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  • 2020-2022  (7)
  • 2005-2009  (9)
  • 1985-1989  (2)
Document type
Keywords
Publisher
Language
Years
Year
  • 1
    Book
    Book
    Ein zweidimensionales Modell zur thermohalinen Zirkulation unter dem Schelfeis : = A two-dimensional model for the thermohaline circulation under an ice shelf (1989)
    Bremerhaven : Alfred-Wegener-Inst. für Polar- und Meeresforschung
    Details Availability
    Keywords: Meridional overturning circultion ; Glaciers ; Hochschulschrift ; Schelfeis ; Zirkulation ; Modell ; Antarktis ; Wasserumlauf ; Schelfeis ; Modell ; Antarktis ; Wasserumlauf ; Bodenwasser ; Schelfeis ; Wasserumlauf ; Südpolarmeer ; Meeresströmung ; Schelfeis ; Antarktis ; Schelfeis ; Zirkulationsmodell
    Type of Medium: Book
    Pages: 87 S. , zahlr. graph. Darst., Kt.
    Series Statement: Berichte zur Polarforschung 60
    URL: https://www.gbv.de/dms/tib-ub-hannover/027415767.pdf
    DDC: 551.46/9
    RVK:
    RY 20075
    Language: German , English
    Note: Literaturverz. S. 82 - 86 , Vollst. zugl.: Hamburg, Univ., Diss., 1988
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  • 2
    Book
    Book
    The Southern Ocean : a survey of oceanographic and marine meteorological research work (1985)
    Bremerhaven : Alfred-Wegener-Inst. für Polar- u. Meeresforschung
    Details Availability
    Keywords: Literaturbericht ; Antarktis ; Meer ; Meteorologie ; Antarktis ; Meereskunde ; Antarktis ; Klima ; Südpolarmeer ; Klima ; Südpolarmeer
    Type of Medium: Book
    Pages: 115 S. , graph. Darst., Kt.
    Series Statement: Berichte zur Polarforschung 26
    URL: https://www.gbv.de/dms/tib-ub-hannover/016456882.pdf
    DDC: 551.46/9
    RVK:
    RY 20075
    Language: English
    Note: Literaturverz. S. 102 - 115
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  • 3
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    25 Jahre Alfred-Wegener-Institut für Polar- und Meeresforschung (poster) (2005)
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Details
    Publication Date: 2023-09-01
    Type: Dataset
    Format: application/zip, 11.5 MBytes
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  • 4
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    (Table 1) Iceberg characteristics and start and end date and location of iceberg buoys in the Weddell Sea (2006)
    PANGAEA
    In:  Supplement to: Schodlok, Michael P; Hellmer, Hartmut H; Rohardt, Gerd; Fahrbach, Eberhard (2006): Weddell Sea iceberg drift: Five years of observations. Journal of Geophysical Research, 111(C6), https://doi.org/10.1029/2004JC002661
    Details
    Publication Date: 2023-10-28
    Description: The drift of 52 icebergs tagged with GPS buoys in the Weddell Sea since 1999 has been investigated with respect to prevalent drift tracks, sea ice/iceberg interaction, and freshwater fluxes. Buoys were deployed on small- to medium-sized icebergs (edge lengths 〈= 5 km) in the southwestern and eastern Weddell Sea. The basin-scale iceberg drift of this size class was established. In the western Weddell Sea, icebergs followed a northward course with little deviation and mean daily drift rates up to 9.5 ± 7.3 km/d. To the west of 40°W the drift of iceberg and sea ice was coherent. In the highly consolidated perennial sea ice cover of 95% the sea ice exerted a steering influence on the icebergs and was thus responsible for the coherence of the drift tracks. The northward drift of buoys to the east of 40°W was interrupted by large deviations due to the passage of low-pressure systems. Mean daily drift rates in this area were 11.5 ± 7.2 km/d. A lower threshold of 86% sea ice concentration for coherent sea ice/iceberg movement was determined by examining the sea ice concentration derived from Special Sensor Microwave Imager (SSM/I) and Advanced Microwave Scanning Radiometer for EOS (AMSR-E) satellite data. The length scale of coherent movement was estimated to be at least 200 km, about half the value found for the Arctic Ocean but twice as large as previously suggested. The freshwater fluxes estimated from three iceberg export scenarios deduced from the iceberg drift pattern were highly variable. Assuming a transit time in the Weddell Sea of 1 year, the iceberg meltwater input of 31 Gt which is about a third of the basal meltwater input from the Filchner Ronne Ice Shelf but spreads across the entire Weddell Sea. Iceberg meltwater export of 14.2 × 103 m3 s-1, if all icebergs are exported, is in the lower range of freshwater export by sea ice.
