cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.718371
title: Basic measurements of radiation at station Boulder, SURFRAD (1997-11)

description: Version 2, 2009-06-12
DOI: 10.1594/pangaea.664048
title: Oceanography at CTD/bottle station IFREMER_0889
DOI: 10.1594/pangaea.718574
title: Radiosonde measurements from station Boulder, SURFRAD (2002-01)

description: Start location: Denver, CO; Distance from radiation site: 40 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown; Version 2, 2009-06-12
DOI: 10.1594/pangaea.720048
title: Other measurements at 10 m from station Desert Rock (2000-06)

description: Version 2, 2009-06-16
DOI: 10.1594/pangaea.720105
title: Radiosonde measurements from station Desert Rock (2001-08)

description: Version 2, 2009-06-16; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.498500
title: Physical oceanography from BT during cruise U90OT08032B_1976
DOI: 10.1594/pangaea.964805
title: Surface heights at Swiss Camp (West Greenland) in May 2021

description: Since 1991, the first author has been running a project to study ice height change, flow velocity and deformation using GNSS ground measurements at Swiss Camp near the equilibrium line in the western margin of the Greenland Ice Sheet. The data so far came from 12 campaigns in the period 1991 to 2014, i.e. on average every two years. Recently, the HEIM-group has crossed the Greenland Ice Sheet from east to west with sleds and also determined the surface heights in 2021, it was also possible to measure the Swiss Camp area. The measurements in 2021 were made using kinematic GNSS at one-second intervals, which were evaluated using the Precise Point Positioning (PPP) method. With their results, it was now possible to extend the height change to 30 years and thus form a unique long-term time series.
description: The position coordinates refer to a plane, local coordinate system with zero point at gauge 106-99 (position in 1999) with WGS84 coordinates . Latitude 69.568605 N, longitude 49.316930 W.Height reference to EUREF, difference ITRF-EUREF = -1.08 m.Mean snow layer above ice horizon 1.42 m.
DOI: 10.1594/pangaea.494887
title: Physical oceanography during cruise U90XX00025C_1983
DOI: 10.1594/pangaea.722311
title: Ultra-violet measurements from station Goodwin Creek (2000-03)

description: Version 2, 2009-06-24. UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-03.
DOI: 10.1594/pangaea.718804
title: Ultra-violet measurements from station Sioux Falls (2008-06)

description: UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-03.
DOI: 10.1594/pangaea.823010
title: (Table 1) Major and trace elements at DSDP Leg 56 Holes
DOI: 10.1594/pangaea.719977
title: Radiosonde measurements from station Desert Rock (1999-05)

description: Version 2, 2009-06-16; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.679768
title: Mineral composition of sediments from Hole VNIIO-1987-10a drilled in the Barents Sea
DOI: 10.1594/pangaea.911203
title: Grain size of sediment core KGR-3 from the Kimberley coast, north-western Australia

description: Grain sizes were measured using a Malvern Mastersizer 2000F Laser Particle Sizer, after pretreated with 10% H2O2, 10% HCl and 0.05% (NaPO3)6 solution.
DOI: 10.1594/pangaea.496705
title: Physical oceanography from BT during cruise IXXXXB_1975
DOI: 10.1594/pangaea.498958
title: Physical oceanography from BT during cruise U90X008122B_1989
DOI: 10.1594/pangaea.751947
title: Meteorological observations during Santa Gertrudis cruise from Montevideo to Cádiz started at 1794-06-21
DOI: 10.1594/pangaea.884049
title: Phytoplankton size classes derived from pigment data in surface waters along 170°W (South Pacific Ocean) in 2016

description: Phytoplankton size classes or functional types calculated from diagnostic pigments according to Hirata et al. (2011)
DOI: 10.1594/pangaea.906064
title: Monthly wind directional indices based on ships logbooks observations, NI

description: SOURCES: Daily data of wind direction over the English Channel based on direct marine observations derived from Royal Navy ships' logbooks (1685-1870) and ICOADS v3.0 (1750-2014) datasets. DESCRIPTION: The NI is the Directional Indices (DIs) that give a measure of the notherly flow. It is an instrumental-based monthly index defined as the proportion of notherly days per month (in % with respect to the total number of available days for each month)over the English Channel. A notherly day is defined as a day with prevailing wind from the east (wind blowing from the [315, 45)N sector). When only one daily observation was available, the day was classified from the wind direction of that single observation. If several observations per day were available overthe English Channel, a notherly wind day was said to occur when at least a percentage of 36% of the total number of observations of that day corresponded to westerly wind.DATA:NI: Notherly Index (% of days in a month with notherly wind direction with respect to the total number of available (i.e., non missing) days in the month)No: Number of available days (i.e., with at least one wind observation) in a month (in % with respect to the total number of days in the month). Months with no wind direction observation at all in the full month are labeled as missing (-99.9)IMPORTANT NOTE: Please, note that the NI is herein provided regardless the number of observations. Some months have a low number of observations (No &lt; 50 %)
DOI: 10.1594/pangaea.718186
title: Other measurements at 10 m from station Boulder, SURFRAD (2008-01)
DOI: 10.1594/pangaea.476321
title: Hydrochemistry measured on water bottle samples at station NAtl_1981_AN_26N/174

