cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.5285/bbf12a6f-7d97-4951-9bd1-e4224e2abac9
title: Antarctic daily precipitation amounts for January 1979 - July 2017 from the RACMO version 3p2 limited area atmospheric model, along with flags that indicate extreme precipitation events

description: Two netcdf files are provided that contain daily precipitation amounts for January 1979 - July 2017 from the RACMO version 3p2 limited area, atmosphere-only model. The model is described in van Wessem, J. M., C. H. Reijmer, M. Morlighem, J. Mouginot, E. Rignot, B. Medley, and E. van Meijgaard, (2014) Improved representation of East Antarctic surface mass balance in a regional atmospheric climate model, Journal of Glaciology, 60, 761-770. The model was run over a 262 by 240 grid point domain covering Antarctica and parts of the Southern Ocean. The model was forced at the lateral boundaries by data from the European Centre for Medium-range Weather Forecasting (ECMWF) Interim reanalysis (ERA-Interim). Flags are provided for extreme precipitation events. A precipitation day was taken as a daily total of precipitation of greater than 0.02 mm. Extreme precipitation events were then taken as days when daily precipitation amount was greater than the 90th percentile of the daily precipitation values over the period 1979 - 2016.
DOI: 10.5439/1021460
title: ARM: Balloon-borne sounding system (BBSS): Vaisala-processed winds, press., temp, and RH

description: Balloon-borne sounding system (BBSS): Vaisala-processed winds, press., temp, and RH
DOI: 10.5439/1025306
title: ARM: Total Sky Imager (TSI): cloud decision images, PNG format

description: Total Sky Imager (TSI): cloud decision images, PNG format
DOI: 10.6073/pasta/6744cb28a544fda827805db123d36557
title: A digital archive of human activity in the McMurdo Dry Valleys, Antarctica from 1902 to present

description: Over the last half century, the McMurdo Dry Valleys (MDV) of East Antarctica have become a globally important site for scientific research and environmental monitoring. Historical data can make important contributions to current research activities and environmental management in Antarctica, but tend to be widely scattered and difficult to access. We address this need in the MDV by compiling over 5,000 historical photographs, sketches, maps, oral interviews, publications, and other archival resources into an online digital archive. The data have been digitized and georeferenced using a standardized metadata structure, which enables intuitive searches and data discovery via an online interface. The ultimate aim of the archive is to create as comprehensive as possible a record of human activity in the MDV to support ongoing research, management, and conservation efforts. This is a valuable tool for scientists seeking to understand the dynamics of change in lakes, glaciers, and other physical systems, as well as humanistic inquire into the history of the Southern continent. In addition to providing benchmarks for understanding change over time, the data can help target field sampling for studies working under the assumption of a pristine landscape by enabling researchers to identify the date and extent of past human activities. The full database is accessible via the McMurdo Dry Valleys Long Term Ecological Research site: http://mcmurdohistory.lternet.edu/.
DOI: 10.6084/m9.figshare.13159748
title: mr-2020-26 .tar.gz

