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  • 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  (1)
  • Marine Mammal Tracking; MMT  (1)
  • Submesoscale instabilities  (1)
Document type
Keywords
Years
  • 1
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Roquet, Fabien; Wunsch, Carl; Forget, Gael; Heimbach, Patrick; Guinet, Christophe; Reverdin, Gilles; Charrassin, Jean-Benoît; Bailleul, Frederic; Costa, Daniel P; Huckstadt, Luis A; Goetz, Kimberly T; Kovacs, Kit Maureen; Lydersen, Christian; Biuw, Martin; Nøst, Ole Anders; Bornemann, Horst; Plötz, Joachim; