements of radiation at station Abashiri (2021-08)
DOI: 10.1594/pangaea.954792
title: Basic measurements of radiation at station Abashiri (2022-08)
DOI: 10.1594/pangaea.937866
title: Basic measurements of radiation at station Abashiri (2021-07)
DOI: 10.1594/pangaea.974704
title: Basic measurements of radiation at station Abashiri (2024-11)
DOI: 10.1594/pangaea.880101
title: Soil temperature and volumetric soil moisture at Bayelva Station in 2009 (level 2)
DOI: 10.1594/pangaea.880104
title: Soil temperature and volumetric soil moisture at Bayelva Station in 2012 (level 2)
DOI: 10.1594/pangaea.880094
title: Soil temperature and volumetric soil moisture at Bayelva Station in 2003 (level 2)
DOI: 10.1594/pangaea.880099
title: Soil temperature and volumetric soil moisture at Bayelva Station in 2007 (level 2)
DOI: 10.1594/pangaea.880102
title: Soil temperature and volumetric soil moisture at Bayelva Station in 2010 (level 2)
DOI: 10.1594/pangaea.936226
title: Soil data at station Bayelva (2020, level 1)

description: Understanding permafrost processes and changes requires long-term observational datasets. This dataset is a continuation of the dataset available from the Bayelva Site at Ny-Ålesund, Svalbard, where meteorology, energy balance components and subsurface observations have been made for more than the last 20 years. The data provide observations of temporally variable parameters that mitigate energy fluxes between permafrost and the atmosphere, such as active layer and permafrost temperature, soil volumetric water content and soil bulk electrical conductivity. They are suitable for use in integrating, calibrating and testing permafrost as a component in Earth System Models. The resulting quality-controlled dataset is unique in the Arctic and serves as a baseline for future studies.
DOI: 10.1594/pangaea.825430
title: (Table 2) Grain size distribution of surface sediments taken in the Gulf of Taranto

description: Columns e-f-g are subdivisions of the silt fraction (column c), whereas columns h and i represent most of the sand fraction.
DOI: 10.1594/pangaea.936272
title: Meteorological observations at Bayelva Station in 2020 (level 1)

description: Understanding permafrost processes and changes requires long-term observational datasets. This dataset is a continuation of the dataset available from the Bayelva Site at Ny-Ålesund, Svalbard, where meteorology, energy balance components and subsurface observations have been made for more than the last 20 years. The data provide observations of temporally variable parameters that mitigate energy fluxes between permafrost and atmosphere, such as snow depth, snow dielectric number, snow temperature, liquid precipitation, air temperature, relative humidity, wind speed and direction and radiation fluxes. They are suitable for use in integrating, calibrating and testing permafrost as a component in Earth System Models. The resulting quality-controlled dataset is unique in the Arctic and serves as a baseline for future studies.
description: This dataset of 2020 is a continuation of a data record, which was published in Boike et al. (2018), doi:10.5194/essd-10-355-2018. If you use this dataset, please cite this publication.
DOI: 10.1594/pangaea.880100
title: Soil temperature and volumetric soil moisture at Bayelva Station in 2008 (level 2)
DOI: 10.1594/pangaea.949924
title: Basic measurements of radiation at station Abashiri (2022-07)
DOI: 10.1594/pangaea.880073
title: Snow height at Bayelva Station in 2002 (level 2)
DOI: 10.1594/pangaea.881824
title: Meteorological observations at Bayelva Station in 2007 (level 1)
DOI: 10.1594/pangaea.946201
title: Basic measurements of radiation at station Abashiri (2022-04)
DOI: 10.1594/pangaea.949082
title: Basic measurements of radiation at station Abashiri (2022-05)
DOI: 10.1594/pangaea.942867
title: Basic measurements of radiation at station Abashiri (2022-01)
DOI: 10.1594/pangaea.949086
title: Basic measurements of radiation at station Abashiri (2022-06)
DOI: 10.1594/pangaea.960178
title: Basic measurements of radiation at station Abashiri (2023-02)
DOI: 10.1594/pangaea.960242
title: Basic measurements of radiation at station Abashiri (2023-04)
DOI: 10.1594/pangaea.960244
title: Basic measurements of radiation at station Abashiri (2023-03)
DOI: 10.1594/pangaea.961520
title: Basic measurements of radiation at station Abashiri (2023-05)
DOI: 10.1594/pangaea.947034
title: Soil data at station Samoylov (2019)

description: Understanding permafrost processes and changes requires long-term observational datasets. This dataset is a continuation of the dataset available from the long-term observational site Samoylov, located in the Lena River Delta, Siberia (72.37°N, 126.48°E). The location is characterized by a cold, dry tundra climate with mean annual air temperature of -11.7°C (using years with complete data between 1998 and 2017). The monthly mean temperatures over this period varied between 9.4°C in the warmest month (July) and -31.7°C in the coldest month (February). The average summer rainfall (June-October) was 145.2 mm. This dataset adds recent years to the observations of meteorological parameters, energy balance, and subsurface observations which have been recorded since 1998. The instrumentation, calibration, processing and data quality control is explained in Boike et al. (2019). The data provide observations of temporally variable parameters that mitigate energy fluxes between permafrost and atmosphere, such as ground heat flux, active layer and permafrost temperature, soil volumetric water content, relative permittivity, and soil bulk electrical conductivity. Those variables were measured at various depths and beneath different microtopographic features (a polygon center, a rim, a slope, and a trough), representing landscape heterogeneity. The observations are suitable for use in integrating, calibrating and testing permafrost as a component in Earth System Models. The resulting quality-controlled dataset is unique in the Arctic and serves as a baseline for future studies.
DOI: 10.1594/pangaea.961672
title: Meteorological observations at Bayelva Station in 2022 (level 1)

description: Understanding permafrost processes and changes requires long-term observational datasets. This dataset is a continuation of the dataset available from the Bayelva Site at Ny-Ålesund, Svalbard, where meteorology, energy balance components and subsurface observations have been made for more than the last 20 years. The data provide observations of temporally variable parameters that mitigate energy fluxes between permafrost and atmosphere, such as snow depth, snow dielectric number, snow temperature, liquid precipitation, air temperature, relative humidity, wind speed and direction and radiation fluxes. They are suitable for use in integrating, calibrating and testing permafrost as a component in Earth System Models. The resulting quality-controlled dataset is unique in the Arctic and serves as a baseline for future studies.
description: This dataset of 2022 is a continuation of a data record, which was published in Boike et al. (2018), doi:10.5194/essd-10-355-2018. If you use this dataset, please cite this publication.
DOI: 10.1594/pangaea.898683
title: Meteorological observations at Bayelva Station in 2018 (level 1)

description: ** PLEASE NOTE ** On 2020-10-07 it was detected that two parameters were wrongly assigned. Parameter no. 28 was therefore changed from "Snow height" to "Permittivity, relative" and parameter no. 30 from "Permittivity, relative" to "Temperature, air" (at 5 cm)
DOI: 10.1594/pangaea.962024
title: Basic measurements of radiation at station Abashiri (2023-06)
DOI: 10.1594/pangaea.825342
title: (Figure 6) Selected elemental ratios from X-ray fluorescence (XRF) core scanning of sediment core DP30PC
DOI: 10.1594/pangaea.961673
title: Soil data at station Bayelva (2022, level 1)

description: Understanding permafrost processes and changes requires long-term observational datasets. This dataset is a continuation of the dataset available from the Bayelva Site at Ny-Ålesund, Svalbard, where meteorology, energy balance components and subsurface observations have been made for more than the last 20 years. The data provide observations of temporally variable parameters that mitigate energy fluxes between permafrost and the atmosphere, such as active layer and permafrost temperature, soil volumetric water content and soil bulk electrical conductivity. They are suitable for use in integrating, calibrating and testing permafrost as a component in Earth System Models. The resulting quality-controlled dataset is unique in the Arctic and serves as a baseline for future studies.
description: This dataset of 2022 is a continuation of a data record, which was published in Boike et al. (2018), doi:10.5194/essd-10-355-2018. If you use this dataset, please cite this publication.
DOI: 10.1594/pangaea.806208
title: Soil temperature measured on Samoylov Island, 2006-2011
DOI: 10.1594/pangaea.882058
title: Meteorologic data at station Bayelva (1998-2017, level 1, version 1), link to archive
DOI: 10.1594/pangaea.891139
title: Meteorologic data at station Samoylov (2002-2018, level 2, version 1), link to archive

description: WRONG DATA!Meteorologic data at station Samoylov (2002-2018, level 1 & level 2, version 1) are with wrong precipitation data during the period 2009–2018.PLEASE USE NEW VERSION!Precipitation was doubled during the period 2009–2018 due to incorrect application of the multiplication factor. This was due to a change in the precipitation gauge setup due to a complete destruction of the gauge sometime in autumn 2009. The broken Environmental Measurements ARG100 gauge was exchanged to an R. M. Young Company 52203 tipping bucket gauge on 26 July 2010. The required adaption of the multiplication factor (i.e. from 0.2 to 0.1) was not performed for the final calculation of the precipitation data.
DOI: 10.1594/pangaea.891138
title: Meteorologic data at station Samoylov (2002-2018, level 1, version 1), link to archive

description: WRONG DATA!Meteorologic data at station Samoylov (2002-2018, level 1 & level 2, version 1) are with wrong Precipitation data during the period 2009–2018.PLEASE USE NEW VERSION!Precipitation was doubled during the period 2009–2018 due to incorrect application of the multiplication factor. This was due to a change in the precipitation gauge setup due to a complete destruction of the gauge sometime in autumn 2009. The broken Environmental Measurements ARG100 gauge was exchanged to an R. M. Young Company 52203 tipping bucket gauge on 26 July 2010. The required adaption of the multiplication factor (i.e. from 0.2 to 0.1) was not performed for the final calculation of the precipitation data.
DOI: 10.1594/pangaea.905230
title: Meteorologic data at station Samoylov (2002-2018, level 1, version 201908), link to archive

description: *** Attention: The precipitation (Prec) value at 2017-06-12 9:30 (25.2mm) is incorrect and must be flagged (Prec_fl = 6).--This is an updated version of this data: https://doi.pangaea.de/10.1594/PANGAEA.891138, please use and cite the updated version!
DOI: 10.1594/pangaea.882059
title: Meteorologic data at station Bayelva (1998-2017, level 2, version 1), link to archive
DOI: 10.1594/pangaea.898685
title: Soil data at station Bayelva (2018, level 1)
DOI: 10.1594/pangaea.806207
title: Soil temperature from a borehole on Samoylov Island, 2006-2011
DOI: 10.1594/pangaea.905229
title: Calm data at station Samoylov (2002-2018, level 1, version 201908), link to archive

description: This is an updated version of this data: https://doi.pangaea.de/10.1594/PANGAEA.892372, please use and cite the updated version!
DOI: 10.1594/pangaea.825421
title: (Figure 4) Age and Calcium/Titanium ratio of sediment core GeoB10745-3
DOI: 10.1594/pangaea.880084
title: Snow height at Bayelva Station in 2013 (level 2)
DOI: 10.1594/pangaea.881816
title: Meteorological observations at Bayelva Station in 1999 (level 1)
DOI: 10.1594/pangaea.881833
title: Meteorological observations at Bayelva Station in 2016 (level 1)
DOI: 10.1594/pangaea.880093
title: Soil temperature and volumetric soil moisture at Bayelva Station in 2002 (level 2)
DOI: 10.1594/pangaea.881826
title: Meteorological observations at Bayelva Station in 2009 (level 1)
DOI: 10.1594/pangaea.825343
title: (Figure 6) Selected elemental ratios from X-ray fluorescence (XRF) core scanning of sediment core GeoB10704-5
DOI: 10.1594/pangaea.880080
title: Snow height at Bayelva Station in 2009 (level 2)
DOI: 10.1594/pangaea.880098
title: Soil temperature and volumetric soil moisture at Bayelva Station in 2006 (level 2)
DOI: 10.1594/pangaea.825413
title: (Figure 4 and 5) Age and Calcium/Titanium ratio of sediment core DP30PC
DOI: 10.1594/pangaea.825417
title: (Figure 4) Age and Calcium/Titanium ratio of sediment core GeoB10706-4
DOI: 10.1594/pangaea.846518
title: (Figure 3) Air temperature, humiditiy, wind speed, and radiation measured at the Samoylov climate station, 2009-07 to 2011-08
DOI: 10.1594/pangaea.879341
title: Hourly meteorology and snow height at Samoylov met-station (2012-08-01 - 2013-06-30)

