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  • 2015-2019  (15)
Document type
Keywords
Publisher
Years
Year
  • 1
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    Ocean microstructure measurements in the Weddell Sea continental slope, Antarctica, during the RRS Ernest Shackleton cruise ES033 (2015)
    PANGAEA
    Details
    Publication Date: 2023-01-13
    Keywords: Conductivity sensor, SEA-BIRD SBE 4; DATE/TIME; DEPTH, water; Ernest Shackleton; ES033; ES033_vmp_004; ES033_vmp_005; ES033_vmp_006; ES033_vmp_007; ES033_vmp_008; ES033_vmp_009; ES033_vmp_010; ES033_vmp_011; ES033_vmp_012; ES033_vmp_013; ES033_vmp_015; ES033_vmp_016; ES033_vmp_017; ES033_vmp_018; ES033_vmp_019; ES033c_vmp_000; ES033c_vmp_002; ES033c_vmp_003; ES033c_vmp_004; ES033c_vmp_006; ES033c_vmp_007; ES033c_vmp_008; ES033c_vmp_009; ES033c_vmp_010; ES033c_vmp_011; ES033c_vmp_012; ES033c_vmp_013; ES033c_vmp_014; ES033c_vmp_015; ES033c_vmp_016; ES033c_vmp_017; ES033c_vmp_018; ES033c_vmp_019; ES033c_vmp_020; ES033c_vmp_021; ES033c_vmp_022; ES033c_vmp_023; ES033c_vmp_024; Event label; LATITUDE; LONGITUDE; MSD; Multi Sensor Device; Pressure, water; Rate of turbulent kinetic energy dissipation; Salinity; Sample elevation; Temperature, water; Temperature sensor, SEA-BIRD SBE 3; Vertical Microstructure Profiler, Rockland Scientific, VMP-2000 SN 009
    Type: Dataset
    Format: text/tab-separated-values, 53577 data points
    Location Call Number Limitation Availability
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    DATA PANGAEA
  • 2
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    Current measurements from LADCP in the Weddell Sea, Antarctica, during the RRS Ernest Shackleton cruise ES033 (2015)
    PANGAEA
    Details
    Publication Date: 2023-02-20
    Keywords: Acoustic Doppler Current Profiling (LADCP) [lowered with CTD]; Current velocity, east-west; Current velocity, error; Current velocity, north-south; DATE/TIME; DEPTH, water; Ernest Shackleton; ES033; ES033_ctd_002; ES033_ctd_003; ES033_ctd_004; ES033_ctd_005; ES033_ctd_006; ES033_ctd_007; ES033_ctd_008; ES033_ctd_009; ES033_ctd_010; ES033_ctd_011; ES033_ctd_012; ES033_ctd_013; ES033_ctd_014; ES033_ctd_015; ES033_ctd_016; ES033_ctd_017; ES033_ctd_018; ES033_ctd_019; ES033_ctd_020; ES033_ctd_021; ES033_ctd_022; ES033_ctd_023; ES033_ctd_024; ES033_ctd_025; ES033_ctd_026; ES033_ctd_027; ES033_ctd_028; ES033_ctd_029; ES033_ctd_030; ES033_ctd_031; ES033_ctd_032; ES033_ctd_033; ES033_ctd_034; ES033_ctd_035; ES033_ctd_036; ES033_ctd_037; ES033_ctd_038; ES033_ctd_039; ES033_ctd_040; ES033_ctd_041; ES033_ctd_042; ES033_ctd_043; ES033_ctd_044; ES033_ctd_045; ES033_ctd_046; ES033_ctd_047; ES033_ctd_048; ES033_ctd_049; ES033_ctd_050; ES033_ctd_051; ES033_ctd_052; ES033_ctd_053; ES033_ctd_054; ES033_ctd_055; ES033_ctd_056; ES033_ctd_057; ES033_ctd_058; ES033_ctd_059; ES033_ctd_087; ES033_ctd_088; ES033_ctd_089; ES033_ctd_090; ES033_ctd_091; ES033_ctd_092; ES033_ctd_093; ES033_ctd_094; ES033_ctd_095; ES033_ctd_096; ES033_ctd_097; ES033_ctd_098; ES033_ctd_099; ES033_ctd_100; ES033_ctd_101; ES033_ctd_102; ES033_ctd_103; ES033_ctd_104; ES033_ctd_105; ES033_ctd_106; ES033_ctd_107; ES033_ctd_108; ES033_ctd_109; ES033_ctd_110; ES033_ctd_111; ES033_ctd_112; ES033_ctd_113; ES033_ctd_114; ES033_ctd_115; ES033_ctd_116; ES033_ctd_117; ES033_ctd_118; ES033_ctd_119; ES033_ctd_120; ES033_ctd_121; ES033_ctd_122; ES033_ctd_123; ES033_ctd_124; ES033_ctd_125; ES033_ctd_126