description: Compressed tar file of all NMR spectra belonging to the figures of the submission mr-2020-26 to the Copernicus journal Magnetic Resonance.<br>Table of contents <br> Experiment number Experiment <br> 1 ubiquitin E18Sep with Y3+ (Fig. 1a) 2 ubiquitin E18Sep with Tb3+ (Fig. 1a) 3 ubiquitin E18Sep with Tm3+ (Fig. 1a) 4 ubiquitin E16Q/E18Sep with Y3+ (Fig. 1b) 5 ubiquitin E16Q/E18Sep with Tb3+ (Fig. 1b) 6 ubiquitin E16Q/E18Sep with Tm3+ (Fig. 1b) 7 ubiquitin E18Sep/D21N with Y3+ (Fig. 1c) 8 ubiquitin E18Sep/D21N with Tb3+ (Fig. 1c) 9 ubiquitin E18Sep/D21N with Tm3+ (Fig. 1c) 10 GB1 K10D/T11Sep with Y3+ (Fig. 3a) 11 GB1 K10D/T11Sep with Tb3+ (Fig. 3a) 12 GB1 K10Sep/T11Sep with Y3+ (Fig. 3b) 13 GB1 K10Sep/T11Sep with Tb3+ (Fig. 3b) 14 GB1 A24Sep/K28Sep with Y3+ (Fig. 4a) 15 GB1 A24Sep/K28Sep with Tb3+ (Fig. 4a) 16 GB1 A24Sep/K28Sep with Tm3+ (Fig. 4a) 17 ubiquitin T22Sep/N25D with Y3+ (Fig. 7a) 18 ubiquitin T22Sep/N25D with Tb3+ (Fig. 7a) 19 ubiquitin T22Sep/N25D/K29Q with Y3+ (Fig. 7b) 20 ubiquitin T22Sep/N25D/K29Q with Tb3+ (Fig. 7b) 21 ubiquitin Q2D/E64Sep with Y3+ (Fig. S5) 22 ubiquitin Q2D/E64Sep with Tb3+ (Fig. S5) 23 ubiquitin Q2D/E64Sep with Tm3+ (Fig. S5) 24 wild-type GB1 (Fig. S7a) 25 GB1 K4D/I6Sep (Fig. S7b) 26 wild-type Hsp90-N (Fig. S9a) 27 HSP90-N N91Sep (Fig. S9b)
DOI: 10.6092/ingv.it-cpti11
title: Catalogo Parametrico dei Terremoti Italiani (CPTI11)
title: Italian Parametric Earthquake Catalogue (CPTI11)
title: CPTI11

description: CPTI11 updates and improves the 2004 version of CPTI with respect to background information and structure. It is based on updated macroseismic (DBMI11; Locati et al., 2011) and instrumental databases; it contains records of foreshocks and aftershocks; for some offshore events, macroseismic earthquake parameters have been determined by means of the method by Bakun and Wentworth (1997); when both macroseismic and instrumental parameters are available, the two determinations and a default one are provided (in this case, the epicentre is selected according to expert judgement, while Mw is obtained as a weighted mean); for some events, whose macroseismic data are poor, no macroseismic parameters have been determined. CPTI11 does not include the results of some methodological developments performed in the frame of the EC project "SHARE". It does not consider the information background provided by: Molin et al. (2008); Camassi et al. (2011); recent studies on individual earthquakes; ECOS 2009 (Faeh et al., 2011) and SisFrance, 2010, yet, which will be considered in the next version. The area covered by CPTI11 is slightly reduced with respect to the one of CPTI04 (Fig. 1). The catalogue is composed of two sections: the main one (1000-2006) and the “Etna” earthquakes, for which a specific calibration is used for determining earthquake parameters. Appendix 4 supplies the list of the events which were included in CPTI04 but not in CPTI11 and the relevant explanation.
DOI: 10.14291/tccon.ggg2014.reunion01.r1
title: TCCON data from Réunion Island (RE), Release GGG2014.R1

description: The Total Carbon Column Observing Network (TCCON) is a network of ground-based Fourier Transform Spectrometers that record direct solar absorption spectra of the atmosphere in the near-infrared. From these spectra, accurate and precise column-averaged abundances of atmospheric constituents including CO2, CH4, N2O, HF, CO, H2O, and HDO, are retrieved. This data set contains observations from the TCCON station on Réunion Island.
description: <br>Cite this record as:<br>De Mazière, M., Sha, M. K., Desmet, F., Hermans, C., Scolas, F., Kumps, N., Metzger, J.-M., Duflot, V., & Cammas, J.-P. (2017). <i>TCCON data from Réunion Island (RE), Release GGG2014.R1</i> (Version R1) [Data set]. CaltechDATA. https://doi.org/10.14291/TCCON.GGG2014.REUNION01.R1<br> or choose a different citation style.<br>Download Citation<br>
description: <br>Unique Views: 351<br>Unique Downloads: 13<br> between December 20, 2017 and July 12, 2021<br>More info on how stats are collected<br>
DOI: 10.1594/pangaea.895777
title: Changes in growth parameters of cultured coccolithophores and isotopic composition of coccolith calcite with salinity

