cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.898764
title: Annual melt ratios obtained from Meltlayer catalogs of the RECAP_S2 ice core, East Greenland

description: Annual melt ratios of the RECAP ice cores have been obtained by calculating the Snow Water Equivalent (SWE) of the summed thicknesses of melt layers contained in an annual layer and divided the result by the SWE of the respective annual layer. Densities of the annual layers have been taken from 2D computed tomohraph measurements performed on each core.
DOI: 10.1594/pangaea.887414
title: Year-round particle size distribution measurements at the coastal Antarctic site Neumayer
DOI: 10.1594/pangaea.936472
title: Expanded measurements from station Ny-Ålesund (2018-11)

description: 99999: No clouds detected; Version 2, 2021-09-28 with some previously missing values for 10000m CBH inserted
DOI: 10.1594/pangaea.954634
title: Radiosonde measurements from station Bondville (2021-01)

description: Start location: Lincoln, IL; Distance from radiation site: 82 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.954635
title: Other measurements at 10 m from station Bondville (2021-01)
DOI: 10.1594/pangaea.847628
title: Biomass of mesozooplankton in the western part of the Black Sea in 1997 during the Cooperative Marine Science Program for the Black Sea (CoMSBlack)

description: The “15BO1997001” dataset is based on samples collected in the spring of 1997. The whole dataset is composed of 66 samples (from 27 stations of National Monitoring Sampling Grid) with data of zooplankton species composition, abundance and biomass. Samples were collected in discrete layers 0-10, 0-20, 0-50, 10-25, 25-50, 50-100 and from bottom up to the surface at depths depending on water column stratification and the thermocline depth.The collected material was analysed using the method of Dimov (1959). Samples were brought to volume of 25-30 ml depending upon zooplankton density and mixed intensively until all organisms were distributed randomly in the sample volume. After that 5 ml of sample was taken and poured in the counting chamber which is a rectangle form for taxomomic identification and count. Large (&gt; 1 mm body length) and not abundant species were calculated in whole sample. Counting and measuring of organisms were made in the Dimov chamber under the stereomicroscope to the lowest taxon possible. Taxonomic identification was done at the Institute of Oceanology by Asen Konsulov using the relevant taxonomic literature (Mordukhay-Boltovskoy, F.D. (Ed.). 1968, 1969,1972 ). The biomass was estimated as wet weight by Petipa, 1959 (based on species specific wet weight). Wet weight values were transformed to dry weight using the equation DW=0.16*WW as suggested by Vinogradov & Shushkina, 1987.The collected material was analysed using the method of Dimov (1959). Samples were brought to volume of 25-30 ml depending upon zooplankton density and mixed intensively until all organisms were distributed randomly in the sample volume. After that 5 ml of sample was taken and poured in the counting chamber which is a rectangle form for taxomomic identification and count. Copepods and Cladoceras were identified and enumerated; the other mesozooplankters were identified and enumerated at higher taxonomic level (commonly named as mesozooplankton groups). Large (&gt; 1 mm body length) and not abundant species were calculated in whole sample. Counting and measuring of organisms were made in the Dimov chamber under the stereomicroscope to the lowest taxon possible. Taxonomic identification was done at the Institute of Oceanology by Asen Konsulov using the relevant taxonomic literature (Mordukhay-Boltovskoy, F.D. (Ed.). 1968, 1969,1972 ). The biomass was estimated as wet weight by Petipa, 1959 ussing standard average weight of each species in mg/m3. WW were converted to DW by equation DW=0.16*WW (Vinogradov ME, Sushkina EA, 1987).
DOI: 10.1594/pangaea.552380
title: Thick-section images of the EDML ice core from 1300 to 1400 m depth

