cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.326900
title: Helicopter-borne sea ice thickness measurements during campaign IRIS2004 from flight IRIS2004_21
DOI: 10.1594/pangaea.326905
title: Helicopter-borne sea ice thickness measurements during campaign IRIS2004 from flight IRIS2004_26
DOI: 10.1594/pangaea.326908
title: Helicopter-borne sea ice thickness measurements during campaign IRIS2004 from flight IRIS2004_29
DOI: 10.1594/pangaea.326911
title: Helicopter-borne sea ice thickness measurements during campaign IRIS2004 from flight IRIS2004_32
DOI: 10.1594/pangaea.326912
title: Helicopter-borne sea ice thickness measurements during campaign IRIS2004 from flight IRIS2004_33
DOI: 10.1594/pangaea.326914
title: Helicopter-borne sea ice thickness measurements during campaign IRIS2004 from flight IRIS2004_35
DOI: 10.1594/pangaea.326916
title: Helicopter-borne sea ice thickness measurements during campaign IRIS2004 from flight IRIS2004_37
DOI: 10.1594/pangaea.326957
title: Helicopter-borne sea ice thickness measurements during campaign IRIS2004 from flight IRIS2004_78
DOI: 10.1594/pangaea.326958
title: Helicopter-borne sea ice thickness measurements during campaign IRIS2004 from flight IRIS2004_79
DOI: 10.1594/pangaea.326959
title: Helicopter-borne sea ice thickness measurements during campaign IRIS2004 from flight IRIS2004_80
DOI: 10.1594/pangaea.706309
title: (Table 1) Age, magnetic susceptibility, and mass accumulation rate of volcanic glass and IRD from ODP Site 145-887

description: Depth is common depth (m)
DOI: 10.1594/pangaea.717708
title: Abundance of macrozoobenthos in surface sediments sampled during POLARSTERN cruise ANT-V/1

description: Depth = penetration depth of gear (max = 45 cm).
DOI: 10.1594/pangaea.742746
title: Physical oceanography during ODEN cruise OD91
DOI: 10.1594/pangaea.778265
title: Helicopter-borne sea ice thickness measurements during the POL-ICE field campaign in the Bay of Bothnia in March 2007 from flight HEM_POL-ICE07_01c
DOI: 10.1594/pangaea.778269
title: Helicopter-borne sea ice thickness measurements during the POL-ICE field campaign in the Bay of Bothnia in March 2007 from flight HEM_POL-ICE07_04
DOI: 10.1594/pangaea.784100
title: Helicopter-borne sea ice thickness measurements during ARANDA campaign IRIS 2005 from flight HEM_IRIS05_01
DOI: 10.1594/pangaea.784105
title: Helicopter-borne sea ice thickness measurements during ARANDA campaign IRIS 2005 from flight HEM_IRIS05_05a
DOI: 10.1594/pangaea.784166
title: Helicopter-borne sea ice thickness measurements during campaign IRIS 2003 from flight HEM_IRIS03_07
DOI: 10.1594/pangaea.784169
title: Helicopter-borne sea ice thickness measurements during campaign IRIS 2003 from flight HEM_IRIS03_10
DOI: 10.1594/pangaea.834041
title: Abundance of macrozoobenthos in surface sediments sampled during POLARSTERN cruise ANT-XV/3

description: Depth = penetration depth of gear (max = 45 cm).
DOI: 10.1594/pangaea.834053
title: Abundance of macrozoobenthos in surface sediments sampled during POLARSTERN cruise ANT-XXIII/8

description: Depth = penetration depth of gear (max = 45 cm).
DOI: 10.1594/pangaea.834057
title: Abundance of macrozoobenthos in surface sediments sampled during POLARSTERN cruise ANT-XXVII/3

description: Depth = penetration depth of gear (max = 45 cm).
DOI: 10.1594/pangaea.834069
title: Abundance of macrozoobenthos in surface sediments sampled during POLARSTERN cruise ANT-XIX/5

description: Depth = penetration depth of gear (max = 45 cm).
DOI: 10.1594/pangaea.898689
title: Hydrothermal cleft monazite SIMS Th-Pb age data, central Alps