description: The table shows the physicochemical parameters of the medium and the data measured for cell division rates, cell size and oxygen and carbon isotope of coccoliths calcite according to salinity.
description: Supplement to: Hermoso, Michael; Lecasble, Marceau (2018): The effect of salinity on the biogeochemistry of the coccolithophores with implications for coccolith-based isotopic proxies. Biogeosciences, 15(22), 6761-6772
DOI: 10.1594/pangaea.897092
title: Raw data of continuous VM-ADCP (vessel-mounted Acoustic Doppler Current Profiler) profile during POLARSTERN cruise PS113
DOI: 10.1594/pangaea.898716
title: Physical oceanography during POLARSTERN cruise PS113
DOI: 10.1594/pangaea.900380
title: SID-3 analysis results for 2D scattering patterns during the ACLOUD campaign in 2017

description: Analysis results of the SID-3 2D scattering patterns measured during ACLOUD. Results contain information on the particle shape, sphericity and mesoscopic complexity. Data is in NASA ames format.
DOI: 10.1594/pangaea.900617
title: Output from iLOVECLIM Pa/Th module: Pre-industrial equilibrium and Nordic Seas hosing experiment

description: This dataset contains the model output from iLOVECLIM and its recently developed Pa/Th module for Pre-industrial equilibrium control run and Nordic Seas hosing experiments (freshwater addition in the Nordic Seas). The Pa/Th module computes the evolution of dissolved and particulate 231Pa and 230Th within the ocean model CLIO (3x3 degrees 20 vertical layers). For the Pre-Industrial control simulation, the dissolved and particulate 231Pa and 230Th activities are shown for the last 100 years of the equilibrium run (Figures 1, S1, S2). For the Nordic Seas hosing experiment (from Pre-Industrial equilibrium), the dataset contains the carbon isotopes and particulate Pa/Th responses and response times (as defined in Figure 2 - Figures 3, 4, S4, S5) as well as carbon isotopes and Pa/Th time series over the complete hosing simulation for 1) three selected locations in the Atlantic Basin (Figure 5) and the Bermuda rise (Figure 6).
DOI: 10.1594/pangaea.904420
title: Raw data from Triaxus topAWI tows during POLARSTERN cruise PS113
DOI: 10.1594/pangaea.907579
title: Statistical Reconstruction of Daily Precipitation and Temperature Fields in Switzerland back to 1864

description: Spatial information on past weather contributes to better understand the processes behind day-to-day weather variability and to assess the risks arising from weather extremes. This dataset provides daily, high-resolution reconstructions of precipitation and temperature fields for Switzerland back to 1864. Reconstructions are provided as "raw" data resulting from an analogue resampling method (ARM), as well as post-processed data (using an ensemble Kalman fitting approach for temperature and quantile mapping for precipitation. For further information, the reader is referred to the references.The dataset comprises the following files:- 2019-10-06_precip_ARM_1864-01-01-2017-12-31.nc (precipitation, analogue reconstructions)- 2019-10-06_precip_qmap_1864-01-01-2017-12-31.nc (precipitation, post-processed)- 2019-10-06_temp_ARM_1864-01-01-2017-12-31.nc (temperature, analogue reconstructions)- 2019-10-06_temp_EnKF_1864-01-01-2017-12-31.nc (temperature, post-processed)
description: Supplement to: Pfister, Lucas; Brönnimann, Stefan; Schwander, Mikhaël; Isotta, Francesco Alessandro; Horton, Pascal; Rohr, Christian (2020): Statistical reconstruction of daily precipitation and temperature fields in Switzerland back to 1864. Climate of the Past, 16(2), 663-678
DOI: 10.1594/pangaea.912597
title: A new dataset of satellite observation-based global surface soil moisture covering 2003-2018