description: measured at AWI
DOI: 10.1594/pangaea.954653
title: Other measurements at 10 m from station Bondville (2021-05)
DOI: 10.1594/pangaea.875899
title: Meteorological synoptical observations from station Minamitorishima (2017-03)
DOI: 10.1594/pangaea.724481
title: Zooplankton time series at station Point B in 1989
DOI: 10.1594/pangaea.936416
title: Expanded measurements from Neumayer Station (2014-06)

description: 99999: No clouds detected; Version 2, 2021-09-27 with some previously missing values for 10000m CBH inserted
DOI: 10.1594/pangaea.496649
title: Water temperature XBT profiles from cruise UNM_1986
DOI: 10.1594/pangaea.846921
title: (Table 1) Mean sea-ice properties from moored upward looking sonars along the Greenwich meridian

description: Sea-ice ocean interaction processes are of significant influence on the water mass formation in the Weddell gyre. On the basis of data obtained between 1984 and 2008 from eight repeat hydrographic sections, moored instruments and profiling floats in the Weddell gyre on the Greenwich meridian - almost all of them collected with R.V. Polarstern - we identified variations in the properties of the Winter Water and the sea ice draft. In the Winter Water the salinity was relatively low throughout the 1990s (with a minimum in 1992) and a maximum was observed in 2003. Observations of sea ice draft by moored upward looking sonars are available from 1996 onwards. In the southern part of the transect they display variations on a decadal time scale with a minimum in sea-ice thickness in 1998 and an increase since then. Salinity variations in the Winter Water layer cannot be explained only by variations in sea-ice formation and variable entrainment of underlying Warm Deep Water, but lateral advection of water and sea ice needs to be taken into account as well. Potential sources are melt water from the ice shelves in the western Weddell Sea or transport of water of low salinity entering the Weddell gyre from the east. Accompanying variations of the properties of Warm Deep Water are discussed in detail in a companion paper (Fahrbach et al., 2011, doi:10.1016/j.dsr2.2011.06.007).
description: Supplement to: Behrendt, Axel; Fahrbach, Eberhard; Hoppema, Mario; Rohardt, Gerd; Boebel, Olaf; Klatt, Olaf; Wisotzki, Andreas; Witte, Hannelore (2011): Variations of Winter Water properties and sea ice along the Greenwich meridian on decadal time scales. Deep Sea Research Part II: Topical Studies in Oceanography, 58(25-26), 2524-2532
DOI: 10.1594/pangaea.936419
title: Expanded measurements from Neumayer Station (2015-08)

description: 99999: No clouds detected; Version 2, 2021-09-27 with some previously missing values for 10000m CBH inserted
DOI: 10.1594/pangaea.954660
title: Ultra-violet measurements from station Bondville (2021-07)
DOI: 10.1594/pangaea.936420
title: Expanded measurements from Neumayer Station (2015-10)

description: 99999: No clouds detected; Version 2, 2021-09-27 with some previously missing values for 10000m CBH inserted
DOI: 10.1594/pangaea.724491
title: Zooplankton time series at station Point B in 1999
DOI: 10.1594/pangaea.900858
title: CICE output from Navy Earth System Prediction Capability (ESPC) for 2019022512

description: INITIALIZATION: 2019022512FORECASTS: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.793042
title: (Appendix F) Major element composition of Cr-spinel from ODP Leg 135 holes
DOI: 10.15468/dl.uncj6n
title: Occurrence Download

description: A dataset containing 4 species occurrences available in GBIF matching the query:
{
 "and" : [
 "DatasetKey is HUSC - Herbário Unisanta",
 "TaxonKey is Droseraceae"
 ]
}