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.602335
title: Time series of water surface temperature at station Isla_santa_maria_b in 2003, Chile
DOI: 10.1594/pangaea.747189
title: Meteorological observations during Admiraal Evertsen cruise from Coastal East India to Coastal East India started at 1817-10-23
DOI: 10.1594/pangaea.964285
title: Expanded measurements from station Ny-Ålesund (2023-11)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.748074
title: Hydrography on standard level calculated from water bottle samples of RV Cape Torrell in 1900
DOI: 10.1594/pangaea.750970
title: Meteorological observations during NOORDBEVELAND cruise from Batavia to Rammekens started at 1759-11-01
DOI: 10.1594/pangaea.864545
title: Other measurements at 10 m from station Fort Peck (2011-11)
DOI: 10.1594/pangaea.664762
title: Oceanography at CTD/bottle station IFREMER_1602
DOI: 10.1594/pangaea.747779
title: Meteorological observations during BUITENZORG cruise from Batavia to the Netherlands started at 1850-11-02
DOI: 10.1594/pangaea.917133
title: 1-Hz PPP displacements at GEONET station 0959 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.494641
title: Physical oceanography during cruise IPO58PB3XXC
DOI: 10.1594/pangaea.495321
title: Water temperature XBT profiles from cruise U31X040271_1967
DOI: 10.1594/pangaea.713193
title: Smear slide analysis of sediment core GeoB6308-3
DOI: 10.1594/pangaea.748667
title: Meteorological observations during Dover Castle cruise from Madas to The Downs started at 1807-10-25
DOI: 10.1594/pangaea.511158
title: Radiosonde at Georg-Forster station on 1988-11-19 12:00h

description: Height of tropopause 8052 m, total ozone 306.4 DU
DOI: 10.1594/pangaea.751267
title: Meteorological observations during PORTLAND cruise from Portsmouth to St. Helena started at 1771-01-12
DOI: 10.1594/pangaea.719025
title: Radiosonde measurements from station Bondville (2006-02)

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.747650
title: Meteorological observations during BELLONA cruise from Coastal Indonesian Archipelago started at 1840-11-04
DOI: 10.1594/pangaea.869685
title: Other measurements at 10 m from station Sioux Falls (2013-01)
DOI: 10.1594/pangaea.879681
title: Other measurements at 10 m from station Sioux Falls (2015-07)
DOI: 10.1594/pangaea.718631
title: Radiosonde measurements from station Boulder, SURFRAD (2003-03)

description: Start location: Denver, CO; Distance from radiation site: 40 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown; Version 2, 2009-06-12
DOI: 10.1594/pangaea.721474
title: Other measurements at 10 m from station Fort Peck (1999-04)

description: Version 2, 2009-06-19
DOI: 10.1594/pangaea.749842
title: Meteorological observations during ISIS cruise from Downs to St. Helena started at 1798-02-18
DOI: 10.1594/pangaea.906063
title: Monthly wind directional indices based on ships logbooks observations, EI

description: SOURCES: Daily data of wind direction over the English Channel based on direct marine observations derived from Royal Navy ships' logbooks (1685-1870) and ICOADS v3.0 (1750-2014) datasets. DESCRIPTION: The EI is the Directional Indices (DIs) that give a measure of the easterly flow. It is an instrumental-based monthly index defined as the proportion of easterly days per month (in % with respect to the total number of available days for each month) over the English Channel. A easterly day is defined as a day with prevailing wind from the east (wind blowing from the [45, 135)ºN sector). When only one daily observation was available, the day was classified from the wind direction of that single observation. If several observations per day were available over the English Channel, a easterly wind day was said to occur when at least a percentage of 44% of the total number of observations of that day corresponded to westerly wind.DATA:EI: Easterly Index (% of days in a month with easterly wind direction with respect to the total number of available (i.e., non missing) days in the month)No: Number of available days (i.e., with at least one wind observation) in a month (in % with respect to the total number of days in the month). Months with no wind direction observation at all in the full month are labeled as missing (-99.9)IMPORTANT NOTE: Please, note that the EI is herein provided regardless the number of observations. Some months have a low number of observations (No &lt; 50 %)
DOI: 10.1594/pangaea.695639
title: Radiosonde measurements from station Sede Boqer (2007-02)

description: Wind speed was multiplied by a factor of 0.1 (2009-08-28). Start location: Bet-Dagan, Israel; Distance from radiation site: 120 km
DOI: 10.1594/pangaea.890515
title: Vertical profiles of suspended sediment concentration collected by CTD in the tidal river part of the Ems estuary, Germany
DOI: 10.1594/pangaea.718299
title: Ultra-violet measurements from station Boulder, SURFRAD (1996-05)

description: Version 2, 2009-06-12. UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-09.
DOI: 10.1594/pangaea.476541
title: Hydrochemistry measured on water bottle samples at station NAtl_1983_6N_37W/56