description: Soil moisture is an important variable linking the atmosphere and the terrestrial ecosystems. However, long-term satellite monitoring of surface soil moisture is still lacking at global scale. In this study, we conducted data fusion of up to 11 microwave remote sensing-based soil moisture products through a set of neural networks, with SMAP soil moisture data applied as the fundamental training target. The training efficiency proves to be high (R2 =0.95) due to the selection of 9 quality impact factors of microwave soil moisture products and the elaborate organization structure of multiple different neural networks (5 rounds of simulation; 8 substeps; 74 independent neural networks; and &gt;106 regional subnetworks). We achieved global satellite monitoring of surface soil moisture during 2003~2018 at 0.1° resolution. This new dataset, once validated against the International Soil Moisture Network (ISMN) records, is found superior to the existing products (ASCAT-SWI, GLDAS Noah, ERA5-Land, CCI/ECV and GLEAM), and is applicable to studying both the spatial and temporal patterns. It suggests an increase in global surface soil moisture, and reveals that the surface moisture decline on rainless days is highest in summers over the low-latitudes but highest in winters in most mid-latitude areas. Notably, the error propagation with the extension of the simulation period to the past is well controlled, indicating that the fusion algorithm will be more meaningful in future when more advanced sensors are in operation.
DOI: 10.1594/pangaea.914677
title: Scavenging amphipod abundance at trap stations during SONNE cruises SO239 and SO242/1, Clarion Clipperton Fracture Zone (Pacific) and DISCOL area (Peru Basin)

description: This data set summarises the scavenging Amphipoda data which were collected using baited trap sampling from two abyssal basins in 2015. Sampling was carried out at eight stations in the eastern Clarion-Clipperton Zone, and at five stations in the Discol experimental area, during expeditions SO239 and SO242/1 respectively. The purpose of this sampling was to construct a biodiversity assessment and to investigate the ecological impacts of deep-sea mining in the Pacific Ocean, by comparison of the Clarion-Clipperton Zone assemblage to this a smaller-scale disturbance proxy site.
DOI: 10.17596/0000001
title: Global Nutrients Dataset 2013

description: In this site, a new dataset for nutrients in sea water, Global Nutrient Dataset 2013 (GND13), is provided. The data in the dataset are traceable to the SI. Although data synthesis work was made also for previous datasets such as WOA09, WOA13, GLODAPv2, etc., influences of quality of original data are not controlled sufficiently, and the traceability is not guaranteed. These are caveats of previous dataset. The GND13 has comparability and traceability of data, because the dataset is well quality-controlled based on data collected during CLIVAR and subsequent GO-SHIP cruises mainly by the R/V Mirai, where reference materials for nutrients in seawater were used.
DOI: 10.17882/41334
title: Global Ocean delayed mode in-situ observations of ocean surface currents

description: The In Situ delayed mode product designed for reanalysis purposes integrates the best available version of in situ data for ocean surface currents. The data are collected from the Surface Drifter Data Assembly Centre (SD-DAC at NOAA AOML). All surface drifters data have been processed to check for drogue loss. Drogued and undrogued drifting buoy surface ocean currents are provided with a drogue presence flag as well as a wind slippage correction for undrogued buoys. Altimeter and wind data have been used to extract the direct wind slippage from the total drifting buoy velocities. This product is designed to be assimilated into or for validation purposes of operational models operated by ocean forecasting centers for reanalysis purposes or for research community. These users need data aggregated and quality controlled in a reliable and documented manner.
DOI: 10.18140/flx/1440161
title: FLUXNET2015 FR-Fon Fontainebleau-Barbeau