 The dataset includes 4 records from 1 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0031176-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.954662
title: Radiosonde measurements from station Bondville (2021-07)

description: Start location: Lincoln, IL; Distance from radiation site: 82 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.724493
title: Zooplankton time series at station Point B in 2001
DOI: 10.1594/pangaea.841217
title: (Table 4a) Assumed asexual regeneration events in aspen (Populus tremula) related to climatic and biotic factors for the period 1916–2009

description: The annual number of trees (total n = 160) assumed to have arisen by asexual regeneration was related to: (1) summer temperature (mean = 10.0 °C, SE = 0.14); (2) summer precipitation (mean = 84 mm, SE = 3.46); (3) moth damage to birch, possibly affecting aspen asexual reproduction and survival; high positive values point to increased damage (mean = -0.03 negative birch-minus-pine indices, SE = 0.03).
DOI: 10.1594/pangaea.884904
title: Radiosonde measurements from station Minamitorishima (2017-11)
DOI: 10.1594/pangaea.875718
title: Geochemistry of sediment core INVAS12-10
DOI: 10.1594/pangaea.845457
title: Meteorological synoptical observations from Neumayer Station (2014-04)
DOI: 10.1594/pangaea.898307
title: Sea-bed videos (benthos) from the North Sea along ROV profile HE169/760

description: Positions and depths from the ship's automatic data recording system. The ROV-system sprint 103 was equipped with two video- and one 36mm still camera, lights, flash-lights, compass, and parallel lasers providing a scale in the images, a tether-management system (TMS), a winch, and the board units. All cameras used the same main lens and could be tilted. Videos were recorded in Betacam-format. Videos were uploaded for documentation reasons independently of partly low quality due to a ROV driving strategy responding to varying environmental conditions such as sunlight and turbidity. Photographs along the same ROV-transect are available at https://doi.org/10.1594/PANGAEA.250429. J. Gutt: mailto:Julian.Gutt@awi.de
DOI: 10.1594/pangaea.787948
title: (Table T4) Anisotropy of magnetic susceptibility for ODP Site 172-1061

description: DEPTH, sediment is given in mbsf.
DOI: 10.1594/pangaea.954676
title: Other measurements at 10 m from station Bondville (2021-10)
DOI: 10.1594/pangaea.897647
title: Microwave-induced self-organization in mineral systems. II. Prussian blue (conentrated sol; 2.45 GHz; 450 W; 2 min). Erosion and reticulation

description: In this dataset cycle we consider a multifactor nature of the self-organization procees of soft matter dissipative microstructures from the iron-containing colloidal precursors with different particle size under microwave irradiation. The resulting structures' morphology determined by the dehydration-aggregation procees under the microwave field, as well as their phase state, chemical composition and the degree of crystallinity, are shown to be dependent on the irradiation time, the microwave field power and the particle size of the chemical "precursor".
DOI: 10.1594/pangaea.954674
title: Ultra-violet measurements from station Bondville (2021-10)
DOI: 10.1594/pangaea.896763
title: CICE output from Global Ocean Forecast System (GOFS) 3.1 for 2018120712

description: INITIALIZATION: 2018120712FORECASTS: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.899401
title: CICE output from Global Ocean Forecast System (GOFS) 3.1 for 2019022412

description: INITIALIZATION: 2019022412FORECASTS: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.499371
title: Physical oceanography from BT during cruise U90XX07120B_1956
DOI: 10.1594/pangaea.898377
title: Temporal continuos drone-based thermal infrared data

description: The data are raw data recorded during a drone flight. Yet, instead of flying the drone hovered over a predefined location (31.576516°, 35.415775°) recording the very same location for a period for 167 seconds at approximately 5Hz. Thus, the data consist of 670 single thermal infrared images recorded with a long-wave infrared camera core (FLIR Tau2), which is an uncooled VOx Microbolometer with a 19mm lens and a 640x512 focal plane array. The intention was to exploit spatiotemporal continuous thermal infrared data to outline and investigate submarine groundwater discharge and deduce possible discharge behavior. The here presented raw data are the basis for the study Mallast, U. and Siebert, C.: Combining continuous spatial and temporal scales for SGD investigations using UAV-based thermal infrared measurements, Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2018-361, in review, 2018.
description: Supplement to: Mallast, Ulf; Siebert, Christian (2019): Combining continuous spatial and temporal scales for SGD investigations using UAV-based thermal infrared measurements. Hydrology and Earth System Sciences, 23(3), 1375-1392
DOI: 10.1594/pangaea.897646
title: Microwave-induced self-organization in mineral systems. I. Prussian blue (2.45 GHz; 450 W; 3 min)

description: In this dataset cycle we consider a multifactor nature of the self-organization processes of soft matter dissipative microstructures from the iron-containing colloidal precursors with different particle size under microwave irradiation. The resulting structures' morphology determined by the dehydration-aggregation processes under the microwave field, as well as their phase state, microchemical composition and the degree of crystallinity, are shown to be dependent on the irradiation time, the microwave field power and the particle size and the layer thickness of the chemical precursor.
DOI: 10.1594/pangaea.722417
title: Other measurements at 10 m from station Goodwin Creek (2003-02)

description: Version 2, 2009-06-24
DOI: 10.1594/pangaea.896646
title: Physical oceanography from mooring KPO_1123

description: mooring_id = kpo_1123latitude = 59.2155longitude = -47.0818principal_investigator = Johannes Karstenseninstrument = Label:kpo_1123_01 File:OS_OSNAP-10692_KPO_1123_DSOW4_201408_D_MCTD_OSNAPstyleOceanSITES.nc Type: Seabird MicroCat SN:10692instrument = Label:kpo_1123_02 File:OS_OSNAP-2620901_KPO_1123_DSOW4_201408_D_CM_OSNAPstyleOceanSITES.nc Type: Nortek Aquadopp SN:2620901instrument = Label:kpo_1123_03 File:OS_OSNAP-10698_KPO_1123_DSOW4_201408_D_MCTD_OSNAPstyleOceanSITES.nc Type: Seabird MicroCat SN:10698instrument = Label:kpo_1123_04 File:OS_OSNAP-2620909_KPO_1123_DSOW4_201408_D_CM_OSNAPstyleOceanSITES.nc Type: Nortek Aquadopp SN:2620909
DOI: 10.1594/pangaea.954675
title: Radiosonde measurements from station Bondville (2021-10)

description: Start location: Lincoln, IL; Distance from radiation site: 82 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.892668
title: Chronostratigraphy of short monoliths (FRK IV) blanket bog at Connemara National Park, Letterfrack, Co. Galway, Ireland
DOI: 10.1594/pangaea.900427
title: Ceilometer raw data measured at Neumayer Station (2018-03), links to files

description: The ceilometer is mounted on the roof of the station building, the height offset was set to 25m. This offset only affects the detected cloud levels, not the full backscatter profile.
DOI: 10.1594/pangaea.747789
title: Meteorological observations during CALCUTTA cruise from Sauger Roads to The Downs started at 1804-03-11
DOI: 10.1594/pangaea.919664
title: Seismic refraction survey on the eastern flank of the Juan de Juca Ridge during SONNE cruise SO111

description: During RV SONNE cruise SO111, five 50 to 60 km long seismic refraction and wide-angle profiles were shot on the eastern flank of the Juan de Fuca Ridge near 48°N, southwest of Vancouver Island, Northeastern Pacific. All profiles were shot in 1996 and run parallel to the strike of the spreading centre and sampled crust created 0.5 Myr to 2.6 Myr ago. In total, 24 ocean-bottom-hydrophones (OBH) were deployed to record shots fired using a single low-frequency airgun source (main source frequency of 4-12 Hz). 23 OBH provided data useful for geophysical data analyses.
description: Seismic data are in SEGY format are reduced with 6 km/s.
DOI: 10.1594/pangaea.748465
title: Meteorological observations during DEDAIGNEUSE cruise from Amboyna to Trincomalee started at 1803-04-22
DOI: 10.1594/pangaea.898025
title: CICE output from Global Ocean Forecast System (GOFS) 3.1 for 2019012512

