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  • 1
    facet.materialart.
    Unknown
    Global warming will increase earthquake hazards through rising sea levels and cascading effects (2024)
    In:  Seismological Research Letters
    Details
    Publication Date: 2024-07-04
    Type: info:eu-repo/semantics/article
    Format: application/pdf
    Location Call Number Expected Availability
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    PAPER (OA)
  • 2
    facet.materialart.
    Unknown
    Heavy metals concentrations in river Benue, Adamawa State, Nigeria (2021)
    PANGAEA
    Details
    Publication Date: 2024-07-04
    Description: This study was designed to assess the concentration of heavy metals in water, two fish species (Clarias gariepinus and Oreochromis niloticus), and three different vegetables (Spinach, Rosella, and Jute mallow) which were grown around the riverbank of River Benue. A laboratory-based study was adopted. Fish, water samples, and vegetables were collected monthly at different locations named points A, B, and C from River Benue for five consecutive months between October 2019 and February 2020 and analyzed for physicochemical parameters. The parameters included pH, dissolved oxygen (DO), temperature, conductivity, lead, cadmium, manganese, zinc, Iron, and copper.
    Keywords: fish; heavy metals; Leibniz Centre for Tropical Marine Research; vegetables; water; ZMT
    Type: Dataset
    Format: application/zip, 5 datasets
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 3
    facet.materialart.
    Unknown
    Mercury concentration, total organic carbon and elemantal ratios analysis of sediment core GL-1090 from the subtropical western South Atlantic (2020)
    PANGAEA
    Details
    Publication Date: 2024-07-04
    Description: During glacial/interglacial cycles, changes in the strength of the Atlantic Meridional Overturning Circulation (AMOC) modified the intermediate and deep-water mass proportions and high latitude productivity in the Atlantic Ocean. These factors influence the distribution and geochemical partitioning of trace metals in the ocean. Mercury is a redox and productivity-sensitive trace metal, making it a potential proxy of paleoenvironmental changes. Therefore, this work examines the effect of Atlantic Ocean circulation changes during the last two glacial/interglacial cycles on the biogeochemistry of Hg. For this, a high-resolution record of the total Hg concentration was determined in core GL-1090 collected from the Southwestern Subtropical Atlantic that represents the last 185 thousand years. During the reported glacial/interglacial cycles, Hg showed a distinct trend throughout Marine Isotope Stages with higher concentrations during periods of enhanced penetration of northern component water into the southwestern Atlantic. This is supported by the similarity of mercury variability with benthic foraminifera δ¹³C, suggesting a strong influence of deep ocean circulation on the availability and accumulation of this metal in deep-sea sediments. Mercury geochemistry and particle scavenging were correlated with organic matter (OM) input at the core site. We also noted that mercury responded to redox variation in sediment after Termination II, which can be explained by the increase in deep ocean ventilation due to AMOC strengthening. This hypothesis was confirmed by the antiphase behavior of Hg and Total Organic Carbon when compared with Mn/Al ratios and CaCO3. Our work, therefore, allows for a better understanding of the processes leading to long-term mercury removal to sediments.
    Keywords: Atlantic meridional overturning circulation; Calcium carbonate dissolution; Mercury concentration; Organic matter remineralization; paleoproductivity
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 4
    facet.materialart.
