cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.959838
title: Multibeam bathymetry raw data (Kongsberg EM 122 entire dataset) of RV METEOR during cruise M99

description: Multibeam bathymetry raw data using the ship's own Kongsberg EM 122 multibeam echosounder was not continuously recorded during RV METEOR cruise M99. Data was recorded on 3 days between 2013-08-03 and 2013-08-05. This dataset contains a survey in the South Atlantic Ocean west of Namibia. The approximate average depth of the entire dataset is around 4300m.The data are archived at the Federal Maritime and Hydrographic Agency of Germany (Bundesamt für Seeschifffahrt und Hydrographie, BSH) and provided to PANGAEA database for data curation and publication. Ancillary sound velocity profiles (SVP) files from the cruise are archived at the BSH, thus SVP files are added to this dataset. Data analysis of the multibeam raw data revealed that SVP has not been changed during the survey.This publication is conducted within the efforts of the German Marine Research Alliance in the core area Data management and Digitalization (Deutsche Allianz Meeresforschung, DAM).Data are unprocessed and therefore contains incorrect depth measurements (artifacts) without further processing. Note that refraction errors can be expected due to the lack of proper SVP. Overall, it appears that the data quality is rather good since the gridded hillshade data showed relatively few obstacles.Data can be processed e.g. with the open source software package MB-System (Caress, D. W., and D. N. Chayes, MB-System: Mapping the Seafloor, http://www.mbari.org/products/research-software/mb-system/, 2022).
description: These data should not be used for navigational purposes.Data publishing was realized by Daniel Damaske, MARUM - Center for Marine Environmental Sciences (University Bremen).
DOI: 10.1594/pangaea.962558
title: Continuous thermosalinograph oceanography along RV METEOR cruise track M157

description: Underway temperature and salinity data was collected along the cruise track with two autonomous thermosalinograph (TSG) systems, each consisting of a SBE21 TSG together with a SBE38 Thermometer. Both systems worked independent from each other throughout the cruise. While temperature is taken at the water inlet in about 5 m depth, salinity is estimated within the interior TSG from conductivity and interior temperature. Neither temperature nor salinity were performed. For details to all processing steps see Data Processing Report.
DOI: 10.15468/dl.5ncge2
title: Occurrence Download

description: A dataset containing 8570809 species occurrences available in GBIF matching the query:
{
 "and" : [
 {
 "and" : [
 "HasGeospatialIssue is false",
 "HasCoordinate is true",
 "OccurrenceStatus is Present",
 {
 "not" : {
 "BasisOfRecord" : [
 "is one of (Fossil, Living Specimen)"
 ]
 }
 }
 ]
 },
 "DatasetKey is iNaturalist Research-grade Observations",
 "Country is United States of America",
 "Year is greater than or equal to 2015",
 "Year is less than or equal to 2019"
 ]
}

 The dataset includes 8570809 records from 1 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0048393-251120083545085/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.958530
title: Multibeam bathymetry raw data (Kongsberg EM710 entire dataset) of RV METEOR during cruise M104

description: Multibeam bathymetry raw data using the ship's own Kongsberg EM 710 multibeam echosounder was not continuously recorded during RV METEOR cruise M104. Data was recorded on 4 days between 2014-02-23 and 2014-02-27. This dataset contains a survey west of Namibia in the South Atlantic Ocean. The approximate average depth of the entire dataset is around 600m, covering parts of the the continental shelf and parts of the continental slope.The data are archived at the Federal Maritime and Hydrographic Agency of Germany (Bundesamt für Seeschifffahrt und Hydrographie, BSH) and provided to PANGAEA database for data curation and publication. No ancillary sound velocity profiles (SVP) files from the cruise are archived at the BSH, thus no SVP files are added to this dataset. Data analysis of the multibeam raw data revealed that SVP has not been changed during the survey.This publication is conducted within the efforts of the German Marine Research Alliance in the core area 'Data management and Digitalization' (Deutsche Allianz Meeresforschung, DAM).Data are unprocessed and therefore contains incorrect depth measurements (artifacts) without further processing. Note that refraction errors can be expected due to the lack of proper SVP. Overall, it appears that the data quality is rather moderate in the shelf area since the gridded hillshade data showed relatively few obstacles. However, in the deeper areas at the continental slope the data quality is really bad. The reason for this is unknown.Data can be processed e.g. with the open source software package MB-System (Caress, D. W., and D. N. Chayes, MB-System: Mapping the Seafloor, http://www.mbari.org/products/research-software/mb-system/, 2022).
description: These data should not be used for navigational purposes.Data publishing was realized by Daniel Damaske, MARUM - Center for Marine Environmental Sciences (University Bremen).
DOI: 10.1594/pangaea.922983
title: Multibeam bathymetry raw data (Kongsberg EM 122 entire dataset) of RV METEOR during cruise M86/1c