; ES033_ctd_127; ES033_ctd_128; ES033_ctd_129; ES033_ctd_130; ES033_ctd_131; ES033_ctd_132; ES033_ctd_133; ES033_ctd_134; ES033_ctd_135; ES033_ctd_136; ES033_ctd_137; ES033_ctd_138; ES033_ctd_139; ES033_ctd_140; ES033_ctd_141; ES033_ctd_142; ES033_ctd_143; ES033_ctd_144; ES033_ctd_145; ES033_ctd_146; ES033_ctd_147; ES033_ctd_148; ES033_ctd_149; ES033_ctd_150; ES033_ctd_151; ES033_ctd_152; ES033_ctd_153; ES033_ctd_154; ES033_ctd_155; ES033_ctd_156; ES033_ctd_157; ES033_ctd_158; ES033_ctd_159; ES033_ctd_160; ES033_ctd_161; ES033_ctd_162; ES033_ctd_163; ES033_ctd_164; ES033_ctd_166; Event label; LATITUDE; LONGITUDE; Pressure, water; Sample amount; Sample elevation
    Type: Dataset
    Format: text/tab-separated-values, 236304 data points
    Location Call Number Limitation Availability
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    DATA PANGAEA
  • 3
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    Temperature and current measurements in the Weddell Sea at mooring site Fr1 (2017)
    PANGAEA
    In:  Alfred Wegener Institute for Polar and Marine Research, Bremerhaven (1986-2013)
    Details
    Publication Date: 2023-09-06
    Keywords: Current velocity, east-west; Current velocity, north-south; DATE/TIME; DEPTH, water; Fr1_TUV; Gear identification number; Mooring (long time); MOORY; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 166040 data points
    Location Call Number Limitation Availability
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    DATA PANGAEA
  • 4
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    Temperature and current measurements in the Weddell Sea at mooring site Fr2 (2017)
    PANGAEA
    In:  Alfred Wegener Institute for Polar and Marine Research, Bremerhaven (1986-2013)
    Details
    Publication Date: 2023-09-06
    Keywords: Current velocity, east-west; Current velocity, north-south; DATE/TIME; DEPTH, water; Fr2_TUV; Gear identification number; Mooring (long time); MOORY; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 162392 data points
    Location Call Number Limitation Availability
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    DATA PANGAEA
  • 5
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    Physical oceanography from CTD in the Weddell Sea, Antarctica, during the RRS Ernest Shackleton cruise ES033 (2015)
    PANGAEA
    Details
    Publication Date: 2023-09-06
    Keywords: CTD, SEA-BIRD SBE 9 plus; DATE/TIME; DEPTH, water; Ernest Shackleton; ES033; ES033_ctd_001; ES033_ctd_002; ES033_ctd_003; ES033_ctd_004; ES033_ctd_005; ES033_ctd_006; ES033_ctd_007; ES033_ctd_008; ES033_ctd_009; ES033_ctd_010; ES033_ctd_011; ES033_ctd_012; ES033_ctd_013; ES033_ctd_014; ES033_ctd_015; ES033_ctd_016; ES033_ctd_017; ES033_ctd_018; ES033_ctd_019; ES033_ctd_020; ES033_ctd_021; ES033_ctd_022; ES033_ctd_023; ES033_ctd_024; ES033_ctd_025; ES033_ctd_026; ES033_ctd_027; ES033_ctd_028; ES033_ctd_029; ES033_ctd_030; ES033_ctd_031; ES033_ctd_032; ES033_ctd_033; ES033_ctd_034; ES033_ctd_035; ES033_ctd_036; ES033_ctd_037; ES033_ctd_038; ES033_ctd_039; ES033_ctd_040; ES033_ctd_041; ES033_ctd_042; ES033_ctd_043; ES033_ctd_044; ES033_ctd_045; ES033_ctd_046; ES033_ctd_047; ES033_ctd_048; ES033_ctd_049; ES033_ctd_050; ES033_ctd_051; ES033_ctd_052; ES033_ctd_053; ES033_ctd_054; ES033_ctd_055; ES033_ctd_056; ES033_ctd_057; ES033_ctd_058; ES033_ctd_059; ES033_ctd_060; ES033_ctd_061; ES033_ctd_062; ES033_ctd_063; ES033_ctd_064; ES033_ctd_065; ES033_ctd_066; ES033_ctd_067; ES033_ctd_068; ES033_ctd_069; ES033_ctd_070; ES033_ctd_071; ES033_ctd_072; ES033_ctd_073; ES033_ctd_074; ES033_ctd_075; ES033_ctd_076; ES033_ctd_077; ES033_ctd_078; ES033_ctd_079; ES033_ctd_080; ES033_ctd_081; ES033_ctd_082; ES033_ctd_083; ES033_ctd_084; ES033_ctd_085; ES033_ctd_086; ES033_ctd_087; ES033_ctd_088; ES033_ctd_089; ES033_ctd_090; ES033_ctd_091; ES033_ctd_092; ES033_ctd_093; ES033_ctd_094; ES033_ctd_095; ES033_ctd_096; ES033_ctd_097; ES033_ctd_098; ES033_ctd_099; ES033_ctd_100; ES033_ctd_101; ES033_ctd_102; ES033_ctd_103; ES033_ctd_104; ES033_ctd_105; ES033_ctd_106; ES033_ctd_107; ES033_ctd_108; ES033_ctd_109; ES033_ctd_110; ES033_ctd_111; ES033_ctd_112; ES033_ctd_113; ES033_ctd_114; ES033_ctd_115; ES033_ctd_116; ES033_ctd_117; ES033_ctd_118; ES033_ctd_119; ES033_ctd_120; ES033_ctd_121; ES033_ctd_122; ES033_ctd_123; ES033_ctd_124; ES033_ctd_125; ES033_ctd_126; ES033_ctd_127; ES033_ctd_128; ES033_ctd_129; ES033_ctd_130; ES033_ctd_131; ES033_ctd_132; ES033_ctd_133; ES033_ctd_134; ES033_ctd_135; ES033_ctd_136; ES033_ctd_137; ES033_ctd_138; ES033_ctd_139; ES033_ctd_140; ES033_ctd_141; ES033_ctd_142; ES033_ctd_143; ES033_ctd_144; ES033_ctd_145; ES033_ctd_146; ES033_ctd_147; ES033_ctd_148; ES033_ctd_149; ES033_ctd_150; ES033_ctd_151; ES033_ctd_152; ES033_ctd_153; ES033_ctd_154; ES033_ctd_155; ES033_ctd_156; ES033_ctd_157; ES033_ctd_158; ES033_ctd_159; ES033_ctd_160; ES033_ctd_161; ES033_ctd_162; ES033_ctd_163; ES033_ctd_164; ES033_ctd_165; ES033_ctd_166; Event label; LATITUDE; LONGITUDE; Pressure, water; Salinity; Sample elevation; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 729770 data points
    Location Call Number Limitation Availability
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    DATA PANGAEA
  • 6
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    Measurements of ocean microstructure, physical oceanography and current in the Weddell Sea, Antarctica, during the RRS Ernest Shackleton cruises ES033 and ES060 (2015)
    PANGAEA
    In:  Supplement to: Fer, Ilker; Darelius, Elin; Daae, Kjersti (2016): Observations of energetic turbulence on the Weddell Sea continental slope. Geophysical Research Letters, 43(2), 760-766, https://doi.org/10.1002/2015GL067349
    Details
    Publication Date: 2023-09-06
    Description: Turbulence profile measurements made on the upper continental slope and shelf of the southeastern Weddell Sea reveal striking contrasts in dissipation and mixing rates between the two sites. The mean profiles of dissipation rates from the upper slope are 1-2 orders of magnitude greater than the profiles collected over the shelf in the entire water column. The difference increases toward the bottom where the dissipation rate of turbulent kinetic energy and the vertical eddy diffusivity on the slope exceed 10-7 W kg-1 and 10-2 m2 s-1, respectively. Elevated levels of turbulence on the slope are concentrated within a 100 m thick bottom layer, which is absent on the shelf. The upper slope is characterized by near-critical slopes and is in close proximity to the critical latitude for semidiurnal internal tides. Our observations suggest that the upper continental slope of the southern Weddell Sea is a generation site of semidiurnal internal tide, which is trapped along the slope along the critical latitude, and dissipates its energy in a inline image m thick layer near the bottom and within inline image km across the slope.