    Unknown
    Photobiological Effects on Ice Algae of a Rapid Whole-Fjord Loss of Snow Cover during Spring Growth in Kangerlussuaq, a West Greenland Fjord (2023)
    PANGAEA
    Details
    Publication Date: 2024-07-04
    Description: The presence of snow on sea-ice can have dramatic effects on the photosynthetically available radiation (PAR) that reaches the ice algae. To better quantify this effect in the high Arctic, an experiment was conducted in Kangerlussuaq, west Greenland, throughout March 2013 where snow was cleared off the sea-ice and measured parameters were compared to a control area. Samples of under-ice algae were then taken to analyse the species composition. The bottom 30 mm of the sampled ice cores were used to determine the stress on the photosystems of the sea ice algae as they experienced the rapid irradiance via the variable fluorescence of photosystem II (PSII). PSII was measured using pulse amplitude modulated (PAM) fluorometry (Walz Imaging-PAM fluorometer). This provides the effective quantum yield of PSII (Φ_PSII), which is a unitless ratio of ambient (F) and maximum (F_m) fluorescence yields. These measurements were taken every 3 hours over the final day of the study. Periodically over the week of the study, similar measurements were taken (in triplicate) with a Phyto-PAM System II Emitter-Detector (Phyto-ED) to determine how F and F_m values changed at a courser temporal resolution. Also measured were rapid light curves (RLCs), which allowed for the derivation of the relative electron transfer rate (rETR and rETR_max; µmol é/m²/s), the slope of the light-limited portion of the RLC (α; mol é /mol photons), and the irradiance at which rETR was light-saturated (E_k; µmol photon/m²/s). 100 ml samples of thawed sea-ice were also collected and stored in the dark to be used for species identification. This was done by first enumerating the ice algae to the Utermöhl method. A Zeiss Axiovert 135M (40×) inverted microscope was used to identify and count species/morphological groups via a total of four diagonals per sample. Relative abundances of algae were estimated as percent of total count, and the biomass was calculated according to the ALGESYS protocol. Throughout the experiment the following variables were collected at 5 minute intervals: Air temperature (°C; sun-screened Campbell 107 temperature probe), upwelling and downwelling PAR (µmol photons/m²s; Li-COR Li-191 PAR sensor) at 0.5 m above the sea-ice surface, and under-ice PAR (µmol photon/m²/s; Li-COR –Li-192 submersible PAR sensor). From these data, transmittance (τ) was calculated as the ratio between under-ice PAR and downwelling PAR at the surface, and albedo (0-1 scale) was calculated as the ratio between upwelling and downwelling PAR at the surface.
    Keywords: Arctic Biodiversity & Livelihoods; FACE-IT; Greenland; ice algae; Kangerlussuaq_2013; optics; photobiology; Snow cover; Spectral radiometer; SPRA; stress
    Type: Dataset
    Format: application/zip, 4 datasets
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 5
    facet.materialart.
    Unknown
    Analysis of a sediment core MVSEIS08_TG-2 taken during the MVSEIS2008 expedition in Gulf of Cadiz (2024)
    PANGAEA
    Details
    Publication Date: 2024-07-04
    Description: Core MVSEIS08-TG-2 was acquired during the Euromargin-MVSEIS08 cruise on the Moroccan margin, south of the Gulf of Cadiz. This site was targeted to discuss the possibility of the saline upper branch of the Mediterranean Outflow Water (MOW) diverging southwards along the Moroccan margin, in addition to the well-established northern MOW current. The southern TG-2 is a 2.12 m gravity core. Contourite records cover the time interval from the last deglaciation starting at HS1 (18.6 ka) to the Holocene. New datasets of current velocity (sortable silt) and water mass origin (O and C isotopes of benthic foraminifera) define the intensity of the MOW as contourite deposits, together with element ratios (XRF-scan) and physical properties of the sediment. O and C isotopes of planktonic foraminifera, foraminiferal species and sea surface temperature (simmax.28 transfer function) were used to determine millennial climate changes during the last deglaciation.
    Keywords: contourites; Gulf of Cadiz; Heinrich Event 1; Mediterranean outflow; MOW; sortable silt; SST (foraminifera); stable oxygen and carbon isotopes; Younger Dryas
    Type: Dataset
    Format: application/zip, 9 datasets
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 6
    facet.materialart.
    Unknown
    Analysis of sediment cores GC-01A taken during the CONTOURIBER-1 expedition in Gulf of Cadiz (2024)
    PANGAEA
    Details
    Publication Date: 2024-07-04
    Description: Core GC-01A was collected during the Contouriber-I cruise in the northern Gulf of Cadiz, bathed by the well-established northern Mediterranean Outflow Water (MOW) current along the Iberian margin; this site was a contrasting reference site to discuss the possibility of the saline upper branch of the MOW diverging southwards along the Moroccan margin (core MVSEIS08-TG-2). GC-01A-TC (0.87 m) and GC-01A-PC (5.21 m) consist of trigger and gravity cores from the same site, with both sections connected by a time gap at 8-9 ka. The contourite records cover the time interval from the Last Glacial Maximum (22 ka) through the last deglaciation to the Holocene (GC-01A). New datasets of current velocity (sortable silt) and water mass origin (O and C isotopes of benthic foraminifera) define the intensity of the MOW as contourite deposits, together with element ratios (XRF-scan) and physical properties of the sediment. O and C isotopes of planktonic foraminifera, foraminiferal species and sea surface temperature (simmax.28 transfer function) were used to determine millennial climate changes during the last deglaciation.