    Keywords: AWI_SeaIce; Date/time end; Date/time start; Freeboard; Identification; LATITUDE; Latitude 2; Length; LONGITUDE; Longitude 2; ORDINAL NUMBER; Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; Sea Ice Physics @ AWI; SPP1158; Width
    Type: Dataset
    Format: text/tab-separated-values, 422 data points
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  • 5
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    Chlorofluorocarbons, helium, and neon measured on water bottle samples during POLARSTERN cruise ANT-XXII/2 (ISPOL) (2008)
    PANGAEA
    In:  Supplement to: Huhn, Oliver; Hellmer, Hartmut H; Rhein, Monika; Rodehacke, Christian; Roether, Wolfgang; Schodlok, Michael P; Schröder, Michael (2008): Evidence of deep- and bottom-water formation in the western Weddell Sea. Deep Sea Research Part II: Topical Studies in Oceanography, 55(8-9), 1098-1116, https://doi.org/10.1016/j.dsr2.2007.12.015
    Details
    Publication Date: 2024-06-25
    Description: During Ice Station POLarstern (ISPOL; R.V. Polarstern cruise ANT XXII/2, November 2004-January 2005), hydrographic and tracer observations were obtained in the western Weddell Sea while drifting closely in front of the Larsen Ice Shelf. These observations indicate recently formed Weddell Sea Bottom Water, which contains significant contributions of glacial melt water in its upper part, and High-Salinity Shelf Water in its lower layer. The formation of this bottom water cannot be related to the known sources in the south, the Filchner-Ronne Ice Shelf. We show that this bottom water is formed in the western Weddell Sea, most likely in interaction with the Larsen C Ice Shelf. By applying an Optimum Multiparameter Analysis (OMP) using temperature, salinity, and noble gas observations (helium isotopes and neon), we obtained mean glacial melt-water fractions of about 0.1% in the bottom water. On sections across the Weddell Gyre farther north, melt-water fractions are still on the order of 0.04%. Using chlorofluorocarbons (CFCs) as age tracers, we deduced a mean transit time between the western source and the bottom water found on the slope toward the north (9±3 years). This transit time is larger and the inferred transport rate is small in comparison to previous findings. But accounting for a loss of the initially formed bottom water volume due to mixing and renewal of Weddell Sea Deep Water, a formation rate of 1.1±0.5 Sv in the western Weddell Sea is plausible. This implies a basal melt rate of 35±19 Gt/year or 0.35±0.19 m/year at the Larsen Ice Shelf. This bottom water is shallow enough that it could leave the Weddell Basin through the gaps in the South Scotia Ridge to supply Antarctic Bottom Water. These findings emphasize the role of the western Weddell Sea in deep- and bottom-water formation, particularly in view of changing environmental conditions due to climate variability, which might induce enhanced melting or even decay of ice shelves.