    Type: Dataset
    Format: application/zip, 4 datasets
    Location Call Number Limitation Availability
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    DATA PANGAEA
  • 7
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    Temperature and current measurements in the Weddell Sea at mooring site Fr1 and Fr2 (2017)
    PANGAEA
    In:  Alfred Wegener Institute for Polar and Marine Research, Bremerhaven (1986-2013)
    Details
    Publication Date: 2023-09-06
    Description: In 1995, two current meter moorings where deployed in the Weddell Sea at the northern exit of the Filchner Trough, during a cruise with the vessel Polarstern. At the two sites, Fr1 and Fr2, temperature and currents were measured at various depths. The moorings were recovered in 1998. For more details see reference Woodgate et al. (1998).
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
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    DATA PANGAEA
  • 8
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    Noble gas measurements beneath Filchner-Ronne Ice Sheet (2017)
    PANGAEA
    In:  Supplement to: Huhn, Oliver; Hattermann, Tore; Davis, Peter E D; Dunker, Erich; Hellmer, Hartmut H; Nicholls, Keith W; Østerhus, Svein; Rhein, Monika; Schröder, Michael; Sültenfuß, Jürgen (2018): Basal Melt and Freezing Rates From First Noble Gas Samples Beneath an Ice Shelf. Geophysical Research Letters, 45(16), 8455-8461, https://doi.org/10.1029/2018GL079706
    Details
    Publication Date: 2024-02-16
    Description: A climatically induced acceleration in ocean‐driven melting of Antarctic ice shelves would have consequences for both the discharge of continental ice into the ocean and thus global sea level, and for the formation of Antarctic Bottom Water and the oceanic meridional overturning circulation. Using a novel gas‐tight in situ water sampler, noble gas samples have been collected from six locations beneath the Filchner Ice Shelf, the first such samples from beneath an Antarctic ice shelf. Helium and neon are uniquely suited as tracers of glacial meltwater in the ocean. Basal meltwater fractions range from 3.6% near the ice shelf base to 0.5% near the sea floor, with distinct regional differences. We estimate an average basal melt rate for the Filchner‐Ronne Ice Shelf of 177 ± 95 Gt/year, independently confirming previous results. We calculate that up to 2.7% of the meltwater has been refrozen, and we identify a local source of crustal helium.
    Keywords: Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; SPP1158
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
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    DATA PANGAEA
  • 9
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    Filchner Ice Shelf cavity noble gas (helium and neon) measurements (2017)
    PANGAEA
    Details
    Publication Date: 2024-05-22
    Keywords: ANT-Land_2015/16_FISP; ANT-Land_2016/17_FISP; AWI Antarctic Land Expedition; CTD; CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Distance; Event label; Filchner Shelf; FISP_FNE1-1; FISP_FNE2-9; FISP_FNE3-12; FISP_FNE3-13; FISP_FSE1-19; FISP_FSE2-10; FISP_FSE2-11; FISP_FSE2-12; FISP_FSE2-13; FISP_FSW2-23; FISP_FSW2-24; Freeboard; Helium-3; Helium-4; Ice thickness; Latitude of event; Longitude of event; Neon; Pressure, total; Pressure, water; Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; Salinity; Sample ID; SPP1158; Temperature, water, potential; δ Helium-3
    Type: Dataset
    Format: text/tab-separated-values, 220 data points
    Location Call Number Limitation Availability
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    DATA PANGAEA
  • 10
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    Basal Melt and Freezing Rates From First Noble Gas Samples Beneath an Ice Shelf (2018)
    Wiley
    In:  EPIC3Geophysical Research Letters, Wiley, 45(16), pp. 8455-8461, ISSN: 00948276
    Details
    Publication Date: 2018-09-27
    Description: A climatically-induced acceleration in ocean-driven melting of Antarctic ice shelves would have consequences for both the discharge of continental ice into the ocean and thus global sea level, and for the formation of Antarctic Bottom Water and the oceanic meridional overturning circulation. Using a novel gas-tight in-situ water sampler, noble gas samples have been collected from six locations beneath the Filchner Ice Shelf, the first such samples from beneath an Antarctic Ice shelf. Helium and neon are uniquely suited as tracers of glacial meltwater in the ocean. Basal meltwater fractions range from 3.6% near the ice shelf base to 0.5% near the sea floor, with distinct regional differences. We estimate an average basal melt rate for the Filchner-Ronne Ice Shelf of 177 ± 95 Gt/year, independently confirming previous results. We calculate that up to 2.7% of the meltwater has been refrozen, and we identify a local source of crustal helium.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
    Location Call Number Limitation Availability
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    PAPER (OA)
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