description: Multibeam bathymetry raw data using the ship's own Kongsberg EM 122 multibeam echosounder was almost continuously recorded during RV METEOR cruise M86/1c. Data were recorded on 11 days between 2011-12-12 and 2011-12-23. The approximate average depth of the entire dataset is around 3700m.The cruise took place between 2011-12-06 and 2011-12-23 in the eastern North Atlantic Ocean. The main aim of this cruise was the calibration of the multibeam systems of RV METEOR at Gettysburg seamount.The data are archived at the Federal Maritime and Hydrographic Agency of Germany (Bundesamt für Seeschifffahrt und Hydrographie, BSH) and provided to PANGAEA database for data curation and publication. Ancillary sound velocity profiles (SVP) from the cruise are archived at the BSH, thus added to this dataset. Data analysis of the mulitbeam raw data reveled that SVP has been changed on several occasions during the cruise.This publication is conducted within the efforts of the German Marine Research Alliance in the core area "Data management and Digitalization" (Deutsche Allianz Meeresforschung, DAM).Data are unprocessed and therefore may contain incorrect depth measurements (artifacts) without further processing.Data can be processed e.g. with the open source software package MB-System (Caress, D. W., and D. N. Chayes, MB-System: Mapping the Seafloor, http://www.mbari.org/products/research-software/mb-system/, 2021).
description: These data should not be used for navigational purposes.Data publishing was realized by Daniel Damaske & Ines Vejzovic, MARUM - Center for Marine Environmental Sciences (University Bremen).
DOI: 10.1594/pangaea.958527
title: Multibeam bathymetry raw data (Kongsberg EM 122 entire dataset) of RV METEOR during cruise M104

description: Multibeam bathymetry raw data using the ship's own Kongsberg EM 122 multibeam echosounder was almost continuously recorded during RV METEOR cruise M104. Data was recorded on 20 days between 2014-02-22 and 2014-03-13. This dataset contains a survey during the transit from Walvis Bay, Namibia to Mindelo, CapeVerde in the Atlantic Ocean. The approximate average depth of the entire dataset is around 4500m.The data are archived at the Federal Maritime and Hydrographic Agency of Germany (Bundesamt für Seeschifffahrt und Hydrographie, BSH) and provided to PANGAEA database for data curation and publication. No ancillary sound velocity profiles (SVP) files from the cruise are archived at the BSH, thus no SVP files are added to this dataset. However, data analysis of the multibeam raw data revealed that SVP has been changed during the survey.This publication is conducted within the efforts of the German Marine Research Alliance in the core area 'Data management and Digitalization' (Deutsche Allianz Meeresforschung, DAM).Data are unprocessed and therefore contains incorrect depth measurements (artifacts) without further processing. Note that refraction errors can be expected due to the lack of proper SVP. Overall, it appears that the data quality is rather good since the gridded hillshade data showed relatively few obstacles.Data can be processed e.g. with the open source software package MB-System (Caress, D. W., and D. N. Chayes, MB-System: Mapping the Seafloor, http://www.mbari.org/products/research-software/mb-system/, 2022).
description: These data should not be used for navigational purposes.Data publishing was realized by Daniel Damaske, MARUM - Center for Marine Environmental Sciences (University Bremen).
DOI: 10.1594/pangaea.961671
title: ADCP current measurements (38 kHz) during RV METEOR cruise M186/2