    Keywords: contourites; Gulf of Cadiz; Heinrich Event 1; Mediterranean outflow; MOW; sortable silt; SST (foraminifera); stable oxygen and carbon isotopes; Younger Dryas
    Type: Dataset
    Format: application/zip, 9 datasets
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 7
    facet.materialart.
    Unknown
    Physical oceanography during Maria S. Merian cruise MSM76 (2020)
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Details
    Publication Date: 2024-07-04
    Keywords: AWI_PhyOce; Calculated; Conductivity; CTD, SEA-BIRD SBE 911plus, SN T1526-C1222; CTD, towed system; CTD/Rosette; CTD-RO; CTD-twoyo; CTD-yoyo; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Der Nordatlantik als Teil des Erdsystems; Elevation of event; Event label; FRAM; Fram Strait; FRontiers in Arctic marine Monitoring; Greenland - Ice Sheet/Ocean Interaction: From process understanding to an analysis of the regional system; GROCE; Latitude of event; Longitude of event; Maria S. Merian; MSM76; MSM76_100-1; MSM76_101-1; MSM76_102-1; MSM76_103-1; MSM76_103-10; MSM76_103-11; MSM76_103-12; MSM76_103-13; MSM76_103-14; MSM76_103-15; MSM76_103-16; MSM76_103-17; MSM76_103-18; MSM76_103-19; MSM76_103-2; MSM76_103-20; MSM76_103-21; MSM76_103-22; MSM76_103-23; MSM76_103-24; MSM76_103-25; MSM76_103-26; MSM76_103-3; MSM76_103-4; MSM76_103-5; MSM76_103-6; MSM76_103-7; MSM76_103-8; MSM76_103-9; MSM76_104-1; MSM76_105-1; MSM76_106-1; MSM76_107-1; MSM76_108-1; MSM76_109-1; MSM76_1-1; MSM76_110-1; MSM76_11-1; MSM76_111-1; MSM76_112-1; MSM76_113-1; MSM76_114-1; MSM76_115-1; MSM76_116-1; MSM76_118-1; MSM76_119-1; MSM76_120-1; MSM76_121-1; MSM76_122-1; MSM76_123-1; MSM76_124-1; MSM76_125-1; MSM76_126-1; MSM76_129-1; MSM76_130-1; MSM76_13-1; MSM76_131-1; MSM76_133-1; MSM76_134-1; MSM76_135-1; MSM76_136-1; MSM76_137-1; MSM76_138-1; MSM76_14-1; MSM76_141-1; MSM76_142-1; MSM76_143-1; MSM76_144-1; MSM76_145-1; MSM76_146-1; MSM76_147-1; MSM76_148-1; MSM76_149-1; MSM76_15-1; MSM76_154-1; MSM76_154-10; MSM76_154-11; MSM76_154-12; MSM76_154-13; MSM76_154-14; MSM76_154-15; MSM76_154-16; MSM76_154-17; MSM76_154-18; MSM76_154-19; MSM76_154-2; MSM76_154-20; MSM76_154-21; MSM76_154-22; MSM76_154-23; MSM76_154-24; MSM76_154-25; MSM76_154-26; MSM76_154-27; MSM76_154-28; MSM76_154-29; MSM76_154-3; MSM76_154-30; MSM76_154-31; MSM76_154-4; MSM76_154-5; MSM76_154-6; MSM76_154-7; MSM76_154-8; MSM76_154-9; MSM76_158-1; MSM76_158-10; MSM76_158-11; MSM76_158-12; MSM76_158-13; MSM76_158-14; MSM76_158-15; MSM76_158-16; MSM76_158-17; MSM76_158-18; MSM76_158-19; MSM76_158-2; MSM76_158-20; MSM76_158-3; MSM76_158-4; MSM76_158-5; MSM76_158-6