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.477862
title: Hydrochemistry measured on water bottle samples at station SPac_1970_HH_170W/2

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.718531
title: Other measurements at 10 m from station Boulder, SURFRAD (2001-02)

description: Version 2, 2009-06-12
DOI: 10.1594/pangaea.718196
title: Ultra-violet measurements from station Boulder, SURFRAD (2008-04)

description: UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-09.
DOI: 10.1594/pangaea.718226
title: Radiosonde measurements from station Boulder, SURFRAD (2008-11)

description: Start location: Denver, CO; Distance from radiation site: 40 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.674002
title: Radiosonde measurements from station Boulder (1999-11)

description: Start location: Denver, Colorado, USA; Distance from radiation site: 30 km
DOI: 10.1594/pangaea.720007
title: Ultra-violet measurements from station Desert Rock (1999-09)

description: Version 2, 2009-06-16. UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-08.
DOI: 10.1594/pangaea.719514
title: Ultra-violet measurements from station Bondville (2001-10)

description: Version 2, 2009-06-15. UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-09.
DOI: 10.1594/pangaea.845300
title: Other measurements at 300 m from station Boulder (2012-09)
DOI: 10.1594/pangaea.747564
title: Meteorological observations during AURORA cruise from Kedgeree to St. Helena started at 1801-04-11
DOI: 10.1594/pangaea.749566
title: Meteorological observations during Henriette Clasina cruise from Batavia to Nieuwediep started at 1834-11-17
DOI: 10.1594/pangaea.499456
title: Physical oceanography from BT during cruise U90XX08222B_1975
DOI: 10.1594/pangaea.750006
title: Meteorological observations during KOERIER cruise from Suriname to Curaçao started at 1852-06-08
DOI: 10.1594/pangaea.752405
title: Meteorological observations during SWAN cruise from Halifax to Bermuda started at 1799-12-11
DOI: 10.1594/pangaea.770975
title: Hydrological records from the Vernagtferner Basin - Vernagtbach station, for the year 1982
DOI: 10.1594/pangaea.499520
title: Physical oceanography from BT during cruise U90XX08317B_1984
DOI: 10.1594/pangaea.874015
title: (Table 1, page 86) Chemical composition of ferromanganese crusts from the Waho Shelf, Hawaii Islands

description: Quantitative and qualitative chemical analyses were performed on fourteen manganese nodules and crusts from the Waho Shelf. The analyses showed that submarine weathering has leached several elements, notably Si02, A1203, Na20, CaO and MnO from the hydrated glass surrounding the basaltic seeds of the nodules. The altered glass was enriched in Ti02, MgO, K2O and total Fe. The manganese bands formed on the altered glass were further depleted in Si02, Al203, and similar to the hydrated glass in Na2O and CaO content. The manganese-enriched zones also showed higher TiO2 and NiO than the basaltic seeds, and higher total Fe than pelagic nodules from the North Pacific. Qualitative measurement of Cu, Ni, and Co, showed relative enrichment in the manganese bands. A proposed model for manganese accretion in the Waho Shelf incorporates local submarine weathering of basalts, redistribution of Mn in marine sediments, and an influx of Mn "rain" on the sea floor.
description: Allowance for H2O was made by deduction from other chemical elements assay.From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis..) not present in the NOAA-MMS database.
description: Supplement to: Fein, Charles D; Morgenstein, Maury (1973): Microprobe analysis of manganese crusts from the Hawaiian Archipelago. In: Phase I Report - Inter-University Program of Research on Ferromanganese Deposits of the Ocean Floor. Seabed Assessment Program, IDOE, NSF, Washington D.C., USA - http://catalog.hathitrust.org/Record/005761114 (pdf 733 kB), 85-92
DOI: 10.1594/pangaea.750514
title: Meteorological observations during Lord Walsingham cruise from Java Head to St. Helena started at 1794-04-19
DOI: 10.1594/pangaea.477671
title: Hydrochemistry measured on water bottle samples at station SPac_1967_ET_28S/160