description: Current velocities of the upper water column along the cruise track of R/V Meteor III cruise MET186/2 were collected by a vessel-mounted 38 kHz RDI Ocean Surveyor ADCP. The ADCP transducer was located at 5.0 m below the water line. The instrument was operated in narrowband mode (WM10) with a bin size of 16.00 m, a blanking distance of 16.00 m, and a total of 100 bins, covering the depth range between 37.0 m and 1621.0 m. Heading, pitch and roll data from the ship's motion reference unit and the navigation data from the Global Positioning systems were used by the data acquisition software VmDAS internally to convert ADCP velocities into earth coordinates. Measured velocities and bin-depth mapping were corrected due to occasional incorrect temperature measurements at the transducer that affected the sound velocity calculation. Corrected sound velocity values were derived using temperature measured by the ship's thermosalinograph. The ship's velocity was calculated from position fixes obtained by the Global Positioning System (GPS). Accuracy of the ADCP velocities mainly depends on the quality of the position fixes and the ship's heading data. Further errors stem from a misalignment of the transducer with the ship's centerline. Data post-processing included water track calibration of the misalignment angle (-44.9046° +/ 0.4750°) and scale factor (1.0043 +/- 0.0085) of the Ocean Surveyor signal. The velocity data were averaged in time using an average interval of 60 s. Velocity quality flagging is based on following threshold criteria: abs(UC) or abs(VC) &gt; 1.5 m/s, rms(UC_z) or rms(VC_z) &gt; 0.3.
DOI: 10.1594/pangaea.945800
title: ADCP current measurements (38 kHz) during RV MARIA S. MERIAN cruise MSM102

description: Upper-ocean velocities along the cruise track of RV MARIA S. MERIAN cruise MSM102 were continuously collected by a vessel-mounted Teledyne RD Instruments 38 kHz Ocean Surveyor ADCP. The transducer was located at 6.0 m below the water line. The instrument was operated in narrowband mode with 32 m bins and a blanking distance of 16 m, while 50 bins were recorded using a pulse of 2.87 s. The ship's velocity was calculated from position fixes obtained by the Global Positioning System (GPS). Heading, pitch and roll data from the ship's gyro platforms and the navigation data were used by the data acquisition software VmDas internally to convert ADCP velocities into earth coordinates. Accuracy of the ADCP velocities mainly depends on the quality of the position fixes and the ship's heading data. Further errors stem from a misalignment of the transducer with the ship's centerline. Data post-processing included water track calibration of the misalignment angle (0.40° +/- 0.6886°) and scale factor (1.0008 +/- 0.0494) of the Ocean Surveyor signal. The average interval was set to 120 s.
description: Velocity quality flagging is based on following threshold criteria: abs(UC) or abs(VC) &gt; 1.3 m/s, rms(UC_z) or rms(VC_z) &gt; 0.3.
DOI: 10.1594/pangaea.962921
title: Continuous thermosalinograph oceanography along RV METEOR cruise track M160

description: Underway temperature and salinity data was collected along the cruise track with two autonomous thermosalinograph (TSG) systems, each consisting of a SBE21 TSG together with a SBE38 Thermometer. Both systems worked independent from each other throughout the cruise. While temperature is taken at the water inlet in about 5 m depth, salinity is estimated within the interior TSG from conductivity and interior temperature. Temperature and salinity were calibrated against CTD data from 5 m depth. For details to all processing steps see Data Processing Report.
description: Temperature was calibrated independently for both TSGs against CTD data from 5 m depth. Value added to temperature data TSG1 = -0.003552. Value added to temperature data TSG2 = -0.002632.Salinity was calibrated independently for both TSGs against CTD data from 5 m depth (tim is the time in days since Expocode of this cruise (06M320191123), i.e. since 2019-11-23T00:00:00): Value added to salinity data TSG1 = 0.0018816*tim-0.00555. Value added to salinity data TSG2 = 0.0012664*tim-0.00295.
DOI: 10.1594/pangaea.946377
title: Continuous thermosalinograph oceanography along RV SONNE cruise SO279

description: Underway temperature and salinity data was collected along the cruise track with two autonomous measurement systems, called self-cleaning monitoring boxes (SMBs). Usually, the SMBs are changed after 12 hours. While temperature is taken at the water inlet in about 4 m depth, salinity is estimated within the SMB from conductivity and interior temperature. No calibration was performed, neither for temperature nor for salinity. For details to all processing steps see Data Processing Report.
description: Version 2, 2022-07-15: Previous version doi: 10.1594/PANGAEA.937906 contains data gaps and different quality flagging."
DOI: 10.1594/pangaea.962739
title: Master tracks in different resolutions of METEOR cruise M188, Walvis Bay - Walvis Bay, 2023-03-07 - 2023-04-13

