cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.895040
title: CICE output from Global Ocean Forecast System (GOFS) 3.1 for 2018092412

description: INITIALIZATION: 2018092412FORECASTS:12-hrly out to 7.5 days (t180)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;
DOI: 10.1594/pangaea.895041
title: CICE output from Global Ocean Forecast System (GOFS) 3.1 for 2018092512

description: INITIALIZATION: 2018092512FORECASTS:12-hrly out to 7.5 days (t180)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;
DOI: 10.1594/pangaea.895043
title: CICE output from Navy Earth System Model (NESM) for 2018092312

description: INITIALIZATION: 2018092312FORECASTS:daily at 00Z out to 45 days (t1068)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;
DOI: 10.1594/pangaea.895044
title: CICE output from Navy Earth System Model (NESM) for 2018092412

description: INITIALIZATION: 2018092412FORECASTS:daily at 00Z out to 45 days (t1068)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;
DOI: 10.1594/pangaea.771891
title: (Table S1) Sea surface temperature estimation for sediment core MD01-2444
DOI: 10.1594/pangaea.839316
title: (Table 4a) Calibrated age ranges obtained with the atmospheric calibration curve, of sedimentary total organic carbon, terrestrial macrofossils, and isolated biomarkers originating from differently aged sediment layers, ODP Hole 169-1034C

description: AGE [ka BP] is the sediment age. #0 = modern age. Calibrated with the atmospheric calibration curve using a Delta R of 401 ± 25 years.
DOI: 10.1594/pangaea.895045
title: CICE output from Navy Earth System Model (NESM) for 2018092512

description: INITIALIZATION: 2018092512FORECASTS:daily at 00Z out to 45 days (t1068)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;
DOI: 10.1594/pangaea.770567
title: Present-day King George Island ice cap geometry measured by ground penetrating radar in 2008/09

description: We present a consistent data set for the ice thickness, the bedrock topography and the ice surface topography of the King George Island ice cap (Arctowski Icefield and the adjacent central part). The data set is composed of groundbased and airborne Ground Penetrating Radar (GPR) and differential GPS (DGPS) measurements, obtained during several field campaigns. The data set incorporates groundbased measurements in the safely accessible inner parts and airborne measurements in the heavily crevassed coastal areas of the ice cap. In particular, the inclusion of airborne GPR measurements with the 30MHz BGR-P30-System developed at the Institute of Geophysics (University of Münster) completes the picture of the ice geometry substantially. The compiled digital elevation model of the bedrock shows a rough, highly variable topography with pronounced valleys, ridges, and troughs. The mean ice thickness is approx. 238m, with a maximum value of approx. 400m in the surveyed area. Noticeable are bounded areas in the bedrock topography below sea level where marine based ice exists.
description: See other version for data in NetCDF format.
description: Supplement to: Rückamp, Martin; Blindow, Norbert (2011): King George Island ice cap geometry updated with airborne GPR measurements. Earth System Science Data, 4(1), 23-30
DOI: 10.1594/pangaea.891170
title: Water storage changes in the interior of the Tibetan Plateau, link to data underlying Fig. 1-3 and A1-A13
DOI: 10.1594/pangaea.704796
title: (Table 4) Polarity magnetozones and correlative chrons of DSDP Hole 43-384

description: Below 161.25 mbsf magnetostratigraphy from Larson and Opdyke (1979, doi:10.2973/dsdp.proc.43.139.1979)
DOI: 10.1594/pangaea.840594
title: (Appendix 1) Dissolved organic matter composition of mesocosm experiments given as FT-ICR-MS peak intensities
DOI: 10.1594/pangaea.773308
title: Mass balance measurements on King George Island ice cap in 2007 and 2008