description: Ion probe (SIMS) Th-Pb age measurements of hydrothermal fissure/cleft monazite from the central Alps. The sample area encompasses most of the Lepontine metamorphic dome, the eastern Rhone-Simplon Line, southern Gotthard Nappe and the Forcola Fault.The ages directly date deformation during part of the exhumation and cooling history of the Lepontine dome and deformation along the Rhone-Simplon fault zone. The ages of all crystals range from ca. 19 to 5 Ma, with age distribution and internal crystal structure facilitating to distinguish between areas whose deformational history was dominated by distinct tectonic events or continuous exhumation.
description: (1) The measurement of ²⁰⁴Pb is subject to an unresolvable molecular interference by ²³²Th¹⁴³Nd¹⁶O₂, which may result in an overestimation of common Pb concentrations. A correction was applied whenever the ²³²Th¹⁴³Nd¹⁶O₂ signal at mass 203.5 exceeded the average background signal on the ion-counting detector by three times its standard deviation.(2) The f208 value is the percentage of unradiogenic/common lead ²⁰⁸Pb of the measurement's total ²⁰⁸Pb.
description: Supplement to: Bergemann, Christian A; Gnos, Edwin; Berger, Alfons; Janots, Emilie; Whitehouse, Martin J (2020): Dating tectonic activity in the Lepontine Dome and Rhone-Simplon Fault regions through hydrothermal monazite-(Ce). Solid Earth, 11(1), 199-222
DOI: 10.1594/pangaea.905442
title: Radionuclide data (total 210Pb) measured on sediment multi cores during SONNE cruise SO242/1 at the DISCOL area, Peru Basin

description: Sediment profiles of 210Pb and 226Ra, radio-isotopes from the 234U decay series with half-lives of respectively 22.3 and 1600 year, were measured in multicores collected from the DISCOL Experimental Area in the Peru Basin during SO242-1, for determining biological mixing rates integrated over a ~100 year time-scale. Total 210Pb and 226Ra activity were determined directly by gamma-spectrometry, whilst total 210Pb was also measured indirectly by alpha-spectrometry via its granddaughter isotope 210Po. Activities of anthropogenic 137Cs proved to be generally below detection level. Radionuclide activities are reported in the data base as mBq g-1 dry sediment.For alpha spectrometry measurement of 210Po, 0.5 g of freeze-dried and homogenised sediment contained in a plastic reaction tube was spiked with 1 ml of a standard solution of 209Po in 2M HCl, and then leached for 6 h in 10 ml of concentrated HCl heated to 85ºC. After diluting the fluid with 45 ml of demineralised water and adding 5 ml of an aqueous solution of ascorbic acid (40 g L-1), natural 210Po and added 209Po were collected from the fluid by spontaneous electrochemical deposition on silver plates, which were suspended in the fluid for at least 16 h while the fluid was heated to 70ºC. The Po isotopes collected on the silver plates were then measured by alpha-spectrometry using Canberra Passivated Implanted Planar Silicon detectors, with a count time of 1 day sufficient to reduce counting error to &lt; 3%. 210Pb activity was calculated from 210Po, assuming secular equilibrium and correcting for the time elapsed since collection of the samples.
DOI: 10.1594/pangaea.911966
title: Fish abundances and masses from trawl samples taken in the wider Weddell Sea (Antarctica) during POLARSTERN cruises ANT-XV/3
DOI: 10.1594/pangaea.911970
title: Fish abundances and masses from trawl samples taken in the wider Weddell Sea (Antarctica) during POLARSTERN cruise ANT-XXVII/3
DOI: 10.17882/58728
title: Trieste 1899-2015 near-surface sea temperature

description: The data set includes daily near-surface sea temperatures measured in the harbour of Trieste (Italy) during 1899-2015. Two time series are formed: the first is derived from analogue measurements performed in the 1899-2008 period, the second is derived from digital records in 1986-2015. From these time series a composite time series for 1899-2015 is built. Data records consist of date and daily temperature in degrees Celsius to the 0.1 °C precision.
DOI: 10.18140/flx/1440216
title: FLUXNET2015 DE-RuS Selhausen Juelich