description: Raw data acquired by position sensors on board RV METEOR during expedition M188 were processed to receive a validated master track which can be used as reference of further expedition data. During M188 the motion reference unit Kongsberg SeaTex AS MRU-5 combined with Kongsberg SeaTex AS Seapath 320 and two C and C Technologies GPS receivers C-NAV3050 were used as navigation sensors. Data were downloaded from DAVIS SHIP data base (https://dship.bsh.de) with a resolution of 1 sec. Processing and evaluation of the data is outlined in the data processing report. Processed data are provided as a master track with 1 sec resolution derived from the position sensors' data selected by priority and a generalized track with a reduced set of the most significant positions of the master track.
description: This dataset contains the master track in 10 min resolution, for other resolutions please see "Other version" references.
DOI: 10.1594/pangaea.962672
title: Master tracks in different resolutions of METEOR cruise M187, Walvis Bay - Walvis Bay, 2023-01-25 - 2023-03-04

description: Raw data acquired by position sensors on board RV METEOR during expedition M187 were processed to receive a validated master track which can be used as reference of further expedition data. During M187 the motion reference unit Kongsberg SeaTex AS MRU-5 combined with Kongsberg SeaTex AS Seapath 320 and two C and C Technologies GPS receivers C-NAV3050 were used as navigation sensors. Data were downloaded from DAVIS SHIP data base (https://dship.bsh.de) with a resolution of 1 sec. Processing and evaluation of the data is outlined in the data processing report. Processed data are provided as a master track with 1 sec resolution derived from the position sensors' data selected by priority and a generalized track with a reduced set of the most significant positions of the master track.
description: This dataset contains the master track in 10 min resolution, for other resolutions please see "Other version" references.
DOI: 10.1594/pangaea.962927
title: Continuous thermosalinograph oceanography along RV METEOR cruise track M187

description: Underway temperature and salinity data was collected along the cruise track with two autonomous thermosalinograph (TSG) systems, each consisting of a SBE21 TSG together with a SBE38 Thermometer. Both systems worked independent from each other throughout the cruise. While temperature is taken at the water inlet in about 5 m depth, salinity is estimated within the interior TSG from conductivity and interior temperature. No correction against independent data was performed for temperature. Salinity was calibrated against independent water samples. Finally, TSG1 was chosen for publication. For details to all processing steps see Data Processing Report.
description: Salinity was calibrated independently against water samples from 5 m depth (tim is the time in days since Expocode of this cruise (06M320230125), i.e. since 2023-01-25T00:00:00). Value added to salinity data TSG1 = -0.0021656*tim+0.15411. Value added to salinity data TSG2 = 0.0010045*tim+0.17794.
DOI: 10.1594/pangaea.962710
title: Continuous thermosalinograph oceanography along RV ALKOR cruise track AL573

description: Underway temperature and salinity data was collected along the cruise track with a thermosalinograph (TSG) together with a SBE38 Thermometer. Both systems worked throughout the cruise. While temperature is taken at the water inlet in about 4 m depth, salinity is estimated within the interior TSG from conductivity and interior temperature. No temperature calibration was performed. Salinity was calibrated with independent water samples taken at the water inlet. For details to all processing steps see Data Processing Report.
description: Salinity was calibrated independently against water samples from 4 m depth. Value added to salinity data = 0.014231.
DOI: 10.1594/pangaea.962908
title: Continuous thermosalinograph oceanography along RV MARIA S. MERIAN cruise track MSM109

description: Underway temperature and salinity data was collected along the cruise track with two autonomous measurement systems. Usually, the systems are changed after 6 hours. While temperature is taken at the water inlet in about 6.5 m depth, salinity is estimated within the interior measurement container from conductivity and interior temperature. Neither temperature nor salinity calibration was performed. For details to all processing steps see Data Processing Report.
DOI: 10.1594/pangaea.962910
title: Continuous thermosalinograph oceanography along RV METEOR cruise track M183

