cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.935598
title: Multibeam bathymetry raw data (Kongsberg EM 122 entire dataset) of RV METEOR during cruise M154/1

description: Multibeam bathymetry raw data was recorded in the Atlantic during cruise M154/1 that took place between 2019-04-03 and 2019-04-25. The data was collected using the ship's own Kongsberg EM 122. This data is part of the DAM (German Marine Research Alliance) project Underway Research Data. Sound velocity profiles (SVP) were applied on the data for calibration. SVP data are part of this dataset publication. Please see the cruise report for details.
description: These data should not be used for navigational purposes.
DOI: 10.1594/pangaea.945365
title: ADCP current measurements (38 kHz) during RV MARIA S. MERIAN cruise MSM103

description: Upper-ocean velocities along the cruise track of RV MARIA S. MERIAN cruise MSM103 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 16.0 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 (0.50° +/- 0.7353°) and scale factor (1.0006 +/- 0.0160) 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; 1.0 m/s, rms(UC_z) or rms(VC_z) &gt; 0.3.
DOI: 10.1594/pangaea.935640
title: ADCP current measurements (75 kHz) during RV SONNE cruise SO280

description: Upper-ocean velocities along the cruise track of Sonne cruise SO280 were continuously collected by a vessel-mounted Teledyne RD Instruments 75 kHz Ocean Surveyor ADCP. The transducer was located at 6.0 m below the water line. The instrument was operated in narrowband mode with 8 m bins and a blanking distance of 8.0 m, while 100 bins were recorded using a pulse of 1.44 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 (-0.85° +/- 0.8385°) and scale factor (1.0000 +/- 0.0131) of the Ocean Surveyor signal. The average interval was set to 60 s.
description: Velocity quality flagging is based on following threshold criteria: abs(UC) or abs(VC) &gt; 2.0 m/s, rms(UC_z) or rms(VC_z) &gt; 0.3.
DOI: 10.1594/pangaea.973859
title: Continuous optical chlorophyll-a and turbidity data along R/V SONNE cruise SO298

description: Underway optical chlorophyll-a and turbidity data were collected along the cruise track with Sea-Bird Scientific ECO FLNTU sensors installed within two autonomous measurement systems, called self-cleaning monitoring boxes (SMBs). The SMBs measure alternatingly. While one box is measuring, the other one is being cleaned. The water inlet for the SMBs is at about 4 m below sea surface. Observed chlorophyll-a and turbidity data were both quality controlled and the chlorophyll-a data was additionally calibrated using satellite matchups with the GlobColour CHL1 product. Reference data from water samples were collected by Niskin bottles of the CTD water sampler at 5 m depth or by a tow fish at 2-4 m depth during day time. Chlorophyll-a was determined onboard using a Turner fluorometer as well as in the lab on land via HPLC. The time series shows strong diel cycles connected to non-photochemical quenching. The phytoplankton fluorescence signal is reduced due to high light exposure. It was out of the scope of the applied processing routine to flag or correct for these effects. The daytime reference samples can therefore not be used for calibration of the chlorophyll-a fluorescence data (chlorophyll-a values based on manufacturer calibration). Satellite data was used instead. Details on all quality control steps, the calibration, and comparison with reference sample data can be found in the Data Processing Report. The resulting data set contains the original data, the calibrated data (in case of chlorophyll-a) and corresponding quality flags achieved by the quality control algorithm. The data source is given through the name of the active SMB. The data set contains data during transit time and station work. We recommend to use ship's speed to filter for only transit data.
DOI: 10.1594/pangaea.935638
title: ADCP current measurements (38 kHz) during RV SONNE cruise SO280

description: Upper-ocean velocities along the cruise track of Sonne cruise SO280 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 16.0 m, while 50 bins were recorded using a pulse of 2.88 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 (0.03° +/- 0.8820°) and scale factor (1.0025 +/- 0.0133) of the Ocean Surveyor signal. The average interval was set to 60 s.
description: Velocity quality flagging is based on following threshold criteria: abs(UC) or abs(VC) &gt; 2.0 m/s, rms(UC_z) or rms(VC_z) &gt; 0.3.
DOI: 10.1594/pangaea.974222
title: Continuous thermosalinograph oceanography along RV METEOR cruise track M201

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 and salinity. Finally, TSG1 was chosen for publication. For details to all processing steps see Data Processing Report.
DOI: 10.1594/pangaea.974223
title: Continuous thermosalinograph oceanography along RV METEOR cruise track M202