description: This is the FLUXNET2015 version of the carbon flux data for the site DE-RuS Selhausen Juelich.
DOI: 10.18140/flx/1440219
title: FLUXNET2015 DE-SfN Schechenfilz Nord

description: This is the FLUXNET2015 version of the carbon flux data for the site DE-SfN Schechenfilz Nord.
DOI: 10.25675/10217/201142
title: Data associated with "Convective distribution of dust over the Arabian Peninsula: the impact of model resolution"

description: These data represent the model namelists used to generate simulations using the Weather Research and Forecasting Model Coupled to Atmospheric Chemistry (WRF-Chem) version 3.9.1.
description: Along the coasts of the Arabian Peninsula, convective dust storms are a considerable source of mineral dust to the atmosphere. Reliable predictions of convective dust events are necessary to determine their effects on air quality, visibility, and the radiation budget. In this study, the Weather Research and Forecasting Model coupled with Chemistry (WRF-Chem) is used to simulate a 2016 summertime dust event over the Arabian Peninsula and examine the variability in dust fields and associated vertical transport due to the choice of convective parameterization and explicit versus parameterized convection. Simulations are run at 45 km and 15 km grid spacing with multiple cumulus parameterizations, and are compared to a 3 km simulation that permits explicit convective processes. Five separate cumulus parameterizations at 15 km grid spacing were tested to quantify the spread across different parameterizations. Finally, the impact these variations have on radiation, specifically aerosol heating rates is also investigated. On average, in these simulations the explicit case produces higher quantities of dust than the parameterized cases in terms of dust uplift potential, vertical dust concentrations, and vertical dust fluxes. Major drivers of this discrepancy between the simulations stem from the explicit case exhibiting higher surface windspeeds during convective activity, lower dust emission wind threshold velocities due to drier soil, and more frequent, stronger vertical velocities which transport dust aloft and increase the atmospheric lifetime of these particles. For aerosol heating rates in the lowest levels, the shortwave effect prevails in the explicit case with a net cooling effect, whereas a longwave net warming effect is present in the parameterized cases. The spread in dust concentrations across cumulus parameterizations at the same grid resolution (15 km) is an order of magnitude lower than the impact of moving from parameterized to explicit convection. We conclude that tuning dust emissions in coarse resolution simulations can only improve the results to first-order and cannot fully rectify the discrepancies originating from disparities in the representation of convective dust transport.
DOI: 10.5067/8jknew6bfrvd
title: Radarsat Antarctic Mapping Project Digital Elevation Model, Version 2
DOI: 10.5067/modis/myd08_d3.061
title: MYD08_D3 MODIS/Aqua Aerosol Cloud Water Vapor Ozone Daily L3 Global 1Deg CMG
DOI: 10.5281/zenodo.1403171
title: AgMIP's Global Gridded Crop Model Intercomparison (GGCMI) phase 1 output data set: pDSSAT wheat

description: This is model output from pDSSAT for wheat as part of AgMIP's Global Gridded Crop Model Intercomparison (GGCMI) phase 1 output data set.

The data have been generated following the modeling protocol of Elliott et al. (2015) and has been used to evaluate the models (Müller et al., 2017). A data description paper has been published in Scientific Data (Müller et al. 2019).

References:

Elliott J, Müller C, Deryng D, Chryssanthacopoulos J, Boote KJ, Büchner M, Foster I, Glotter M, Heinke J, Iizumi T, Izaurralde RC, Mueller ND, Ray DK, Rosenzweig C, Ruane AC, and Sheffield J. 2015, The Global Gridded Crop Model intercomparison: data and modeling protocols for Phase 1 (v1.0). Geosci. Model Dev. 8, 261-277, doi:10.5194/gmd-8-261-2015

Müller C, Elliott J, Chryssanthacopoulos J, Arneth A, Balkovic J, Ciais P, Deryng D, Folberth C, Glotter M, Hoek S, Iizumi T, Izaurralde RC, Jones C, Khabarov N, Lawrence P, Liu W, Olin S, Pugh TAM, Ray DK, Reddy A, Rosenzweig C, Ruane AC, Sakurai G, Schmid E, Skalsky R, Song CX, Wang X, de Wit A, and Yang H. 2017, Global gridded crop model evaluation: benchmarking, skills, deficiencies and implications, Geosci. Model Dev., 10, 1403-1422, doi: 10.5194/gmd-10-1403-2017

