cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.847420
title: Incident irradiance above water and upward radiance below the water surface during L'Atalante cruise ATA03 in the Atlantic Ocean at station 020001

description: The incident irradiance above water Es (lambda) and the upward radiance just below the water surface Lu (lambda,0-) were measured with Satlantic surface reference (SMSR-SeaWiFS Multichannel Surface Reference) in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.847421
title: Incident irradiance above water and upward radiance below the water surface during L'Atalante cruise ATA03 in the Atlantic Ocean at station 026001

description: The incident irradiance above water Es (lambda) and the upward radiance just below the water surface Lu (lambda,0-) were measured with Satlantic surface reference (SMSR-SeaWiFS Multichannel Surface Reference) in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.847422
title: Incident irradiance above water and upward radiance below the water surface during L'Atalante cruise ATA03 in the Atlantic Ocean at station 027001

description: The incident irradiance above water Es (lambda) and the upward radiance just below the water surface Lu (lambda,0-) were measured with Satlantic surface reference (SMSR-SeaWiFS Multichannel Surface Reference) in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz.
DOI: 10.1594/pangaea.847429
title: Profiles of downward irradiance and upward radiance during L'Atalante cruise ATA03 in the Atlantic Ocean at station 018001

description: Vertical profiles of downward irradiance Ed (z,lambda) in and upward radiance Lu (z,lambda) in were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles up to 90 m were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz. The free fall velocity of the SPMR instrument was justified by ballast in such a way that more than 5 spectra were samples per meter.
DOI: 10.1594/pangaea.847430
title: Profiles of downward irradiance and upward radiance during L'Atalante cruise ATA03 in the Atlantic Ocean at station 019001

description: Vertical profiles of downward irradiance Ed (z,lambda) in and upward radiance Lu (z,lambda) in were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles up to 90 m were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz. The free fall velocity of the SPMR instrument was justified by ballast in such a way that more than 5 spectra were samples per meter.
DOI: 10.1594/pangaea.847431
title: Profiles of downward irradiance and upward radiance during L'Atalante cruise ATA03 in the Atlantic Ocean at station 020001

description: Vertical profiles of downward irradiance Ed (z,lambda) in and upward radiance Lu (z,lambda) in were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles up to 90 m were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz. The free fall velocity of the SPMR instrument was justified by ballast in such a way that more than 5 spectra were samples per meter.
DOI: 10.1594/pangaea.847432
title: Profiles of downward irradiance and upward radiance during L'Atalante cruise ATA03 in the Atlantic Ocean at station 023001

description: Vertical profiles of downward irradiance Ed (z,lambda) in and upward radiance Lu (z,lambda) in were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles up to 90 m were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz. The free fall velocity of the SPMR instrument was justified by ballast in such a way that more than 5 spectra were samples per meter.
DOI: 10.5281/zenodo.12560881
title: Dataset: NXP Semiconductors N.V. (NXPI) Stock Performance

description: This dataset provides historical stock market performance data for specific companies. It enables users to analyze and understand the past trends and fluctuations in stock prices over time. This information can be utilized for various purposes such as investment analysis, financial research, and market trend forecasting.
DOI: 10.5281/zenodo.12560882
title: Dataset: NXP Semiconductors N.V. (NXPI) Stock Performance

description: This dataset provides historical stock market performance data for specific companies. It enables users to analyze and understand the past trends and fluctuations in stock prices over time. This information can be utilized for various purposes such as investment analysis, financial research, and market trend forecasting.
DOI: 10.1594/pangaea.847433
title: Profiles of downward irradiance and upward radiance during L'Atalante cruise ATA03 in the Atlantic Ocean at station 026001

description: Vertical profiles of downward irradiance Ed (z,lambda) in and upward radiance Lu (z,lambda) in were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles up to 90 m were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz. The free fall velocity of the SPMR instrument was justified by ballast in such a way that more than 5 spectra were samples per meter.
DOI: 10.1594/pangaea.847434
title: Profiles of downward irradiance and upward radiance during L'Atalante cruise ATA03 in the Atlantic Ocean at station 027001