    Keywords: ANT-XXII/2; ANT-XXII/2_003-1; ANT-XXII/2_005-1; ANT-XXII/2_006-1; ANT-XXII/2_007-1; ANT-XXII/2_008-1; ANT-XXII/2_009-1; ANT-XXII/2_010-1; ANT-XXII/2_011-1; ANT-XXII/2_012-1; ANT-XXII/2_013-1; ANT-XXII/2_014-1; ANT-XXII/2_015-1; ANT-XXII/2_017-1; ANT-XXII/2_018-1; ANT-XXII/2_019-1; ANT-XXII/2_020-1; ANT-XXII/2_022-1; CTD/Rosette; CTD from ice float; CTDIF; CTD-RO; ICE; Ice station; Polarstern; Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; PS67/005-1; PS67/006-1; PS67/006-100; PS67/006-102; PS67/006-103; PS67/006-108; PS67/006-109; PS67/006-11; PS67/006-110; PS67/006-111; PS67/006-113; PS67/006-115; PS67/006-118; PS67/006-12; PS67/006-120; PS67/006-123; PS67/006-126; PS67/006-128; PS67/006-13; PS67/006-130; PS67/006-131; PS67/006-134; PS67/006-135; PS67/006-139; PS67/006-140; PS67/006-142; PS67/006-144; PS67/006-146; PS67/006-15; PS67/006-18; PS67/006-19; PS67/006-2; PS67/006-21; PS67/006-22; PS67/006-23; PS67/006-25; PS67/006-27; PS67/006-30; PS67/006-32; PS67/006-35; PS67/006-38; PS67/006-4; PS67/006-40; PS67/006-41; PS67/006-43; PS67/006-45; PS67/006-47; PS67/006-48; PS67/006-51; PS67/006-53; PS67/006-57; PS67/006-59; PS67/006-61; PS67/006-63; PS67/006-65; PS67/006-66; PS67/006-68; PS67/006-7; PS67/006-70; PS67/006-73; PS67/006-74; PS67/006-76; PS67/006-78; PS67/006-79; PS67/006-82; PS67/006-84; PS67/006-87; PS67/006-89; PS67/006-9; PS67/006-92; PS67/006-94; PS67/006-96; PS67/006-98; PS67/006-99; PS67/007-1; PS67/008-1; PS67/009-1; PS67/011-1; PS67/011-2; PS67/011-3; PS67 ISPOL; Scotia Sea, southwest Atlantic; SPP1158; Weddell Sea
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 6
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    Physical oceanography from 120 CTDs, 79 water bottles stations, and 30 helicopter-borne CTDs during POLARSTERN cruise ANT-XXII/2 (ISPOL) (2008)
    PANGAEA
    In:  Supplement to: Absy, Joao Marcelo; Schröder, Michael; Muench, Robin D; Hellmer, Hartmut H (2008): Early summer thermohaline characteristics and mixing in the western Weddell Sea. Deep Sea Research Part II: Topical Studies in Oceanography, 55(8-9), 1117-1131, https://doi.org/10.1016/j.dsr2.2007.12.023
    Details
    Publication Date: 2024-06-25
    Description: The Ice Station POLarstern (ISPOL) cruise revisited the western Weddell Sea in late 2004 and obtained a comprehensive set of conductivity-temperature-depth (CTD) data. This study describes the thermohaline structure and diapycnal mixing environment observed in 2004 and compares them with conditions observed more than a decade earlier. Hydrographic conditions on the central western Weddell Sea continental slope, off Larsen C Ice Shelf, in late winter/early spring of 2004/2005 can be described as a well-stratified environment with upper layers evidencing relict structures from intense winter near-surface vertical fluxes, an intermediate depth temperature maximum, and a cold near-bottom layer marked by patchy property distributions. A well-developed surface mixed layer, isolated from the underlying Warm Deep Water (WDW) by a pronounced pycnocline and characterized by lack of warming and by minimal sea-ice basal melting, supports the assumption that upper ocean winter conditions persisted during most of the ISPOL experiment. Much of the western Weddell Sea water column has remained essentially unchanged since 1992; however, significant differences were observed in two of the regional water masses. The first, Modified Weddell Deep Water (MWDW), comprises the permanent pycnocline and was less saline than a decade earlier, whereas Weddell Sea Bottom Water (WSBW) was horizontally patchier and colder. Near-bottom temperatures observed in 2004 were the coldest on record for the western Weddell Sea over the continental slope. Minimum temperatures were ~0.4 and ~0.3 °C colder than during 1992-1993, respectively. The 2004 near-bottom temperature/salinity characteristics revealed the presence of two different WSBW types, whereby a warm, fresh layer overlays a colder, saltier layer (both formed in the western Weddell Sea). The deeper layer may have formed locally as high salinity shelf water (HSSW) that flowed intermittently down the continental slope, which is consistent with the observed horizontal patchiness. The latter can be associated with the near-bottom variability found in Powell Basin with consequences for the deep water outflow from the Weddell Sea.
    Keywords: ANT-XXII/2; ANT-XXII/2_003-1; ANT-XXII/2_004-1; ANT-XXII/2_005-1; ANT-XXII/2_006-1; ANT-XXII/2_007-1; ANT-XXII/2_007-22; ANT-XXII/2_008-1; ANT-XXII/2_008-22; ANT-XXII/2_009-1; ANT-XXII/2_009-22; ANT-XXII/2_010-1; ANT-XXII/2_011-1; ANT-XXII/2_012-1; ANT-XXII/2_013-1; ANT-XXII/2_014-1; ANT-XXII/2_015-1; ANT-XXII/2_016-1; ANT-XXII/2_017-1; ANT-XXII/2_018-1; ANT-XXII/2_019-1; ANT-XXII/2_020-1; ANT-XXII/2_021-1; ANT-XXII/2_022-1; ANT-XXII/2_066-22; ANT-XXII/2_139-22; ANT-XXII/2_140-22; ANT-XXII/2_142-22; ANT-XXII/2_143-22; ANT-XXII/2_144-22; ANT-XXII/2_146-22; AWI_PhyOce; CTD/Rosette; CTD from ice float; CTDIF; CTD-RO; Physical Oceanography @ AWI; Polarstern; PS67/005-1; PS67/006-10; PS67/006-100; PS67/006-101; PS67/006-102; PS67/006-103; PS67/006-104; PS67/006-105; PS67/006-108; PS67/006-109; PS67/006-11; PS67/006-110; PS67/006-111; PS67/006-113; PS67/006-115; PS67/006-116; PS67/006-118; PS67/006-12; PS67/006-120; PS67/006-121; PS67/006-122; PS67/006-123; PS67/006-126; PS67/006-127; PS67/006-128; PS67/006-13; PS67/006-130; PS67/006-131; PS67/006-132; PS67/006-133; PS67/006-134; PS67/006-135; PS67/006-136; PS67/006-137; PS67/006-139; PS67/006-14; PS67/006-140; PS67/006-142; PS67/006-143; PS67/006-144; PS67/006-146; PS67/006-15; PS67/006-18; PS67/006-19; PS67/006-2; PS67/006-20; PS67/006-21; PS67/006-22; PS67/006-23; PS67/006-25; PS67/006-26; PS67/006-27; PS67/006-29; PS67/006-3; PS67/006-30; PS67/006-32; PS67/006-33; PS67/006-34; PS67/006-35; PS67/006-38; PS67/006-39; PS67/006-4; PS67/006-40; PS67/006-41; PS67/006-43; PS67/006-44; PS67/006-45; PS67/006-47; PS67/006-48; PS67/006-49; PS67/006-5; PS67/006-50; PS67/006-51; PS67/006-53; PS67/006-54; PS67/006-55; PS67/006-56; PS67/006-57; PS67/006-59; PS67/006-6; PS67/006-61; PS67/006-62; PS67/006-63; PS67/006-65; PS67/006-66; PS67/006-67; PS67/006-68; PS67/006-7; PS67/006-70; PS67/006-71; PS67/006-72; PS67/006-73; PS67/006-74; PS67/006-75; PS67/006-76; PS67/006-78; PS67/006-79; PS67/006-80; PS67/006-81; PS67/006-82; PS67/006-84; PS67/006-85; PS67/006-86; PS67/006-87; PS67/006-89; PS67/006-9; PS67/006-90; PS67/006-91; PS67/006-92; PS67/006-94; PS67/006-95; PS67/006-96; PS67/006-98; PS67/006-99; PS67/007-1; PS67/008-1; PS67/009-1; PS67/011-1; PS67/011-2; PS67/011-3; PS67 ISPOL; Scotia Sea, southwest Atlantic; Weddell Sea
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 7
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    Physical oceanography from 30 helicopter-borne CTDs during POLARSTERN cruise ANT-XXII/2 (ISPOL) (2008)
    PANGAEA
    Details
    Publication Date: 2024-06-25
    Keywords: ANT-XXII/2; ANT-XXII/2_003-1; ANT-XXII/2_004-1; ANT-XXII/2_005-1; ANT-XXII/2_006-1; ANT-XXII/2_007-1; ANT-XXII/2_007-22; ANT-XXII/2_008-1; ANT-XXII/2_008-22; ANT-XXII/2_009-1; ANT-XXII/2_009-22; ANT-XXII/2_010-1; ANT-XXII/2_011-1; ANT-XXII/2_012-1; ANT-XXII/2_013-1; ANT-XXII/2_014-1; ANT-XXII/2_015-1; ANT-XXII/2_016-1; ANT-XXII/2_017-1; ANT-XXII/2_018-1; ANT-XXII/2_019-1; ANT-XXII/2_020-1; ANT-XXII/2_021-1; ANT-XXII/2_022-1; ANT-XXII/2_066-22; ANT-XXII/2_139-22; ANT-XXII/2_140-22; ANT-XXII/2_142-22; ANT-XXII/2_143-22; ANT-XXII/2_144-22; ANT-XXII/2_146-22; AWI_PhyOce; Calculated; Conductivity; CTD, SEA-BIRD SBE 19, SN 2715, modified for continuous data acquisition; CTD from ice float; CTDIF; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Elevation of event; Event label; Latitude of event; Longitude of event; Physical Oceanography @ AWI; Polarstern; Pressure, water; PS67 ISPOL; Salinity; Temperature, water; Temperature, water, potential; Weddell Sea
    Type: Dataset
    Format: text/tab-separated-values, 167622 data points
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  • 8
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    Physical oceanography from 120 CTD stations during POLARSTERN cruise ANT-XXII/2 (ISPOL) (2008)
    PANGAEA
    Details
    Publication Date: 2024-06-25
    Keywords: ANT-XXII/2; Attenuation, optical beam transmission; AWI_PhyOce; Calculated; Conductivity; CTD, Sea-Bird, SBE 911plus [SN: 0561]; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Elevation of event; Event label; Fluorometer; Fluorometer, Dr. Haardt Instruments; Latitude of event; Longitude of event; Number of observations; Physical Oceanography @ AWI; Polarstern; Pressure, water; PS67/005-1; PS67/006-10; PS67/006-100; PS67/006-101; PS67/006-102; PS67/006-103; PS67/006-104; PS67/006-105; PS67/006-108; PS67/006-109; PS67/006-11; PS67/006-110; PS67/006-111; PS67/006-113; PS67/006-115; PS67/006-116; PS67/006-118; PS67/006-12; PS67/006-120; PS67/006-121; PS67/006-122; PS67/006-123; PS67/006-126; PS67/006-127; PS67/006-128; PS67/006-13; PS67/006-130; PS67/006-131; PS67/006-132; PS67/006-133; PS67/006-134; PS67/006-135; PS67/006-136; PS67/006-137; PS67/006-139; PS67/006-14; PS67/006-140; PS67/006-142; PS67/006-143; PS67/006-144; PS67/006-146; PS67/006-15; PS67/006-18; PS67/006-19; PS67/006-2; PS67/006-20; PS67/006-21; PS67/006-22; PS67/006-23; PS67/006-25; PS67/006-26; PS67/006-27; PS67/006-29; PS67/006-3; PS67/006-30; PS67/006-32; PS67/006-33; PS67/006-34; PS67/006-35; PS67/006-38; PS67/006-39; PS67/006-4; PS67/006-40; PS67/006-41; PS67/006-43; PS67/006-44; PS67/006-45; PS67/006-47; PS67/006-48; PS67/006-49; PS67/006-5; PS67/006-50; PS67/006-51; PS67/006-53; PS67/006-54; PS67/006-55; PS67/006-56; PS67/006-57; PS67/006-59; PS67/006-6; PS67/006-61; PS67/006-62; PS67/006-63; PS67/006-65; PS67/006-66; PS67/006-67; PS67/006-68; PS67/006-7; PS67/006-70; PS67/006-71; PS67/006-72; PS67/006-73; PS67/006-74; PS67/006-75; PS67/006-76; PS67/006-78; PS67/006-79; PS67/006-80; PS67/006-81; PS67/006-82; PS67/006-84; PS67/006-85; PS67/006-86; PS67/006-87; PS67/006-89; PS67/006-9; PS67/006-90; PS67/006-91; PS67/006-92; PS67/006-94; PS67/006-95; PS67/006-96; PS67/006-98; PS67/006-99; PS67/007-1; PS67/008-1; PS67/009-1; PS67/011-1; PS67/011-2; PS67/011-3; PS67 ISPOL; Salinity; Scotia Sea, southwest Atlantic; Temperature, water; Temperature, water, potential; Weddell Sea