Müller C, Elliott J, Kelly D, Arneth A, Balkovic J, Ciais P, Deryng D, Folberth C, Hoek S, Izaurralde RC, Jones CD, Khabarov N, Lawrence P, Liu W, Olin S, Pugh TAM, Reddy A, Rosenzweig C, Ruane AC, Sakurai G, Schmid E, Skalsky R, Wang X, de Wit A, and Yang H. 2019, The Global Gridded Crop Model Intercomparison phase 1 simulation dataset, Scientific Data, 6, 50, doi: 10.1038/s41597-019-0023-8
DOI: 10.5281/zenodo.3375325
title: Simulation output of Lirung glacier

description: This is the data used for <strong><em>Using 3D turbulence-resolving simulations to understand the impact of surface properties on the energy balance of a debris-covered glacier, </em></strong>by PNJ Bonekamp, CC van Heerwaarden, JF Steiner and WW Immerzeel<br> <br> For each experiment one summary file is present. Description of experiments:<br> HOM<sub>flat</sub> Homogeneous glacier (constant DEM, surface specific moisture and temperature)<br> HOM<sub>1/2DEM</sub> ½ DEM, homogeneous surface specific moisture and temperature<br> HOM<sub>DEM </sub> With the real DEM, homogeneous surface specific moisture and temperature<br> HET<sub>T</sub> Spatially heterogeneous surface temperature, the real DEM, homogeneous surface specific moisture<br> HET<sub>qdry</sub> Surface specific humidity is spatially RH=70-75%, surface temperature constant, real DEM is included<br> HET<sub>qmoist</sub> Spatially RH=70-85%, surface temperature constant, real DEM is included<br> <br> In each file various variables are present;<br> u_xz, v_xz, qt_xz, thl_xz: which are the wind vectors, total specific humidity and liquid potential temperature for the xz cross section respectively<br> u_yz, v_yz, qt_yz, thl_yz: which are the wind vectors, total specific humidity and liquid potential temperature for the yz cross section respectively<br> qtfluxbot_ib, thlfluxbot_ib: the total specific moisture and temperature flux at the surface respectively. See for more specific information:<br> <strong><em>Using 3D turbulence-resolving simulations to understand the impact of surface properties on the energy balance of a debris-covered glacier, </em></strong>PNJ Bonekamp, CC van Heerwaarden, JF Steinerand WW Immerzeel, The Cryosphere, submitted
DOI: 10.5281/zenodo.3375490
title: Simulation output of Lirung glacier (REAL EXP)

description: This is the data used for <strong><em>Using 3D turbulence-resolving simulations to understand the impact of surface properties on the energy balance of a debris-covered glacier, </em></strong>by PNJ Bonekamp, CC van Heerwaarden, JF Steiner and WW Immerzeel. In this netcdf file only the data of the REAL experiment can be found. See for data of the other experiments 10.5281/zenodo.3375325. <br> <br> These variables are present;<br> u_xz, v_xz, qt_xz, thl_xz: which are the wind vectors, total specific humidity and liquid potential temperature for the xz cross section respectively<br> u_yz, v_yz, qt_yz, thl_yz: which are the wind vectors, total specific humidity and liquid potential temperature for the yz cross section respectively<br> qtfluxbot_ib, thlfluxbot_ib: the total specific moisture and temperature flux at the surface respectively. See for more specific information:<br> <strong><em>Using 3D turbulence-resolving simulations to understand the impact of surface properties on the energy balance of a debris-covered glacier, </em></strong>PNJ Bonekamp, CC van Heerwaarden, JF Steiner and WW Immerzeel, The Cryosphere, submitted
DOI: 10.5281/zenodo.3600486
title: Pyruvic acid Dataset. IBAIRN campaign

description: Data used in the manuscript by <strong>Eger et al: </strong> <strong>Pyruvic acid in the boreal forest: first measurements and impact on radical chemistry</strong> In Atmospheric Chemistry and Physics Discussions. https://doi.org/10.5194/acp-2019-768
DOI: 10.5281/zenodo.3667507
title: Raw stable water isotope measurements in water vapour at 8 m a.s.l. on the port side of the ship, made in the austral summer of 2016/2017 during the Antarctic Circumnavigation Expedition (ACE).