; MSM76_158-7; MSM76_158-8; MSM76_158-9; MSM76_159-1; MSM76_159-10; MSM76_159-11; MSM76_159-12; MSM76_159-13; MSM76_159-2; MSM76_159-3; MSM76_159-4; MSM76_159-5; MSM76_159-6; MSM76_159-7; MSM76_159-8; MSM76_159-9; MSM76_16-1; MSM76_162-1; MSM76_163-1; MSM76_164-1; MSM76_165-1; MSM76_166-1; MSM76_167-1; MSM76_168-1; MSM76_169-1; MSM76_170-1; MSM76_17-1; MSM76_171-1; MSM76_172-1; MSM76_173-1; MSM76_174-1; MSM76_175-1; MSM76_176-1; MSM76_177-1; MSM76_180-1; MSM76_18-1; MSM76_181-1; MSM76_182-1; MSM76_183-1; MSM76_184-1; MSM76_185-1; MSM76_186-1; MSM76_187-1; MSM76_188-1; MSM76_189-1; MSM76_190-1; MSM76_19-1; MSM76_191-1; MSM76_192-1; MSM76_193-1; MSM76_194-1; MSM76_195-1; MSM76_196-1; MSM76_197-1; MSM76_200-1; MSM76_20-1; MSM76_201-1; MSM76_207-1; MSM76_208-1; MSM76_209-1; MSM76_2-1; MSM76_210-1; MSM76_211-1; MSM76_212-1; MSM76_215-1; MSM76_216-1; MSM76_217-1; MSM76_218-1; MSM76_219-1; MSM76_220-1; MSM76_221-1; MSM76_222-1; MSM76_223-1; MSM76_224-1; MSM76_227-1; MSM76_228-1; MSM76_229-1; MSM76_230-1; MSM76_231-1; MSM76_232-1; MSM76_233-1; MSM76_234-1; MSM76_235-1; MSM76_236-1; MSM76_237-1; MSM76_238-1; MSM76_239-1; MSM76_24-1; MSM76_25-1; MSM76_26-1; MSM76_27-1; MSM76_28-1; MSM76_29-1; MSM76_30-1; MSM76_3-1; MSM76_31-1; MSM76_32-1; MSM76_33-1; MSM76_34-1; MSM76_35-1; MSM76_36-1; MSM76_37-1; MSM76_38-1; MSM76_39-1; MSM76_40-1; MSM76_4-1; MSM76_41-1; MSM76_42-1; MSM76_43-1; MSM76_44-1; MSM76_45-1; MSM76_46-1; MSM76_47-1; MSM76_48-1; MSM76_49-1; MSM76_50-1; MSM76_5-1; MSM76_53-1; MSM76_55-1; MSM76_56-1; MSM76_57-1; MSM76_58-1; MSM76_59-1; MSM76_60-1; MSM76_6-1; MSM76_61-1; MSM76_62-1; MSM76_63-1; MSM76_64-1; MSM76_65-1; MSM76_66-1; MSM76_67-1; MSM76_68-1; MSM76_69-1; MSM76_70-1; MSM76_7-1; MSM76_71-1; MSM76_72-1; MSM76_73-1; MSM76_74-1; MSM76_75-1; MSM76_76-1; MSM76_77-1; MSM76_78-1; MSM76_79-1; MSM76_80-1; MSM76_8-1; MSM76_81-1; MSM76_82-1; MSM76_83-1; MSM76_84-1; MSM76_85-1; MSM76_86-1; MSM76_87-1; MSM76_88-1; MSM76_89-1; MSM76_90-1; MSM76_91-1; MSM76_92-1; MSM76_93-1; MSM76_94-1; MSM76_95-1; MSM76_96-1; MSM76_97-1; MSM76_98-1; MSM76_99-1; NACLIM; Nordatlantik; North Atlantic; North Atlantic Climate; Number of observations; Oxygen; Oxygen saturation; Physical Oceanography @ AWI; Pressure, water; Priority Programme 1889 Regional Sea Level Change and Society; RACE; Regional Atlantic Circulation and global Change; Salinity; SPP1889; Temperature, water; Temperature, water, potential; TRR181; TRR181 Energy transfers in Atmosphere and Ocean; Yoyo-CTD
    Type: Dataset
    Format: text/tab-separated-values, 1762191 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 8
    facet.materialart.