    Type: Dataset
    Format: text/tab-separated-values, 1565623 data points
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  • 9
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    Helium and neon measured on helicopter CTD samples during POLARSTERN cruise ANT-XXII/2 (ISPOL) (2008)
    PANGAEA
    Details
    Publication Date: 2024-06-25
    Keywords: ANT-XXII/2; ANT-XXII/2_003-1; ANT-XXII/2_005-1; ANT-XXII/2_006-1; ANT-XXII/2_007-1; ANT-XXII/2_008-1; ANT-XXII/2_009-1; ANT-XXII/2_010-1; ANT-XXII/2_011-1; ANT-XXII/2_012-1; ANT-XXII/2_013-1; ANT-XXII/2_014-1; ANT-XXII/2_015-1; ANT-XXII/2_017-1; ANT-XXII/2_018-1; ANT-XXII/2_019-1; ANT-XXII/2_020-1; ANT-XXII/2_022-1; CTD from ice float; CTDIF; Date/Time of event; DEPTH, water; Elevation of event; Event label; Helium; Isotope ratio mass spectrometry; Latitude of event; Longitude of event; Neon; Polarstern; PS67 ISPOL; Weddell Sea; δ Helium-3
    Type: Dataset
    Format: text/tab-separated-values, 51 data points
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    DATA PANGAEA
  • 10
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    Chlorofluorocarbons, helium, and neon measured on water bottle samples during POLARSTERN cruise ANT-XXII/2 (ISPOL) (2008)
    PANGAEA
    Details
    Publication Date: 2024-06-25
    Keywords: ANT-XXII/2; Bottle number; CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Elevation of event; Event label; Freon-11 (trichorofluoromethane); Freon-12 (dichlorodifluoromethane); Gas chromatography; Helium; ICE; Ice station; Isotope ratio mass spectrometry; Latitude of event; Longitude of event; Neon; Polarstern; PS67/005-1; PS67/006-1; PS67/006-103; PS67/006-108; PS67/006-115; PS67/006-120; PS67/006-126; PS67/006-13; PS67/006-131; PS67/006-135; PS67/006-139; PS67/006-142; PS67/006-25; PS67/006-32; PS67/006-38; PS67/006-4; PS67/006-43; PS67/006-48; PS67/006-53; PS67/006-61; PS67/006-65; PS67/006-66; PS67/006-70; PS67/006-74; PS67/006-79; PS67/006-84; PS67/006-89; PS67/006-94; PS67/006-99; PS67/007-1; PS67/008-1; PS67/009-1; PS67/011-3; PS67 ISPOL; Scotia Sea, southwest Atlantic; Weddell Sea; δ Helium-3
    Type: Dataset
    Format: text/tab-separated-values, 2374 data points
    Location Call Number Limitation Availability
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    DATA PANGAEA
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