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.674496
title: Radiosonde measurements from Neumayer Station (2004-06)
DOI: 10.1594/pangaea.892355
title: CICE output from Navy Earth System Model (NESM) for 2018062412

description: INITIALIZATION: 2018062412FORECASTS: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.476066
title: Hydrochemistry measured on water bottle samples at station AOS94/31-1

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.958842
title: Nature of agricultural and pastoral activities and main trees in Lake La Thuile catchment over the last 6400 years

description: Method used to produce the sedimentary DNA datasets: DNA sequences were produced by using g (5'-GGGCAATCCTGAGCCAA-3') and h (5'-CCATTGAGTCTCTGCACCTATC-3') primers for plants and MamP007F (5'-CGAGAAGACCCTATGGAGCT-3') and MamP007R (5'-CCGAGGTCRCCCCAACC-3') primers and the human-blocking primer (5'-GGAGCTTTAATTTATTAATGCAAACAGTACCC-3') for mammals. The sequences have been produced by the Illumina technology (HiSeq instrument). The bioinformatic treatment of the sequences was operated applying the Obitool program (Boyer, F. et al. OBITOOLS:aUNIX-inspired software package for DNA metabarcoding. Mol. Ecol. Resour. 16, 176–182 (2016)) and following the procedure described in Giguet-Covex et al. New insights on lake sediment DNA from the catchment: importance of taphonomic and analytical issues on the record quality. Scientific Reports. 9, 14676 (2019) (DOI https://doi.org/10.1038/s41598-019-50339-1). Then, other filtering processing were performed as also described in Giguet-Covex et al. 2019. These second treatments allow for removing 1) taxa assigned to a reference taxon at &lt;95 % of sequence identity, 2) potential contaminations (based on sampling, extraction and PCR controls, and recognition of exotic taxa) and 3) stochastic detections. Several analytical replicates by samples were performed (4 for the plants and 12 for the mammals). Data are presented in number of positive replicates by sample. A replicate is considered as positive if more than 5 sequences are detected.
DOI: 10.1594/pangaea.958847
title: Selected pollen from sediments in Lake La Thuile over the last 7000 years
DOI: 10.1594/pangaea.722212
title: Ultra-violet measurements from station Goodwin Creek (1997-06)

description: Version 2, 2009-06-24. UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-03.
DOI: 10.1594/pangaea.664265
title: Oceanography at CTD/bottle station IFREMER_1106
DOI: 10.1594/pangaea.722222
title: Other measurements at 10 m from station Goodwin Creek (1997-09)

description: Version 2, 2009-06-24
DOI: 10.1594/pangaea.749536
title: Meteorological observations during HARRIER cruise from Spithead to Madras started at 1807-01-13
DOI: 10.1594/pangaea.958871
title: Intensity index of pastoral activities reconstructed from Lake Anterne sediments over the Holocene

description: Method used to calculate the index: This index has been calculated on the basis of pastoral indicators obtained from the DNA metabarcoding approach targeting plants (ruderal/nitrophilous taxa associated with pastoralism) and mammals (for domesticated animals). The selected pastoral indicators, here, are Plantago sp. for plants, and Bos, Ovis and Equus for mammals. They are standardized by calculating a z-score. Then, the index is calculated as the average of all these standardized indicators.Method used to generate sediment DNA datasets: DNA sequences were generated using g (5'-GGGCAATCCTGAGCCAA-3') and h (5'-CCATTGAGTCTCTGCACCTATC-3') primers for plants and MamP007F (5'-CGAGAAGACCCTATGGAGCT-3') and MamP007R (5'-CCGAGGTCRCCCCAACC-3') primers and the human-blocking primer (5'-GGAGCTTTAATTTATTAATGCAAACAGTACCC-3') for mammals. The sequences have been produced by the Illumina technology (HiSeq instrument). The bioinformatic treatment of the sequences was operated applying the Obitool program (Boyer, F. et al. OBITOOLS:aUNIX-inspired software package for DNA metabarcoding. Mol. Ecol. Resour. 16, 176–182 (2016)) and following the procedure described in Giguet-Covex et al. New insights on lake sediment DNA from the catchment: importance of taphonomic and analytical issues on the record quality. Scientific Reports. 9, 14676 (2019) (DOI https://doi.org/10.1038/s41598-019-50339-1). Further filtering treatments were then applied, as also described in Giguet-Covex et al. 2019. These second treatments allow the removal of 1) taxa assigned to a reference taxon at &lt;95 % of sequence identity, 2) potential contaminations (based on sampling, extraction and PCR controls, and recognition of exotic taxa) and 3) stochastic detections. Multiple analytical replicates by samples were performed (8 for both, the plants and mammals). Data are presented in number of positive replicates by sample. A replicate is considered as positive if more than 5 sequences are detected.
DOI: 10.1594/pangaea.752810
title: Meteorological observations during WALPOLE cruise from Portsmouth to Canton started at 1794-06-25