description: This is the FLUXNET2015 version of the carbon flux data for the site FR-Fon Fontainebleau-Barbeau.
DOI: 10.18140/flx/1440215
title: FLUXNET2015 DE-RuR Rollesbroich

description: This is the FLUXNET2015 version of the carbon flux data for the site DE-RuR Rollesbroich.
DOI: 10.18739/a2fp03
title: Reactive gases in the Dome C snowpack, Antarctica, 2012-2014
DOI: 10.23728/b2share.0d3a99db75df4238820ee548f35ee36b
title: The Tall Tower Dataset

description: A dataset containing quality controlled wind observations from 181 different tall towers has been created. Wind speed and wind direction measurements have been collected from existing tall towers around the world within the context of the INDECIS project in an effort to boost the utilisation of these non-standard atmospheric datasets. Wind observations taken at several heights greater than 10 meters above ground level have been retrieved from various sparse datasets and compiled in a unique collection with a common format, access, documentation and quality control. For the latter, a total of 18 Quality Control checks have been considered to ensure a high quality of the wind observations. Non-quality-controlled temperature, relative humidity and barometric pressure data have been also obtained and made available. Complete information on the collection and quality control processes can be found at https://earth.bsc.es/wiki/lib/exe/fetch.php?media=library:external:technical_memoranda:technical_report_talltower_database_v2.pdf 

These data are made available in good faith to be used for non-commercial purposes. In no event will the authors be liable to you or any third party for any damage or loss resulting from any use or misuse of these data.

Updates from the previous version: Data that failed at least one of the QC tests have been removed. The flag values and raw data are still accessible now labelled with '_raw'. Attribute name 'flag_meanings' has been renamed to 'flag_definition'. Added temperature, relative humidity and pressure data to the BCI tall tower. Corrected an erratum in the pressure unit attribute.
DOI: 10.5067/modis/mod05_l2.061
title: MODIS/Terra Total Precipitable Water Vapor 5-Min_x005F_x000D__x000D_ L2 Swath 1km and 5km
DOI: 10.5067/reyn2-oimow
title: Reynolds NCEP Level 4 Optimally Interpolated SST Weekly Version 2
DOI: 10.5067/suborbital/oracles/p3/2016_v1
title: Suite of Aerosol, Cloud, and Related Data Acquired Aboard P3 During ORACLES 2016, Version 1
DOI: 10.5281/zenodo.1252036
title: Radio/X-Ray Correlation Database For X-Ray Binaries

description: The radio-X-ray correlation in accretion neutron stars and black holes has been discussed in detail in the literature. BH X-ray binaries (XRBs) show compact partially self-absorbed jet emission in quiescence and in the hard state during outbursts, making them brighter in radio compared to NS LMXBs with similar X-ray luminosities. Since, there have been numerous efforts at further exploring and understanding this correlation. Numerous sources (both known and newly identified) have been observed in radio and X-rays. Here, we have compiled a collection of these measurements from the literature and we actively add new measurements as we notice new publications. This package contains a catalog of radio and X-ray observations of Galactic X-ray binaries as reported in literature.
DOI: 10.5281/zenodo.1308857
title: Prior And Posterior Uncertainties Of Sea Ice Volume And Snow Volume

description: Prior and posterior uncertainties of sea ice volume (SIV, columns 4-6) and snow volume (SNV, columns 7-9) respectively for three regions in km3. Column 1 indicates observation, column 2 indicates uncertainty range ("product" refers to uncertainty specification provided with product), column 3 indicates uncertainty range of additional hypothetical snow product ("–" means no snow product is used). In each of columns 4-9 the lowest uncertainty range is highlighted in bold face font. The two bottom rows give estimates for the uncertainty due to model error, i.e. the residual uncertainty with optimal control vector.
DOI: 10.5281/zenodo.3104573
title: Modern calibration of Poa flabellata (Tussac grass) as a new paleoclimate proxy in the South Atlantic