description: The Antarctic Peninsula has been identified as a region of rapid on-going climate change with impacts on the cryosphere. The knowledge of glacial changes and freshwater budgets resulting from intensified glacier melt is an important boundary condition for many biological and integrated earth system science approaches. We provide a case study on glacier and mass balance changes for the ice cap of King George Island. The area loss between 2000 and 2008 amounted to about 20 km**2 (about 1.6% of the island area) and compares to glacier retreat rates observed in previous years. Measured net accumulation rates for two years (2007 and 2008) show a strong interannual variability with maximum net accumulation rates of 4950 mm w.e./a and 3184 mm w.e./a, respectively. These net accumulation rates are at least 4 times higher than reported mean values (1926-95) from an ice core. An elevation dependent precipitation rate of 343 mm w.e./a (2007) and 432 mm w.e./a (2008) per 100 m elevation increase was observed. Despite these rather high net accumulation rates on the main ice cap, consistent surface lowering was observed at elevations below 270 m above ellipsoid over an 11-year period. These DGPS records reveal a linear dependence of surface lowering with altitude with a maximum annual surface lowering rate of 1.44 m/a at 40 m and -0.20 m/a at 270 m above ellipsoid. These results fit well to observations by other authors and surface lowering rates derived from the ICESat laser altimeter. Assuming that climate conditions of the past 11 years continue, the small ice cap of Bellingshausen Dome will disappear in about 285 years.
description: We provide mass balance measurements on the King George Island ice cap on several locations for two subsequent time periods. The measured net accumulation rates for two years (2007 and 2008) show a strong interannual variability with maximum net accumulation rates of 4950 mm w.e. a^-1 and 3184 mm w.e. a^-1, respectively. These net accumulation rates are at least 4 times higher than reported mean values (1926-95) from an ice core. An elevation dependent precipitation rate of 343 mm w.e. a^-1 (2007) and 432 mm w.e. a^-1 (2008) per 100 m elevation increase was observed.
description: Supplement to: Rückamp, Martin; Braun, Matthias Holger; Suckro, Sonja K; Blindow, Norbert (2011): Observed glacial changes on the King George Island ice cap, Antarctica, in the last decade. Global and Planetary Change, 79(1-2), 99-109
DOI: 10.1594/pangaea.855310
title: SST reconstruction trom a fossil coral from Tasmaloum

description: A fossil coral from Tasmaloum (Vanuatu) was found between 0.80 and 1.20 m depth in drill core 9A, collected at an altitude of +4.66 m above sea level. Owing to the calculated uplift rate the paleodepth of the Porites can be estimated ~10-15 m at 4150 years B.P. The surrounding coral assemblages indicate an open shallow marine environment. For the present study, precision on the Sr/Ca paleothermometer was ±1.3 deg C, and ±0.9 deg C for the U/Ca paleothermometer. The data consist of reconstructed Sea Surface Temperatures extrapolated from analyses of trace element ratios in a fossil coral head. A date of 4166 ±15 calendar yr BP was obtained by the U/Th series technique for the coral. This date corresponds to the cold episode centered around sample #464.
DOI: 10.1594/pangaea.855311
title: Sr/Ca and U/Ca ratios of a fossil coral from Tasmaloum

description: A fossil coral from Tasmaloum (Vanuatu) was found between 0.80 and 1.20 m depth in drill core 9A, collected at an altitude of +4.66 m above sea level. Owing to the calculated uplift rate the paleodepth of the Porites can be estimated ~10-15 m at 4150 years B.P. The surrounding coral assemblages indicate an open shallow marine environment.
DOI: 10.1594/pangaea.894989
title: Basic and other measurements of radiation at station Cape Baranova (2016-07)
DOI: 10.1594/pangaea.814098
title: (Appendix 4) Nd and Mn concentration in mixed planktonic foraminifera of sediment cores BOFS10K and BOFS11K

description: Planktonic foraminifera size fraction &gt;250 µm.
DOI: 10.1594/pangaea.858343
title: Time series of atmospheric water vapour at station AZUL_S1
DOI: 10.1594/pangaea.863409
title: Continuous thermosalinograph oceanography along HEINCKE cruise track HE440
DOI: 10.1594/pangaea.810709
title: Plant Functional Type (PFT) map over Siberia derived from GlobCover 2005 dataset, link to dataset in NetCDF format