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 (06M320240721), i.e. since 2024-07-21T00:00:00). Value added to salinity data TSG1 = -0.0004998*tim+0.017765. Value added to salinity data TSG2 = -0.0002846*tim+0.024270.
DOI: 10.1594/pangaea.974233
title: Shipboard ADCP current measurements (38 kHz) during RV METEOR cruise M201

description: Current velocities of the upper water column along the cruise track of R/V Meteor cruise M201 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 8.00 m, and a total of 80 bins, covering the depth range between 29.0 m and 1293.0 m. Attitude data from the ship's motion reference unit were used by the data acquisition software VmDAS internally to convert ADCP beam velocities to geographic coordinates. The Python toolbox OSADCP (version 2.0.0) was used for data post-processing. Single-ping data were screened for bottom signals and, where appropriate, a bottom mask was manually processed. Acoustic Interferences were identified based on outliers in the ADCP echo intensity data. Echo intensity data were cleaned accordingly and affected velocity cells were flagged to be removed prior ensemble-averaging. The ship's velocity was calculated from position fixes obtained by the Global Navigation Satellite System (GNSS), taking into account lever arms of ADCP transducer and GNSS antenna. Accuracy of the derived water 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 processing included water track calibration of the misalignment angle (0.1241° +/- 0.6306°) and scale factor (1.0030 +/- 0.0100) of the measured velocities. The velocity data were averaged in time using an average interval of 180 s. Depth cells with ensemble-averaged percent-good values below 25% are marked as 'bad data'.
DOI: 10.1594/pangaea.974225
title: Continuous thermosalinograph oceanography along RV ALKOR cruise track AL618

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 with water samples from 4m depth (tim is the time in days since Expocode of this cruise (06AK20240818), i.e. since 2024-08-18T00:00:00): Value added to salinity data = -0.0038328*tim+0.14874.
DOI: 10.1594/pangaea.974234
title: Shipboard ADCP current measurements (75 kHz) during RV METEOR cruise M201

description: Current velocities of the upper water column along the cruise track of R/V Meteor cruise M201 were collected by a vessel-mounted 75 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 8.00 m, a blanking distance of 4.00 m, and a total of 100 bins, covering the depth range between 17.0 m and 809.0 m. Attitude data from the ship's motion reference unit were used by the data acquisition software VmDAS internally to convert ADCP beam velocities to geographic coordinates. The Python toolbox OSADCP (version 2.0.0) was used for data post-processing. Single-ping data were screened for bottom signals and, where appropriate, a bottom mask was manually processed. Acoustic Interferences were identified based on outliers in the ADCP echo intensity data. Echo intensity data were cleaned accordingly and affected velocity cells were flagged to be removed prior ensemble-averaging. The ship's velocity was calculated from position fixes obtained by the Global Navigation Satellite System (GNSS), taking into account lever arms of ADCP transducer and GNSS antenna. Accuracy of the derived water 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 processing included water track calibration of the misalignment angle (-46.3800° +/- 0.6261°) and scale factor (1.0031 +/- 0.0102) of the measured velocities. The velocity data were averaged in time using an average interval of 180 s. Depth cells with ensemble-averaged percent-good values below 25% are marked as 'bad data'.
DOI: 10.57760/sciencedb.33416
title: Crude Oil Price and other security market factors
title: Crude Oil Price and other security market factors

description: Data of crude oil price and factors of security market
description: Data of crude oil price and factors of security market
DOI: 10.1594/pangaea.974224
title: Continuous thermosalinograph oceanography along RV ALKOR cruise track AL575

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. No salinity calibration was performed. For details to all processing steps see Data Processing Report.
DOI: 10.1594/pangaea.974283
title: Shipboard ADCP current measurements (75 kHz) during RV SONNE cruise SO305

description: Current velocities of the upper water column along the cruise track of R/V Sonne cruise SO305 were collected by a vessel-mounted 75 kHz RDI Ocean Surveyor ADCP. The ADCP transducer was located at 6.0 m below the water line. The instrument was operated in narrowband mode (WM10) with a bin size of 8.00 m, a blanking distance of 4.00 m, and a total of 100 bins, covering the depth range between 18.0 m and 810.0 m. Attitude data from the ship's motion reference unit were used by the data acquisition software VmDAS internally to convert ADCP beam velocities to geographic coordinates. The Python toolbox OSADCP (version 2.0.0) was used for data post-processing. Acoustic Interferences were identified based on outliers in the ADCP echo intensity data. Echo intensity data were cleaned accordingly and affected velocity cells were flagged to be removed prior ensemble-averaging. The ship's velocity was calculated from position fixes obtained by the Global Navigation Satellite System (GNSS), taking into account lever arms of ADCP transducer and GNSS antenna. Accuracy of the derived water 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 processing included water track calibration of the misalignment angle (-0.1314° +/- 0.5800°) and scale factor (1.0004 +/- 0.0098) of the measured velocities. The velocity data were averaged in time using an average interval of 60 s. Depth cells with ensemble-averaged percent-good values below 25% are marked as 'bad data'.
DOI: 10.1594/pangaea.974291
title: Shipboard ADCP current measurements (38 kHz) during RV MARIA S. MERIAN cruise MSM56