    Unknown
    Physical oceanography measured on water bottle samples during Maria S. Maria cruise MSM76 (2020)
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Details
    Publication Date: 2024-07-04
    Keywords: AWI_PhyOce; Bottle number; Calculated; Conductivity; CTD, SEA-BIRD SBE 911plus, SN T1526-C1222; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Der Nordatlantik als Teil des Erdsystems; Elevation of event; Event label; FRAM; Fram Strait; FRontiers in Arctic marine Monitoring; Greenland - Ice Sheet/Ocean Interaction: From process understanding to an analysis of the regional system; GROCE; Latitude of event; Longitude of event; Maria S. Merian; MSM76; MSM76_100-1; MSM76_101-1; MSM76_102-1; MSM76_104-1; MSM76_105-1; MSM76_106-1; MSM76_107-1; MSM76_108-1; MSM76_109-1; MSM76_1-1; MSM76_110-1; MSM76_11-1; MSM76_111-1; MSM76_112-1; MSM76_113-1; MSM76_114-1; MSM76_115-1; MSM76_116-1; MSM76_118-1; MSM76_119-1; MSM76_120-1; MSM76_121-1; MSM76_122-1; MSM76_123-1; MSM76_124-1; MSM76_125-1; MSM76_126-1; MSM76_129-1; MSM76_130-1; MSM76_13-1; MSM76_131-1; MSM76_133-1; MSM76_134-1; MSM76_135-1; MSM76_136-1; MSM76_137-1; MSM76_138-1; MSM76_14-1; MSM76_141-1; MSM76_142-1; MSM76_143-1; MSM76_144-1; MSM76_145-1; MSM76_146-1; MSM76_147-1; MSM76_148-1; MSM76_149-1; MSM76_15-1; MSM76_16-1; MSM76_162-1; MSM76_163-1; MSM76_164-1; MSM76_165-1; MSM76_166-1; MSM76_167-1; MSM76_168-1; MSM76_169-1; MSM76_170-1; MSM76_17-1; MSM76_171-1; MSM76_172-1; MSM76_173-1; MSM76_174-1; MSM76_175-1; MSM76_176-1; MSM76_177-1; MSM76_180-1; MSM76_181-1; MSM76_182-1; MSM76_183-1; MSM76_184-1; MSM76_185-1; MSM76_186-1; MSM76_187-1; MSM76_188-1; MSM76_189-1; MSM76_190-1; MSM76_19-1; MSM76_191-1; MSM76_192-1; MSM76_193-1; MSM76_194-1; MSM76_195-1; MSM76_196-1; MSM76_197-1; MSM76_200-1; MSM76_201-1; MSM76_207-1; MSM76_208-1; MSM76_209-1; MSM76_2-1; MSM76_210-1; MSM76_211-1; MSM76_212-1; MSM76_215-1; MSM76_216-1; MSM76_218-1; MSM76_220-1; MSM76_222-1; MSM76_224-1; MSM76_24-1; MSM76_26-1; MSM76_27-1; MSM76_28-1; MSM76_29-1; MSM76_30-1; MSM76_3-1; MSM76_31-1; MSM76_32-1; MSM76_33-1; MSM76_34-1; MSM76_35-1; MSM76_36-1; MSM76_37-1; MSM76_38-1; MSM76_39-1; MSM76_40-1; MSM76_4-1; MSM76_41-1; MSM76_42-1; MSM76_43-1; MSM76_44-1; MSM76_45-1; MSM76_46-1; MSM76_47-1; MSM76_48-1; MSM76_49-1; MSM76_50-1; MSM76_5-1; MSM76_53-1; MSM76_55-1; MSM76_56-1; MSM76_57-1; MSM76_58-1; MSM76_59-1; MSM76_60-1; MSM76_6-1; MSM76_61-1; MSM76_62-1; MSM76_63-1; MSM76_64-1; MSM76_65-1; MSM76_66-1; MSM76_67-1; MSM76_68-1; MSM76_69-1; MSM76_70-1; MSM76_7-1; MSM76_71-1; MSM76_72-1; MSM76_73-1; MSM76_74-1; MSM76_75-1; MSM76_76-1; MSM76_77-1; MSM76_78-1; MSM76_79-1; MSM76_80-1; MSM76_8-1; MSM76_81-1; MSM76_82-1; MSM76_83-1; MSM76_84-1; MSM76_85-1; MSM76_86-1; MSM76_87-1; MSM76_88-1; MSM76_89-1; MSM76_90-1; MSM76_91-1; MSM76_92-1; MSM76_93-1; MSM76_94-1; MSM76_95-1; MSM76_96-1; MSM76_97-1; MSM76_98-1; MSM76_99-1; NACLIM; Nordatlantik; North Atlantic; North Atlantic Climate; Oxygen; Oxygen saturation; Oxygen sensor, SBE 43; Physical Oceanography @ AWI; Pressure, water; Priority Programme 1889 Regional Sea Level Change and Society; RACE; Regional Atlantic Circulation and global Change; Salinity; SPP1889; Temperature, water; Temperature, water, potential; TRR181; TRR181 Energy transfers in Atmosphere and Ocean
    Type: Dataset
    Format: text/tab-separated-values, 4671 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 9
    facet.materialart.