description: INITIALIZATION: 2019012512FORECASTS: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.892672
title: Pollen counts, profile (FRK II) from Connemara National Park, Letterfrack, Co. Galway, Ireland

description: Analyst: Máire BowlerLaboratory: Palaeoenvironmental Research Unit, NUI Galway, Galway, IrelandData analysis completed: 1986Sampling in field: Date of sampling: 1984-09-01. Cut from a clean peat bank; top of peat bank to cutover surface: 1.2 m; ca. 2.4 m of peat below (not cutover) - this extracted by digging a hole and removing a long monolith. Uppermost section: top to 1.14 m cut from bank left by turfcutters. Hole dug and took to depth of 3.5 m in 3 sections. Lowest deposit (in a small depression beside a boulder). sample density: variable; mainly 4 cm intervals. Pollen preparation: Lycopodium spore suspension of know concentration added; acetolysis, mounted in glycerine. Cereal-type pollen differentiated using Beug (1961) criteria (37 um taken as cutoff point; but only pollen grains 40 um and greater included in cereal-type). Pollen nomenclature generally follows Moore et al. 1991. &lt;1 = recorded outside the pollen counts (most samples searched for additional taxa). Distinction between Myrica and Corylus not regarded as reliable; individual taxa and combined counts given. Charcoal particles ≥37 um counted during routine pollen counting.
DOI: 10.1594/pangaea.898023
title: CICE output from Global Ocean Forecast System (GOFS) 3.1 for 2019012312

description: INITIALIZATION: 2019012312FORECASTS: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.919828
title: Seabed photographs taken along OFOBS profile HE502_6-1 during HEINCKE cruise HE502

description: The OFOBS system consisted of a towed underwater camera system equipped with both a high-resolution photo-camera (iSiTEC, CANON EOS 5D Mark III) and a high-definition video-camera (iSiTEC, Sony FCB-H11) as well as an integrated sidescan sonar system. The cameras were mounted on a steel frame (140L x 92W x 135H cm), together with two strobe lights (iSiTEC UW-Blitz 250, TTL driven), three laser pointers spaced with a distance of 50 cm used to estimate the size of seafloor structures, four LED lights, and a USBL positioning system (Posidonia) to track the position of the OFOBS during deployments, with additional positioning information provided by the integrated INS and DVL systems, which was undergoing testing during this cruise.In this dataset seabed photos from a height of approximately 60 cm from the seafloor, depicting an area of approximately 1.5 m**2, with variations depending on the actual height above ground of the system. Conditions were not optimal, with many particles in the water and considerable ship heave.
DOI: 10.1594/pangaea.895337
title: Permanent transect BTN_PNRA_T2 (revisited in 2017) at Tethys Bay (Terra Nova Bay, Ross Sea, Antarctica)

description: This dataset is composed by 619 still frames extracted from a diver-based video survey, recorded in 14th November 2017 during a combined field event between the New Zealand Researchers of Waikato University and the Korean Researchers of Korean Polar Research Institute (KOPRI). The frames depict the permanent transect "BTN_PNRA_T2" established in 2015, in the context of the XXXI Italian National Antarctic Program (PNRA) expedition. The diving site is named "Zecca" (coordinates: 74° 41.410' S, 164° 06.233 E) and the transect is at 19.4 m of depth.
DOI: 10.1594/pangaea.900488
title: Radiosonde raw data from tandem soundings at Neumayer Station (2018-12), links to files

description: At Neumayer station the transition of sonde type from Vaisala RS92-SGP to RS41-SGP is controlled by tandem soundings starting in July 2018. Each file in this dataset was acquired together with the corresponding data file in doi:10.1594/PANGAEA.900465.
DOI: 10.1594/pangaea.893451
title: CICE output from Global Ocean Forecast System (GOFS) 3.1 for 2018020312

description: INITIALIZATION: 2018020312FORECASTS: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" ;