description: <strong>Dataset abstract</strong> This dataset includes the raw data of stable water vapour isotope (δ18O, δ2H, deuterium excess) and water vapour mixing ratio measurements at a height of approximately 8 meters above sea level taken in the Southern Ocean during the Antarctic Circumnavigation Expedition (ACE) from November 2016 to April 2017 using a Picarro laser spectrometer L2120 mounted on the port side of the ship. The spectrometer was operated throughout the whole expedition. This data has to be calibrated using the calibration runs and applying an appropriate calibration procedure following the IAEA guide lines. Two similar datasets also measuring stable water isotopes (SWIs) in water vapour were collected during the same expedition and can be distinguished from this dataset due to the height of the measurement collection (at 8 m a.s.l and 13.5 m a.s.l). The three ACE datasets of SWIs in water vapour are described and compared in Thurnherr et al. (2020). <strong>Dataset contents</strong> leg*/HBDS2190-yyyymmdd-hhmmssZ-DataLog_User.dat, data file, comma-separated values data_file_header.txt, metadata, text format README.txt, metadata, text format <strong>Dataset license</strong> This raw stable water isotope measurements dataset is made available under the Creative Commons Attribution 4.0 International License (CC BY 4.0) whose full description can be found at https://creativecommons.org/licenses/by/4.0/ <strong>Dataset citation</strong> Please cite this dataset as:<br> Kozachek, A. (2020). Raw stable water isotope measurements in water vapour at 8 m a.s.l. on the port side of the ship, made in the austral summer of 2016/2017 during the Antarctic Circumnavigation Expedition (ACE). (Version 1.0) [Data set]. Zenodo.
description: The Antarctic Circumnavigation Expedition was made possible by funding from the Swiss Polar Institute and Ferring Pharmaceuticals.
description: {"references": ["Thurnherr, I., Kozachek, A., Graf, P., Weng, Y., Bolshiyanov, D., Landwehr, S. J., Pfahl, S., Schmale, J., Sodemann, H., Steen-Larsen, H. C., Toffoli, A., Wernli, H. and Aemisegger, F.: Meridional and vertical variations of the marine boundary layer water vapour isotope composition in the Atlantic and the Southern Ocean. Accepted (2020). Atmospheric Chemistry and Physics.", "IAEA: Reference Sheet for VSMOW2 and SLAP2 international measurement standards, International Atomic Energy Agency (IAEA), 2009", "David W H Walton, & Jenny Thomas. (2018, November 22). Cruise Report - Antarctic Circumnavigation Expedition (ACE) 20th December 2016 - 19th March 2017 (Version 1.0). Zenodo. http://doi.org/10.5281/zenodo.1443511"]}
DOI: 10.5281/zenodo.3720444
title: National Severe Storms Laboratory Mobile Soundings during Lapse-Rate (CLAMPS trailer)

description: This dataset includes files from the National Severe Storms Laboraory mobile sounding units operated during the LAPSE-RATE field campaign. The files contained here are for each individual sounding launched from the CLAMPS trailer owned and operated by the University of Oklahoma, along with a readme file explaining the data format and processing.
DOI: 10.5281/zenodo.55156
title: Error

description: ..
DOI: 10.5285/9c972cfb-0ffa-4144-a943-da6eb82431d2
title: Ice core chemistry, density, conductivity, dust, snow accumulation rate, and stable nitrate isotopic composition of the 120 m ISOL-ICE ice core, Dronning Maud Land, Antarctica