    Unknown
    Continuous VM-ADCP (vessel-mounted Acoustic Doppler Current Profiler) profile during Maria S. Merian cruise MSM76 (2023)
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Details
    Publication Date: 2024-07-04
    Keywords: -; Acoustic Doppler Current Profiler; Acoustic Doppler Current Profiling, vessel-mounted (VM-ADCP); ADCP; AWI_PhyOce; Bin number; Current velocity, east-west; Current velocity, error; Current velocity, north-south; Current velocity, standard deviation; Current velocity, vertical; DATE/TIME; Depth, relative; DEPTH, water; LATITUDE; LONGITUDE; Maria S. Merian; MSM76; MSM76_0_underway-2; North Atlantic; Number; Percentage; Physical Oceanography @ AWI; Profile ID; Quality; SADCP; Ship speed; Ship speed, standard deviation; Ship velocity, East; Ship velocity, North; Ship velocity, vertical; VM-ADCP
    Type: Dataset
    Format: text/tab-separated-values, 10766304 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 10
    facet.materialart.
    Unknown
    Lowered Acoustic Doppler Current Profiler (LADCP) data collected during Maria S. Merian cruise MSM76 (2020)
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Details
    Publication Date: 2024-07-04
    Description: For the station-based current velocity measurements during MSM76, a pair of 307kHz. Lowered Acoustic Doppler Current Profilers (LADCPs) was used, mounted on the CTD rosette. Each cast was processed with LDEO Software Version IX-13 from ftp://ftp.ldeo.columbia.edu/pub/LADCP.
    Keywords: Acoustic Doppler Current Profiling (LADCP) [lowered with CTD]; ADCP; AWI_PhyOce; CTD, towed system; CTD/Rosett; CTD/Rosette; CTD-RO; CTD-twoyo; CTD-yoyo; current; Current velocity, east-west; Current velocity, north-south; DATE/TIME; DEPTH, water; Event label; LADCP; LATITUDE; LONGITUDE; Maria S. Merian; MSM76; MSM76_100-1; MSM76_101-1; MSM76_102-1; MSM76_103-1; MSM76_103-10; MSM76_103-11; MSM76_103-12; MSM76_103-13; MSM76_103-14; MSM76_103-15; MSM76_103-16; MSM76_103-17; MSM76_103-18; MSM76_103-19; MSM76_103-2; MSM76_103-20; MSM76_103-21; MSM76_103-22; MSM76_103-23; MSM76_103-24; MSM76_103-25; MSM76_103-26; MSM76_103-3; MSM76_103-4; MSM76_103-5; MSM76_103-6; MSM76_103-7; MSM76_103-8; MSM76_103-9; MSM76_104-1; MSM76_105-1; MSM76_106-1; MSM76_107-1; MSM76_108-1; MSM76_109-1; MSM76_1-1; MSM76_110-1; MSM76_11-1; MSM76_111-1; MSM76_112-1; MSM76_113-1; MSM76_114-1; MSM76_115-1; MSM76_116-1; MSM76_118-1; MSM76_119-1; MSM76_120-1; MSM76_121-1; MSM76_122-1; MSM76_123-1; MSM76_124-1; MSM76_125-1; MSM76_126-1; MSM76_129-1; MSM76_130-1; MSM76_13-1; MSM76_131-1; MSM76_133-1; MSM76_134-1; MSM76_135-1; MSM76_136-1; MSM76_137-1; MSM76_138-1; MSM76_14-1; MSM76_141-1; MSM76_142-1; MSM76_143-1; MSM76_144-1; MSM76_145-1; MSM76_146-1; MSM76_147-1; MSM76_148-1; MSM76_149-1; MSM76_15-1; MSM76_154-1; MSM76_154-10; MSM76_154-11; MSM76_154-12; MSM76_154-13; MSM76_154-14; MSM76_154-15; MSM76_154-16; MSM76_154-17; MSM76_154-18; MSM76_154-19; MSM76_154-2; MSM76_154-20; MSM76_154-21; MSM76_154-22; MSM76_154-23; MSM76_154-24; MSM76_154-25; MSM76_154-26; MSM76_154-27; MSM76_154-28; MSM76_154-29; MSM76_154-3; MSM76_154-30; MSM76_154-31; MSM76_154-4; MSM76_154-5; MSM76_154-6; MSM76_154-7; MSM76_154-8; MSM76_154-9; MSM76_158-1; MSM76_158-10; MSM76_158-11; MSM76_158-12; MSM76_158-13; MSM76_158-14; MSM76_158-15; MSM76_158-16; MSM76_158-17; MSM76_158-18; MSM76_158-19; MSM76_158-2; MSM76_158-20; MSM76_158-3; MSM76_158-4; MSM76_158-5; MSM76_158-6; MSM76_158-7; MSM76_158-8; MSM76_158-9; MSM76_159-1; MSM76_159-10; MSM76_159-11; MSM76_159-12; MSM76_159-13; MSM76_159-2; MSM76_159-3; MSM76_159-4; MSM76_159-5; MSM76_159-6; MSM76_159-7; MSM76_159-8; MSM76_159-9; MSM76_16-1; MSM76_162-1; MSM76_163-1; MSM76_164-1; MSM76_165-1; MSM76_166-1; MSM76_167-1; MSM76_168-1; MSM76_169-1; MSM76_170-1; MSM76_17-1; MSM76_171-1; MSM76_172-1; MSM76_173-1; MSM76_174-1; MSM76_175-1; MSM76_176-1; MSM76_180-1; MSM76_18-1; MSM76_181-1; MSM76_182-1; MSM76_183-1; MSM76_184-1; MSM76_185-1; MSM76_186-1; MSM76_187-1; MSM76_188-1; MSM76_189-1; MSM76_190-1; MSM76_19-1; MSM76_191-1; MSM76_192-1; MSM76_193-1; MSM76_194-1; MSM76_195-1; MSM76_196-1; MSM76_197-1; MSM76_200-1; MSM76_20-1; MSM76_201-1; MSM76_207-1; MSM76_208-1; MSM76_209-1; MSM76_2-1; MSM76_210-1; MSM76_211-1; MSM76_212-1; MSM76_215-1; MSM76_216-1; MSM76_217-1; MSM76_218-1; MSM76_219-1; MSM76_220-1; MSM76_221-1; MSM76_222-1; MSM76_223-1; MSM76_224-1; MSM76_227-1; MSM76_228-1; MSM76_229-1; MSM76_230-1; MSM76_231-1; MSM76_232-1; MSM76_233-1; MSM76_234-1; MSM76_235-1; MSM76_236-1; MSM76_237-1; MSM76_238-1; MSM76_239-1; MSM76_24-1; MSM76_25-1; MSM76_26-1; MSM76_27-1; MSM76_28-1; MSM76_29-1; MSM76_30-1; MSM76_3-1; MSM76_31-1; MSM76_32-1; MSM76_33-1; MSM76_34-1; MSM76_35-1; MSM76_36-1; MSM76_37-1; MSM76_38-1; MSM76_39-1; MSM76_40-1; MSM76_4-1; MSM76_41-1; MSM76_42-1; MSM76_43-1; MSM76_44-1; MSM76_45-1; MSM76_46-1; MSM76_47-1; MSM76_48-1; MSM76_49-1; MSM76_50-1; MSM76_5-1; MSM76_53-1; MSM76_55-1; MSM76_56-1; MSM76_57-1; MSM76_58-1; MSM76_59-1; MSM76_60-1; MSM76_6-1; MSM76_61-1; MSM76_62-1; MSM76_63-1; MSM76_64-1; MSM76_65-1; MSM76_66-1; MSM76_67-1; MSM76_68-1; MSM76_69-1; MSM76_70-1; MSM76_7-1; MSM76_71-1; MSM76_72-1; MSM76_73-1; MSM76_74-1; MSM76_75-1; MSM76_76-1; MSM76_77-1; MSM76_78-1; MSM76_79-1; MSM76_80-1; MSM76_8-1; MSM76_81-1; MSM76_82-1; MSM76_83-1; MSM76_84-1; MSM76_85-1; MSM76_86-1; MSM76_87-1; MSM76_88-1; MSM76_89-1; MSM76_90-1; MSM76_91-1; MSM76_92-1; MSM76_93-1; MSM76_94-1; MSM76_95-1; MSM76_96-1; MSM76_97-1; MSM76_98-1; MSM76_99-1; North Atlantic; Physical Oceanography @ AWI; Station label; velocity; Yoyo-CTD
    Type: Dataset
    Format: text/tab-separated-values, 75351 data points
    Location Call Number Expected Availability
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