description: Carbon and oxygen stable isotopes in alpha cellulose from <em>Poa flabellata</em> leaf and root material collected between September 2015 to September 2016 in the Falkland Islands at four different locations.
DOI: 10.5281/zenodo.3359192
title: Greenland monthly surface mass balance 1840-2012

description: This surface mass balance (SMB) product is based on Box (2013), with refinements described by Schlegel et al. (2016), Appendix. It includes monthly estimates of accumulation and melt, as well as estimates for SMB error for the historical period (1960-2012). It is the results of a calibration of observational data to regional climate model (RCM) output, in this case RACMO2.3 (Noël et al., 2016). The calibration for temperature (T) and SMB components is based on a 53-year overlap period (1960-2012). Note that the overlap period for the calibration of snow accumulation rate is shorter, since ice core data availability drops after 1999. Calibration is made using linear regression coefficients for 5 km grid cells that match the average of the reconstruction to RACMO2.3. The RACMO2.3 output are resampled and reprojected from the native 0.1 deg (~10 km) grid to a 5 km grid better resolving areas where sharp gradients occur, especially near the ice margin where mass fluxes are largest.
description: {"references": ["Box, J. E.: Greenland Ice Sheet Mass Balance Reconstruction. Part II: Surface Mass Balance (1840-2010), J. Clim., 26, 6974\u20136989, doi:10.1175/JCLI-D-12-00518.1, 2013.", "No\u00ebl, B., van de Berg, W. J., Machguth, H., Lhermitte, S., Howat, I., Fettweis, X., and van den Broeke, M. R.: A daily, 1\u202fkm resolution data set of downscaled Greenland ice sheet surface mass balance (1958\u20132015), The Cryosphere, 10, 2361-2377, https://doi.org/10.5194/tc-10-2361-2016, 2016.", "Schlegel, N.-J., Wiese, D. N., Larour, E. Y., Watkins, M. M., Box, J. E., Fettweis, X., and van den Broeke, M. R.: Application of GRACE to the assessment of model-based estimates of monthly Greenland Ice Sheet mass balance (2003\u20132012), The Cryosphere, 10, 1965-1989, https://doi.org/10.5194/tc-10-1965-2016, 2016."]}
DOI: 10.5281/zenodo.3467300
title: Blue Green Wave hydrological data

description: The Blue Green Wave of Champs-sur-Marne (France) represents the largest green roof (1 ha) of the Greater Paris Area. The Hydrology, Meteorology and Complexity lab of Ecole des Ponts ParisTech has chosen to convert this architectural building as a full-scale monitoring site devoted to study the performances of green infrastructures in stormwater management. For this purpose, the relevant components of the water balance during a rainfall event have been monitored: rainfall, water content in the substrate and the discharge flowing out of the infrastructure. Data provided by adapted measurement sensors were collected during 78 days between February and May 2018. The related raw data and a python program transforming them into hydrological quantities and providing some first elements of analysis have been made available. These measurements are useful to better understand the processes (infiltration and retention) conducted their hydrological performances, and their spatial variability due to substrate heterogeneity.
DOI: 10.5281/zenodo.3522841
title: Synthetic geophysical survey using geological modelling from the Yerrida Basin (Western Australia)

description: This is a companion dataset to the manuscript:
"Towards geologically reasonable lithological classification from integrated geophysical inverse modelling", by J. Giraud, M. Lindsay, M. Jessell, and V. Ogarko.
This dataset contains the true model, the geological uncertainty volume constraining inversion, the starting model for inversion, and the inverted model. It also contains the inverted geophysical data. The inverted data were generated using geological modelling from the area and prior petrophysical information (more information in the above-mentioned document). For standalone usage of this dataset, the inversion parameters can be found in the following publication: 
Giraud, J., M. Lindsay, V. Ogarko, M. Jessell, R. Martin, and E. Pakyuz-Charrier, 2019a, Integration of geoscientific uncertainty into geophysical inversion by means of local gradient regularization: Solid Earth, 10, 193–210.