description: High-latitude ecosystems play an important role in the global carbon cycle and in regulating the climate system and are presently undergoing rapid environmental change. Accurate land cover data sets are required to both document these changes as well as to provide land-surface information for benchmarking and initializing Earth system models. Earth system models also require specific land cover classification systems based on plant functional types (PFTs), rather than species or ecosystems, and so post-processing of existing land cover data is often required. This study compares over Siberia, multiple land cover data sets against one another and with auxiliary data to identify key uncertainties that contribute to variability in PFT classifications that would introduce errors in Earth system modeling. Land cover classification systems from GLC 2000, GlobCover 2005 and 2009, and MODIS collections 5 and 5.1 are first aggregated to a common legend, and then compared to high-resolution land cover classification systems, vegetation continuous fields (MODIS VCFs) and satellite-derived tree heights (to discriminate against sparse, shrub, and forest vegetation). The GlobCover data set, with a lower threshold for tree cover and taller tree heights and a better spatial resolution, tends to have better distributions of tree cover compared to high-resolution data. It has therefore been chosen to build new PFT maps for the ORCHIDEE land surface model at 1 km scale. Compared to the original PFT data set, the new PFT maps based on GlobCover 2005 and an updated cross-walking approach mainly differ in the characterization of forests and degree of tree cover. The partition of grasslands and bare soils now appears more realistic compared with ground truth data. This new vegetation map provides a framework for further development of new PFTs in the ORCHIDEE model like shrubs, lichens and mosses, to represent the water and carbon cycles in northern latitudes better. Updated land cover data sets are critical for improving and maintaining the relevance of Earth system models for assessing climate and human impacts on biogeochemistry and biophysics.
description: NetCDF file includes 16 Plant Functional Type Maps:PFT1 - Bare SoilPFT2 - Tropical Broad_leaved EvergreenPFT3 - Tropical Broad_leaved RaingreenPFT4 - Temperate Needleleaf EvergreenPFT5 - Temperate Broad_leaved EvergreenPFT6 - Temperate Broad_leaved SummergreenPFT7 - Boreal Needleleaf EvergreenPFT8 - Boreal Broad-leaved SummergreenPFT9 - Boreal Needleleaf SummergreenPFT10 - C3 GrassPFT11 - C4 GrassPFT12 - C3 AgriculturePFT13 - C4 AgriculturePFT14 - WaterPFT15 - Snow/IcePFT16 - No Data
description: Supplement to: Ottlé, Catherine; Lescure, Julie; Maignan, Fabienne; Poulter, Benjamin; Wang, Tao; Delbart, Nicolas (2013): Use of various remote sensing land cover products for plant functional type mapping over Siberia. Earth System Science Data, 5(2), 331-348
DOI: 10.1594/pangaea.858357
title: Time series of atmospheric water vapour at station CART_S1
DOI: 10.1594/pangaea.858415
title: Time series of atmospheric water vapour at station RIO2_S1
DOI: 10.1594/pangaea.859043
title: LiDAR elevation data of Yukon Coast and Herschel Island in 2012, links to Shapefiles and TIFF images

description: Platform: Device: VQ580 laser scanner; Aircraft: POLAR 5; Flight height: around 200 m; Swath width: around 200 m; Point spacing: 0.5 m; Weather conditions: Weather was cloudy with cloud base around 200 m a.s.l. Air temperature ranged between 10 and 12 °C with wind speed ranging from 15 to 19 km h-1 from easterly direction (70 - 90°).Raster properties: Horizontal resolution: 1m; Vertical accuracy: 0.15 m; Point interpolation: inverse distance weighting (IDW) with 10 m radius; Coordinate system: NAD83 UTM zone 7Raster layers are divided in to 9 sections in order to reduce raster size.
DOI: 10.1594/pangaea.773310
title: Measured ice surface velocities on the King George Island ice cap with DGPS