description: This dataset contains ice core data for the ISOL-ICE core recovered from Dronning Maud Land, Antarctica in January 2017. The core is 120 m in depth and spans a 1349 +/- 3 year period from 2017 to 668 AD. The core was dated by annual layer counting and identifying volcanic horizons as fixed time markers. High-resolution stable nitrate isotopic composition data is accompanied by chemistry data, conductivity, density, insoluble particle counts (dust), and snow accumulation rate data. Funding was provided by the NERC grant NE/N011813/1.
description: See related document (https://ramadda.data.bas.ac.uk/repository/entry/get/methodology.pdf?entryid=synth%3A9c972cfb-0ffa-4144-a943-da6eb82431d2%3AL21ldGFkYXRhL21ldGhvZG9sb2d5LnBkZg%3D%3D)
description: Fast ion chromatography: ICS-3000, Dionex™ with a CERS 4mm suppressor. Isotope ratio mass spectrometer (IRMS) for duel O and N analysis: Thermo Finnigan™ MAT 253 IRMS equipped with a GasBench II™ and coupled to an in-house-built NO3- interface. Inductively coupled plasma-mass spectrometry: 7700 series, Agilent. Abakus: Fa, Klotz, Bad Liebenzell, Germany. Conductivity: Dionex™ conductivity detector.
description: Major ions: At the beginning, end and during the course of the day, a certified reference material (CRM; ERM-CA408 simulated rainwater standards; Sigma-Aldrich) was measured for quality control and yielded an accuracy of 107 %, and precision of 10 % for nitrate. Major elements: At the beginning, end and during the course of the day, a certified reference material (CRM; ERM-CA408 simulated rainwater standards; Sigma-Aldrich) was measured for quality control and yielded an accuracy of 94 and 113 %, and precision of 10 and 13 % for sodium and magnesium. Nitrate stable isotope ratios: Certified reference materials (IAEA USGS-32, USGS-34 and USGS-35; Böhlke et al., 1993; Böhlke et al., 2003) were prepared (matrix match 1 M NaCl solution; ACS grade) and subject to the same analytical procedures as snow and aerosol samples. For each batch of 60 samples, the overall accuracy of the method is estimated as the reduced standard deviation of the residuals from the linear regression between the measured reference materials (n = 16) and their expected values. For the ice core (n = 800), the average uncertainty values obtained for δ18O, δ17O, Δ17O and δ15N were 2.8 ‰, 2.1 ‰ 0.9 ‰ and 2.9 ‰ respectively.
DOI: 10.60598/fue.fs.2021
title: Daten zu Forschungs- und Entwicklungsaktivitäten in Deutschland auf Ebene der Forschungsstätten
DOI: 10.6084/m9.figshare.12758387.v1
title: Litter.xlsx and soil.xlsx

description: Litter.xlsx include the data of litter mass, litter decay rate and the release dynamiacs. soil.xlsx include the data of soil Microbial data and the SOC, DOC, MBC, and the contribution of litter to soil.
DOI: 10.6096/parcs.17
title: Meteorological data Kongsvegen AWS

description: Automatic measurements of meteorological data over the Kongsvegen glacier
DOI: 10.7289/v5sf2tgp
title: NOAA GOES-R Series Advanced Baseline Imager (ABI) Level 2 Clear Sky Mask (ACM)

description: The Clear Sky Mask product contains an image in the form of a binary cloud mask that identifies pixels within a coverage region as clear or cloudy. The production of the clear sky mask is an important step in the processing of many other Advanced Baseline Imager (ABI) Level 2+ products that use the information generated in the production of the clear sky mask to determine the presence of a cloud. The product includes data quality information for the binary cloud mask data values for on-earth pixels. The binary cloud mask value is a dimensionless quantity. The Clear Sky Mask product image is provided at 2 km resolution on the ABI fixed grid for Full Disk, CONUS, and Mesoscale coverage regions from GOES East and West. Product data is produced for geolocated source data to local zenith angles of 90 degrees for both daytime and nighttime conditions.
DOI: 10.1594/pangaea.902611
title: PHIPS particle-by-particle data for the ACLOUD campaign in 2017

description: This dataset contains single particle measurements performed by the PHIPS. It comprises of particle microphysical properties deduced from the stereo imaging as well as angular light scattering measurements. Please see PHIPS-HALO_Data_Readme for more details.
DOI: 10.1594/pangaea.326896
title: Helicopter-borne sea ice thickness measurements during campaign IRIS2004 from flight IRIS2004_17
DOI: 10.5281/zenodo.3228446
title: Data from isotopic measurements for: Hirave et al., 2019

description: Data from isotopic and molecular measurements for: Understanding the effects of early degradation on isotopic tracers: implications for sediment source attribution using compound-specific isotope analysis (CSIA)