description: Vertical profiles of downward irradiance Ed (z,lambda) in and upward radiance Lu (z,lambda) in were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles up to 90 m were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz. The free fall velocity of the SPMR instrument was justified by ballast in such a way that more than 5 spectra were samples per meter.
DOI: 10.1594/pangaea.847435
title: Profiles of downward irradiance and upward radiance during L'Atalante cruise ATA03 in the Atlantic Ocean at station 028001

description: Vertical profiles of downward irradiance Ed (z,lambda) in and upward radiance Lu (z,lambda) in were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles up to 90 m were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz. The free fall velocity of the SPMR instrument was justified by ballast in such a way that more than 5 spectra were samples per meter.
DOI: 10.1594/pangaea.847436
title: Profiles of downward irradiance and upward radiance during L'Atalante cruise ATA03 in the Atlantic Ocean at station 029001

description: Vertical profiles of downward irradiance Ed (z,lambda) in and upward radiance Lu (z,lambda) in were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles up to 90 m were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz. The free fall velocity of the SPMR instrument was justified by ballast in such a way that more than 5 spectra were samples per meter.
DOI: 10.1594/pangaea.847437
title: Profiles of downward irradiance and upward radiance during L'Atalante cruise ATA03 in the Atlantic Ocean at station 030001

description: Vertical profiles of downward irradiance Ed (z,lambda) in and upward radiance Lu (z,lambda) in were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles up to 90 m were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz. The free fall velocity of the SPMR instrument was justified by ballast in such a way that more than 5 spectra were samples per meter.
DOI: 10.1594/pangaea.847438
title: Profiles of downward irradiance and upward radiance during L'Atalante cruise ATA03 in the Atlantic Ocean at station 031001

description: Vertical profiles of downward irradiance Ed (z,lambda) in and upward radiance Lu (z,lambda) in were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles up to 90 m were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz. The free fall velocity of the SPMR instrument was justified by ballast in such a way that more than 5 spectra were samples per meter.
DOI: 10.1594/pangaea.847439
title: Profiles of downward irradiance and upward radiance during L'Atalante cruise ATA03 in the Atlantic Ocean at station 032001

description: Vertical profiles of downward irradiance Ed (z,lambda) in and upward radiance Lu (z,lambda) in were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles up to 90 m were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz. The free fall velocity of the SPMR instrument was justified by ballast in such a way that more than 5 spectra were samples per meter.
DOI: 10.1594/pangaea.847440
title: Profiles of downward irradiance and upward radiance during L'Atalante cruise ATA03 in the Atlantic Ocean at station 035001

description: Vertical profiles of downward irradiance Ed (z,lambda) in and upward radiance Lu (z,lambda) in were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles up to 90 m were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz. The free fall velocity of the SPMR instrument was justified by ballast in such a way that more than 5 spectra were samples per meter.
DOI: 10.1594/pangaea.847441
title: Profiles of downward irradiance and upward radiance during L'Atalante cruise ATA03 in the Atlantic Ocean at station 038001

description: Vertical profiles of downward irradiance Ed (z,lambda) in and upward radiance Lu (z,lambda) in were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles up to 90 m were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz. The free fall velocity of the SPMR instrument was justified by ballast in such a way that more than 5 spectra were samples per meter.
DOI: 10.1594/pangaea.847442
title: Profiles of downward irradiance and upward radiance during L'Atalante cruise ATA03 in the Atlantic Ocean at station 039001

description: Vertical profiles of downward irradiance Ed (z,lambda) in and upward radiance Lu (z,lambda) in were determined with Satlantic profiler (SPMR-SeaWiFS Profiling Multichannel Radiometer). Profiles up to 90 m were covered in 13 channels between 412 nm and 700 nm. All measurements were made according to the recommendations of the SeaWiFS validation team (Mueller and Austin 1995). The sampling data rate was 6 Hz. The free fall velocity of the SPMR instrument was justified by ballast in such a way that more than 5 spectra were samples per meter.
DOI: 10.1594/pangaea.847443
title: Incident irradiance above water during L'Atalante cruise ATA03 in the Atlantic Ocean

description: The incident irradiance above water Es (lambda) was measured with RAMSES hyper-spectral radiometer manufactured by TriOS (Oldenburg, Germany). The calibration was made by the manufacturer. The spectral accuracy of the spectral calibration was 0.3 nm. The detector accuracy was derived by the manufacturer and was better than 6 to 10 % depending on the spectral range (Heuermann et al. 1999).
DOI: 10.1594/pangaea.847444
title: The incident irradiance above water in Mindelo at São Vicente in May 2009

description: The incident irradiance above water Es (lambda) was measured with RAMSES hyper-spectral radiometer manufactured by TriOS (Oldenburg, Germany). The calibration was made by the manufacturer. The spectral accuracy of the spectral calibration was 0.3 nm. The detector accuracy was derived by the manufacturer and was better than 6 to 10 % depending on the spectral range (Heuermann et al. 1999).
DOI: 10.5281/zenodo.12560885
title: Dataset: NextPlat Corp (NXPL) Stock Performance

description: This dataset provides historical stock market performance data for specific companies. It enables users to analyze and understand the past trends and fluctuations in stock prices over time. This information can be utilized for various purposes such as investment analysis, financial research, and market trend forecasting.
DOI: 10.5281/zenodo.12560886
title: Dataset: NextPlat Corp (NXPL) Stock Performance

description: This dataset provides historical stock market performance data for specific companies. It enables users to analyze and understand the past trends and fluctuations in stock prices over time. This information can be utilized for various purposes such as investment analysis, financial research, and market trend forecasting.
DOI: 10.1594/pangaea.848536
title: Underway water measurements of halocarbons during Maria S. Merian criuse MSM18/3
DOI: 10.1594/pangaea.848538
title: Halocarbons measured on water bottle samples during Maria S. Merian cruise MSM18/3
DOI: 10.1594/pangaea.848544
title: (Table 1) Characteristics of multinet stations in Fram Strait during the expedition with Maria S. Merian MSM02/4
DOI: 10.1594/pangaea.848975
title: (Table 1) Air temperature, snow and slush depths and sea ice thickness during R/V Lance cruise in April-May 2011
DOI: 10.1594/pangaea.848977
title: (Table 2) Temperature and salinity of sampled snow, sea ice and slush/brine during R/V Lance cruise in April-May 2011
DOI: 10.1594/pangaea.848838
title: Station list and links to master tracks in different resolutions of POLARSTERN cruise ARK-XIX/3b, Tromsø - Longyearbyen, 2003-06-26 - 2003-07-16
DOI: 10.1594/pangaea.848978
title: (Table 3) Number and mean caliper diameter of ikaite crystals sampled during R/V Lance cruise in April-May 2011
DOI: 10.1594/pangaea.848842
title: Station list and links to master tracks in different resolutions of POLARSTERN cruise PS93.1 (ARK-XXIX/2.1), Longyearbyen - Tromsø, 2015-06-29 - 2015-07-17
DOI: 10.1594/pangaea.849286
title: Chlorophyll-a concentration and sea ice concentration at OFOS stations during POLARSTERN cruise ANT-XXIX/3 derived from the merged daily Full Product Set (FPS) of the GlobColour Archive

description: Empty cells represent missing values
DOI: 10.1594/pangaea.849287
title: Benthic terrain modeler sea-bed classification for OFOS stations during POLARSTERN cruise ANT-XXIX/3

description: Empty cells represent missing values
DOI: 10.1594/pangaea.849289
title: Spatial distribution patterns of ascidians (Ascidiacea: Tunicata) on the continental shelves off the northern Antarctic Peninsula studies from OFOS sea-bed images from POLARSTERN cruise ANT-XXIX/3

description: Empty cells represent missing values
DOI: 10.1594/pangaea.849297
title: Underway fCO2, oxygen and total gas pressure measurements in the Mauretanian upwelling during POSEIDON cruise POS348
DOI: 10.1594/pangaea.848595
title: MSM 18/3, tropical Atlantic, shipborne MAX-DOAS Measurements of IO from 2011-07-01 to 2011-07-18