description: King George Island is located at the northern tip of the Antarctic Peninsula, which is influenced by maritime climate conditions. The observed mean annual air temperature at sea level is -2.4°C. Thus, the ice cap is regarded as sensitive to changing climatic conditions. Ground-penetrating radar surveys indicate a partly temperate ice cap with an extended water layer at the firn/ice transition of the up to 700 m high ice cap. Measured firn temperatures are close to 0°C at the higher elevations, and they differ considerably from the measured mean annual air temperature. The aim of this paper is to present ice-flow dynamics by means of observations and simulations of the flow velocities. During several field campaigns from 1997/98 to 2008/09, ice surface velocities were derived with repeated differential GPS measurements. Ice velocities vary from 0.7 m/a at the dome to 112.1 m/a along steep slopes. For the western part of the ice cap a three-dimensional diagnostic full-Stokes model was applied to calculate ice flow. Parameters of the numerical model were identified with respect to measured ice surface velocities. The simulations indicate cold ice at higher elevations, while temperate ice at lower elevations is consistent with the observations.
description: During several field campaigns from 1997/98 to 2008/09, in-situ ice surface velocities were derived with repeated differential GPS measurements.The calculated velocities range from about 0 m/a close to the domes and ice divides to 112.1m/a at the inner parts of the main ice cap. They neither show seasonal variations nor an incresase/decrease within the observational period. Therefore, in case of multiple readings, the mean value is calaculated. Note that also the location in the provided data set is a mean value.
description: Supplement to: Rückamp, Martin; Blindow, Norbert; Suckro, Sonja K; Braun, Matthias Holger; Humbert, Angelika (2010): Dynamics of the ice cap on King George Island, Antarctica: field measurements and numerical simulations. Annals of Glaciology, 51(55), 80-90
DOI: 10.1594/pangaea.888179
title: Flux summary of measured hydrochemical parameters and statistics on concentrations for 2014, 2015 and 2016
DOI: 10.1594/pangaea.704794
title: (Table 3) Paleomagnetic measurements of DSDP Hole 43-384
DOI: 10.1594/pangaea.858344
title: Time series of atmospheric water vapour at station BAIR_S1
DOI: 10.1594/pangaea.888177
title: Hydrochemistry of a small Low Arctic watershed on Herschel Island (2014)
DOI: 10.1594/pangaea.895142
title: CICE output from Global Ocean Forecast System (GOFS) 3.1 for 2018092612

description: INITIALIZATION: 2018092612FORECASTS:12-hrly out to 7.5 days (t180)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;
DOI: 10.1594/pangaea.895143
title: CICE output from Global Ocean Forecast System (GOFS) 3.1 for 2018092712

description: INITIALIZATION: 2018092712FORECASTS:12-hrly out to 7.5 days (t180)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;
DOI: 10.1594/pangaea.895150
title: CICE output from Navy Earth System Model (NESM) for 2018092912

description: INITIALIZATION: 2018092912FORECASTS:daily at 00Z out to 45 days (t1068)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;
DOI: 10.1594/pangaea.858346
title: Time series of atmospheric water vapour at station BDOS_S1
DOI: 10.1594/pangaea.704825
title: (Table 7) Magnetostratigraphy and calcareous plankton stratigraphy and zonal boundaries of DSDP Hole 43-384

description: In this study, core catchers are located in continuity with the lowest recovered section in a core, in agreement with the current ODP policy. Also several samples analyzed for calcareous nannofossils proved to be out of place (several slides were prepared to rule out laboratory contamination). x shows intervals of uncertainty around biozonal and magnetostratigraphic. The data set includes magnetostratigraphy of Larson and Opdyke (1979, doi:10.2973/dsdp.proc.43.139.1979)
DOI: 10.1594/pangaea.895144
title: CICE output from Global Ocean Forecast System (GOFS) 3.1 for 2018092812

description: INITIALIZATION: 2018092812FORECASTS:12-hrly out to 7.5 days (t180)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;
DOI: 10.1594/pangaea.704826
title: (Table 9) Paleocene calcareous nannoplankton biochronology as deduced from magneostratigraphic correlations in DSDP Hole 43-384 n
DOI: 10.1594/pangaea.888178
title: Hydrochemistry of a small Low Arctic watershed on Herschel Island (2015)
DOI: 10.1594/pangaea.895145
title: CICE output from Global Ocean Forecast System (GOFS) 3.1 for 2018092912

description: INITIALIZATION: 2018092912FORECASTS:12-hrly out to 7.5 days (t180)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;
DOI: 10.1594/pangaea.895146
title: CICE output from Global Ocean Forecast System (GOFS) 3.1 for 2018093012

description: INITIALIZATION: 2018093012FORECASTS:12-hrly out to 7.5 days (t180)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;
DOI: 10.1594/pangaea.895147
title: Georeferenced photographs of benthic photoquadrats acquired along transects from Heron Reef flat and slope areas (2015-11)
DOI: 10.1594/pangaea.890851
title: Wet dissolved carbon concentration during the concentrated rainfall season (July-September, 2015) in Yangjuangou Catchment, Loess Plateau (Other Version)