description: Current velocities of the upper water column along the cruise track of R/V Maria S. Merian cruise MSM56 were collected by a vessel-mounted 38 kHz RDI Ocean Surveyor ADCP. The ADCP transducer was located at 6.0 m below the water line. The instrument was operated in narrowband mode (WM10) with a bin size of 32.00 m, a blanking distance of 16.00 m, and a total of 50 bins, covering the depth range between 54.0 m and 1622.0 m. Attitude data from the ship's motion reference unit were used by the data acquisition software VmDAS internally to convert ADCP beam velocities to geographic coordinates. The Python toolbox OSADCP (version 2.0.0) was used for data post-processing. Single-ping data were screened for bottom signals and, where appropriate, a bottom mask was manually processed. Acoustic Interferences were identified based on outliers in the ADCP echo intensity data. Echo intensity data were cleaned accordingly and affected velocity cells were flagged to be removed prior ensemble-averaging. The ship's velocity was calculated from position fixes obtained by the Global Navigation Satellite System (GNSS), taking into account lever arms of ADCP transducer and GNSS antenna. Accuracy of the derived water 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 processing included water track calibration of the misalignment angle (-0.8276° +/- 0.6763°) and scale factor (0.9962 +/- 0.0127) of the measured velocities. The velocity data were averaged in time using an average interval of 180 s. Depth cells with ensemble-averaged percent-good values below 50% are marked as 'bad data'. Furthermore, the time series of cell 1 to 4 are flagged as 'potentially correctable bad data' because of velocities biases most likely caused by transducer ringing.
DOI: 10.17026/ar/4m5pks
title: PAN-00182009 - eye brooch D

description: &lt;p&gt;This find is registered at Portable Antiquities of the Netherlands with number PAN-00182009&lt;/p&gt;
description: Modified: 2025-11-02T11:39:48+01:00
DOI: 10.1594/pangaea.919058
title: ADCP current measurements (75 kHz) during Maria S. Merian cruise MSM88/1

description: Upper-ocean velocities along the cruise track of Maria S. Merian cruise MSM88/1 were continuously collected by a vessel-mounted Teledyne RD Instruments 75 kHz Ocean Surveyor ADCP. The transducer was located at 6 m below the water line. The instrument was operated in narrowband mode with 8 m bins and a blanking distance of 8 m, while 100 bins were recorded using a pulse of 1.45 seconds. 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 acquistion 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. The ADCP data were processed using the Python-based DAM-ADCP software, adapted from the OSSI toolbox developed by GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel. The average interval was set to 60 seconds. Data post-processing included water track calibration of the misalignment angle (-47.1499° +/- 0.777°) and the amplitude (1.0106 +/- 0.0144) of the Ocean Surveyor signal. Velocity quality flagging is based on following threshold criteria: abs(UC) or abs(VC) &gt; 2 m/s, rms(UC_z) or rms(VC_z) &gt; 0.3.
DOI: 10.1594/pangaea.974298
title: Shipboard ADCP current measurements (75 kHz) during RV SONNE cruise SO307

description: Current velocities of the upper water column along the cruise track of R/V Sonne cruise SO307 were collected by a vessel-mounted 75 kHz RDI Ocean Surveyor ADCP. The ADCP transducer was located at 6.0 m below the water line. The instrument was operated in narrowband mode (WM10) with a bin size of 8.00 m, a blanking distance of 8.00 m, and a total of 100 bins, covering the depth range between 22.0 m and 814.0 m. Attitude data from the ship's motion reference unit were used by the data acquisition software VmDAS internally to convert ADCP beam velocities to geographic coordinates. The Python toolbox OSADCP (version 2.0.0) was used for data post-processing. Single-ping data were screened for bottom signals and, where appropriate, a bottom mask was manually processed. Acoustic Interferences were identified based on outliers in the ADCP echo intensity data. Echo intensity data were cleaned accordingly and affected velocity cells were flagged to be removed prior ensemble-averaging. The ship's velocity was calculated from position fixes obtained by the Global Navigation Satellite System (GNSS), taking into account lever arms of ADCP transducer and GNSS antenna. Accuracy of the derived water 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 processing included water track calibration of the misalignment angle (-45.1454° +/- 0.7491°) and scale factor (0.9976 +/- 0.0120) of the measured velocities. The velocity data were averaged in time using an average interval of 180 s. Depth cells with ensemble-averaged percent-good values below 25% are marked as 'bad data'.
DOI: 10.1594/pangaea.974280
title: Shipboard ADCP current measurements (38 kHz) during RV METEOR cruise M202

description: Current velocities of the upper water column along the cruise track of R/V Meteor cruise M202 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 32.00 m, a blanking distance of 16.00 m, and a total of 55 bins, covering the depth range between 53.0 m and 1781.0 m. Attitude data from the ship's motion reference unit were used by the data acquisition software VmDAS internally to convert ADCP beam velocities to geographic coordinates. The Python toolbox OSADCP (version 2.0.0) was used for data post-processing. Single-ping data were screened for bottom signals and, where appropriate, a bottom mask was manually processed. Acoustic Interferences were identified based on outliers in the ADCP echo intensity data. Echo intensity data were cleaned accordingly and affected velocity cells were flagged to be removed prior ensemble-averaging. The ship's velocity was calculated from position fixes obtained by the Global Navigation Satellite System (GNSS), taking into account lever arms of ADCP transducer and GNSS antenna. Accuracy of the derived water 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 processing included water track calibration of the misalignment angle (0.0492° +/- 0.5431°) and scale factor (1.0041 +/- 0.0107) of the measured velocities. The velocity data were averaged in time using an average interval of 60 s. Depth cells with ensemble-averaged percent-good values below 25% are marked as 'bad data'.