description: Underway temperature and salinity data was collected along the cruise track with two autonomous thermosalinograph (TSG) systems, each consisting of a SBE21 TSG together with a SBE38 Thermometer. Both systems worked independent from each other throughout the cruise. While temperature is taken at the water inlet in about 5 m depth, salinity is estimated within the interior TSG from conductivity and interior temperature. No correction against independent data was performed neither for temperature nor for salinity. Finally, TSG2 was chosen for publication. For details to all processing steps see Data Processing Report.
DOI: 10.1594/pangaea.962924
title: Continuous thermosalinograph oceanography along RV METEOR cruise track M186

description: Underway temperature and salinity data was collected along the cruise track with two autonomous thermosalinograph (TSG) systems, each consisting of a SBE21 TSG together with a SBE38 Thermometer. Both systems worked independent from each other throughout the cruise. While temperature is taken at the water inlet in about 5 m depth, salinity is estimated within the interior TSG from conductivity and interior temperature. No correction against independent data was performed for temperature. Salinity was calibrated against independent water samples. Finally, TSG1 was chosen for publication. For details to all processing steps see Data Processing Report.
description: Salinity was calibrated independently against water samples from 5 m depth (tim is the time in days since Expocode of this cruise (06M320221129), i.e. since 2022-11-29T00:00:00). Value added to salinity data TSG1 = 0.00186*tim+0.00898. Value added to salinity data TSG2 = 0.0007235*tim+0.04700.
DOI: 10.1594/pangaea.962717
title: Continuous thermosalinograph oceanography along RV ALKOR cruise track AL594

description: Underway temperature and salinity data was collected along the cruise track with a thermosalinograph (TSG) together with a SBE38 Thermometer. Both systems worked throughout the cruise. While temperature is taken at the water inlet in about 4 m depth, salinity is estimated within the interior TSG from conductivity and interior temperature. No temperature calibration was performed. Salinity was calibrated with independent water samples taken at the water inlet. For details to all processing steps see Data Processing Report.
description: Salinity was calibrated independently against water samples from 4 m depth. Value added to salinity data = 0.145221.
DOI: 10.1594/pangaea.962913
title: Shipboard ADCP current measurements (75 kHz) during RV METEOR cruise M187

description: Current velocities of the upper water column along the cruise track of R/V Meteor III cruise MET187 were collected by a vessel-mounted 75 kHz RDI Workhorse Long Ranger ADCP. The ADCP transducer was located at 5.0 m below the water line. The instrument was operated in broadband mode (WM1) with two different configurations: (1 - corresponding to met_187_vmadcp_75khz_01.nc) bin size: 5.0 m, blanking distance: 2.0 m, number of bins: 128, vertical range: 12.0 m - 647.0 m; (2 - corresponding to met_187_vmadcp_75khz_0[2,3].nc) bin size: 8.0 m, blanking distance: 4.0 m, number of bins: 100, vertical range: 17.0 - 809.0 m. Heading, pitch and roll data from the ship's motion reference unit and the navigation data from the Global Positioning systems were used by the data acquisition software VmDAS internally to convert ADCP velocities into earth coordinates. Single-ping data / ping ensembles were screened for bottom signals and, where appropriate, a bottom mask was manually processed. The ship's velocity was calculated from position fixes obtained by the Global Positioning System (GPS). Accuracy of the ADCP velocities mainly depends on the quality of the position fixes and the ship's heading data. Further errors stem from a misalignment of the transducer with the ship's centerline. For technical reasons, the transducer was lifted from the moonpool on February 18th, 2023. Therefore, two separate calibrations were carried out: Data post-processing included water track calibration of the misalignment angle and scale factor of the Ocean Surveyor signal. For technical reasons, the transducer was lifted from the moonpool on February 18th, 2023. Therefore, two separate calibrations were carried out: prior February 18th, 2023 (corresponding to met_187_vmadcp_75khz_0[1,2].nc): misalignment angle of -41.8717° +/- 0.4333° (0.5755°), scale factor of 1.0001 +/- 0.0064 (0.0079); after February 18th, 2023 (corresponding to met_187_vmadcp_75khz_03.nc): misalignment angle of -41.8071° +/- 0.5600°, scale factor of 0.9971 +/- 0.0074. The velocity data were averaged in time using an average interval of 60 s. Velocity quality flagging is based on following threshold criteria: abs(UC) or abs(VC) &gt; 1.5 m/s, rms(UC_z) or rms(VC_z) &gt; 0.3.