description: MAX-DOAS measurements were performed during the cruise leg MSM 18/3 using the same MAX-DOAS instrument as during TransBrom described in Grossmann et al 2013 (doi:10.5194/acp-13-3363-2013). Except for the use of an updated water vapour cross-section (HITEMP) and the correction for vibrational Raman scattering in air (Lampel et al 2015, doi:10.5194/amtd-8-5895-2015), the fit settings also agree with Grossmann et al 2013 (doi:10.5194/acp-13-3363-2013). Aerosol profiles were retrieved using the O4 absorption at 360 nm using an optimal estimation scheme described in Yilmaz 2013 (http://archiv.ub.uni-heidelberg.de/volltextserver/13128/) and Frieß et al 2006 (doi: 10.1029/2005JD006618) based on SCIATRAN (Rozanov et al 2010, doi:10.1016/j.asr.2005.03.012). These aerosol profiles were used as input parameter to calculate IO concentration profiles during the cruise leg MSM18/3. Here the surface volume mixing ratios are shown.Upper Limits were determined for the following species, which were not detected in significant amounts during the cruise:BrO: 2.2e13 molec/cm**2 at a telescope elevation angle of 3°, which corresponds to an average surface volume mixing of 1.5±0.5 ppt. The spectral settings for the BrO retrieval, which were applied here are in agreement with Pinardi et al 2013 (doi:10.5194/amt-6-167-2013).Glyoxal: 5e14 molec/cm**2 at a telescope elevation angle of 3°, which corresponds to an average surface volume mixing of 25±10 ppt. The fit range was 432-460 nm and otherwise agreed with the spectral analysis of Glyoxal during Polarstern ANT28 listed in Mahajan et al 2014 (doi:10.1002/2013JD021388).Formaldehyde mixing ratios can be processed on request. The spectral data of the measurements is stored on the measurement data server of the Institute for Environmental Physics, University of Heidelberg.
DOI: 10.1594/pangaea.849314
title: Bathymetry of the Tyrrhenian Sea during METEOR cruise M86/4

description: Processed EM122 and EM710 multibeam data of R/V Meteor expedition M86/4 as ungridded XYZ-files (RAR-Archives). Additionally one grid.file (25m spatial resolution) of the EM122 data is given in ArcView *.asc format. All files given in geographic lat/long, WGS84.
DOI: 10.5281/zenodo.12560887
title: Dataset: NextPlat Corp (NXPLW) Stock Performance

description: This dataset provides historical stock market performance data for specific companies. It enables users to analyze and understand the past trends and fluctuations in stock prices over time. This information can be utilized for various purposes such as investment analysis, financial research, and market trend forecasting.
DOI: 10.5281/zenodo.12560888
title: Dataset: NextPlat Corp (NXPLW) Stock Performance

description: This dataset provides historical stock market performance data for specific companies. It enables users to analyze and understand the past trends and fluctuations in stock prices over time. This information can be utilized for various purposes such as investment analysis, financial research, and market trend forecasting.
DOI: 10.1594/pangaea.849323
title: Ice rafted debris in sediment core MSM05/5_723-2
DOI: 10.1594/pangaea.849324
title: Stable isotope ratios on foraminifera in sediment core MSM05/5_723-2
DOI: 10.1594/pangaea.849326
title: Sea surface temperature reconstruction in sediment core MSM05/5_712-2
DOI: 10.1594/pangaea.849328
title: Sea surface temperature reconstruction in sediment core MSM05/5_723-2
DOI: 10.1594/pangaea.849329
title: Foraminifera abundance in sediment core MSM05/5_723-2
DOI: 10.1594/pangaea.849330
title: Biomarker in sediment core MSM05/5_723-2
DOI: 10.1594/pangaea.849113
title: Age model of sediment core PS58/270-5
DOI: 10.1594/pangaea.849114
title: Age model of sediment core PS58/271-1
DOI: 10.1594/pangaea.849513
title: Continuous meteorological surface measurement during POLARSTERN cruise PS93.1 (ARK-XXIX/2.1)
DOI: 10.1594/pangaea.849661
title: Ceilometer CL51 raw data measured during POLARSTERN cruise PS93.1, links to files
DOI: 10.1594/pangaea.849585
title: Radiosonde PS93/37390 during POLARSTERN cruise PS93.1 (ARK-XXIX/2.1) on 2015-06-30 04:30h