description: The Arctic Samoylov site is extensively described in Boike et al. (2013) and more shortly in Gouttevin et al. (2017) where the present dataset is exploited.Air temperature and relative humidity were obtained from the Samoylov met-station using an HMP45A air temperature and humidity sensor . Unfortunately the sensor became saturated at temperatures below -40 °C From 2013-02-01 to 2013-03-15 air temperatures dropped below -40°C, and TTT in the dataset is replaced by the 2 m air temperature from the ERA-interim (ERA-i) reanalysis Project (Dee et al., 2011). The ERA-i data were linearly interpolated from their native 3 hourly temporal resolution (analysis and forecast fields) to a 30 min time-series. This substitution seems appropriate since for the rest of the 2012-2013 winter period, ERA-i temperatures show a high correlation with Samoylov observations (r2=0.97) and a low bias (-0.9°C). ERA-i fields were also proven to be a high quality source of driving variables to simulate the evolution of the Northern Eurasian snowpack including Siberia (Brun et al., 2013), with minor differences between station data and grid-field over large, rather flat areas like the Lena Delta. Finally, a comparison of ERA-i with locally acquired meteorological data from earlier years at Samoylov confirmed this validity for the skin surface temperature, which responds very sensitively to differences in the driving variables (Langer et al., 2013). Incoming shortwave and longwave radiation were measured at the Samoylov meteorological station with an NR01 Hukseflux 4-Component Net Radiation Sensor. Wind speed was measured at 3 m above ground with a 05103 Young Wind Monitor. Wind speed was (together with air temperature) the only meteorological field for which likely instrumental failure was detected, characterized by periods of a few hours to a few days with null wind-speed. These likely failures were not corrected for in the present dataset.Snow height was continuously recorded by an SR50 sensor (Campbell Scientific, ±1 cm accuracy, ±1 cm precision) located in the Samoylov reference polygon, in the topographically lower center (see Gouttevin et al., 2017 for details). For the "snow h" field provided here, the SR50 raw data was treated by a applying a moving average filter with a window size of 72 hours, thus removing spikes partly due to blowing snow events. Note this "snow h" field does not include the correcting factor used by Gouttevin et al., 2017. Raw SR50 data can be provided on request.
DOI: 10.1594/pangaea.806203
title: Meteorological measurements on Samoylov Island, 2002-2011
DOI: 10.1594/pangaea.806204
title: Radiation on Samoylov Island, 2009-2011
DOI: 10.1594/pangaea.806205
title: Wind speed on Samoylov Island, 2002-2011
DOI: 10.1594/pangaea.806212
title: Meteorological measurements on Samoylov Island, 1998-2002
DOI: 10.1594/pangaea.806213
title: Wind speed on Samoylov Island, 1998-2002
DOI: 10.1594/pangaea.806214
title: Soil temperature measured on Samoylov Island, 1998-2002
DOI: 10.1594/pangaea.880069
title: Snow height at Bayelva Station in 1998 (level 2)
DOI: 10.1594/pangaea.880070
title: Snow height at Bayelva Station in 1999 (level 2)
DOI: 10.1594/pangaea.880071
title: Snow height at Bayelva Station in 2000 (level 2)
DOI: 10.1594/pangaea.880072
title: Snow height at Bayelva Station in 2001 (level 2)
DOI: 10.1594/pangaea.880075
title: Snow height at Bayelva Station in 2004 (level 2)
DOI: 10.1594/pangaea.880076
title: Snow height at Bayelva Station in 2005 (level 2)
DOI: 10.1594/pangaea.882061
title: Soil data at station Bayelva (1998-2017, level 2, version 1), link to archive
DOI: 10.1594/pangaea.881819
title: Meteorological observations at Bayelva Station in 2002 (level 1)
DOI: 10.1594/pangaea.881822
title: Meteorological observations at Bayelva Station in 2005 (level 1)
DOI: 10.1594/pangaea.881828
title: Meteorological observations at Bayelva Station in 2011 (level 1)
DOI: 10.1594/pangaea.881834
title: Meteorological observations at Bayelva Station in 2017 (level 1)
DOI: 10.1594/pangaea.880081
title: Snow height at Bayelva Station in 2010 (level 2)
DOI: 10.1594/pangaea.880082
title: Snow height at Bayelva Station in 2011 (level 2)
DOI: 10.1594/pangaea.880083
title: Snow height at Bayelva Station in 2012 (level 2)
DOI: 10.1594/pangaea.880088
title: Snow height at Bayelva Station in 2017 (level 2)
DOI: 10.1594/pangaea.880091
title: Soil temperature and volumetric soil moisture at Bayelva Station in 2000 (level 2)
DOI: 10.1594/pangaea.880095
title: Soil temperature and volumetric soil moisture at Bayelva Station in 2004 (level 2)
DOI: 10.1594/pangaea.880097
title: Soil temperature and volumetric soil moisture at Bayelva Station in 2005 (level 2)
DOI: 10.1594/pangaea.880103
title: Soil temperature and volumetric soil moisture at Bayelva Station in 2011 (level 2)
DOI: 10.15468/dl.wtwptq
title: Occurrence Download

description: A dataset containing 622451 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is one of (Acer platanoides L.)",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "OccurrenceStatus is Present"
 ]
}

 The dataset includes 622451 records from 1770 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0000224-250225214225278/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.5517/cc137r69
title: CCDC 1020340: Experimental Crystal Structure Determination

description: Related Article: Andrea Cappelli,  Chiara Nannicini,  Andrea Gallelli,  Germano Giuliani,  Salvatore Valenti,  Gal.la Pericot Mohr,  Maurizio Anzini,  Laura Mennuni,  Flora Ferrari,  GianfrancoCaselli,  Antonio Giordani,  Walter Peris,  Francesco Makovec,  Gianluca Giorgi and Salvatore Vomero|2008|J.Med.Chem.|51|2137|doi:10.1021/jm7011563
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.