description: Height of tropopause 9453 m, precipitable water content 1.1378 cm
DOI: 10.1594/pangaea.849586
title: Radiosonde PS93/37391 during POLARSTERN cruise PS93.1 (ARK-XXIX/2.1) on 2015-06-30 10:42h

description: Height of tropopause 9680 m, precipitable water content 1.0443 cm
DOI: 10.1594/pangaea.849587
title: Radiosonde PS93/37392 during POLARSTERN cruise PS93.1 (ARK-XXIX/2.1) on 2015-07-01 04:30h

description: Height of tropopause 9205 m, precipitable water content 0.9567 cm
DOI: 10.5281/zenodo.12560889
title: Dataset: Nexstar Media Group, Inc. (NXST) Stock Performance

description: This dataset provides historical stock market performance data for specific companies. It enables users to analyze and understand the past trends and fluctuations in stock prices over time. This information can be utilized for various purposes such as investment analysis, financial research, and market trend forecasting.
DOI: 10.5281/zenodo.12560890
title: Dataset: Nexstar Media Group, Inc. (NXST) Stock Performance

description: This dataset provides historical stock market performance data for specific companies. It enables users to analyze and understand the past trends and fluctuations in stock prices over time. This information can be utilized for various purposes such as investment analysis, financial research, and market trend forecasting.
DOI: 10.1594/pangaea.849588
title: Radiosonde PS93/37393 during POLARSTERN cruise PS93.1 (ARK-XXIX/2.1) on 2015-07-01 10:42h

description: Height of tropopause 8466 m, precipitable water content 0.9588 cm
DOI: 10.1594/pangaea.849589
title: Radiosonde PS93/37394 during POLARSTERN cruise PS93.1 (ARK-XXIX/2.1) on 2015-07-02 04:31h

description: Height of tropopause 8967 m, precipitable water content 1.4834 cm
DOI: 10.1594/pangaea.849590
title: Radiosonde PS93/37395 during POLARSTERN cruise PS93.1 (ARK-XXIX/2.1) on 2015-07-02 10:40h

description: Height of tropopause 8728 m, precipitable water content 1.2923 cm
DOI: 10.1594/pangaea.849591
title: Radiosonde PS93/37396 during POLARSTERN cruise PS93.1 (ARK-XXIX/2.1) on 2015-07-03 04:31h

description: Height of tropopause 9307 m, precipitable water content 1.1087 cm
DOI: 10.1594/pangaea.849592
title: Radiosonde PS93/37397 during POLARSTERN cruise PS93.1 (ARK-XXIX/2.1) on 2015-07-03 10:40h

description: Height of tropopause 9727 m, precipitable water content 1.2239 cm
DOI: 10.1594/pangaea.849593
title: Radiosonde PS93/37398 during POLARSTERN cruise PS93.1 (ARK-XXIX/2.1) on 2015-07-04 04:31h

description: Height of tropopause 9677 m, precipitable water content 1.6820 cm
DOI: 10.1594/pangaea.849594
title: Radiosonde PS93/37399 during POLARSTERN cruise PS93.1 (ARK-XXIX/2.1) on 2015-07-04 10:39h

description: Height of tropopause 9384 m, precipitable water content 1.8005 cm
DOI: 10.1594/pangaea.849595
title: Radiosonde PS93/37400 during POLARSTERN cruise PS93.1 (ARK-XXIX/2.1) on 2015-07-05 04:36h

description: Height of tropopause 9056 m, precipitable water content 1.2995 cm
DOI: 10.1594/pangaea.849596
title: Radiosonde PS93/37401 during POLARSTERN cruise PS93.1 (ARK-XXIX/2.1) on 2015-07-05 10:42h

description: Height of tropopause 9848 m, precipitable water content 1.2005 cm
DOI: 10.1594/pangaea.849597
title: Radiosonde PS93/37402 during POLARSTERN cruise PS93.1 (ARK-XXIX/2.1) on 2015-07-06 04:31h

description: Height of tropopause 10212 m, precipitable water content 1.0938 cm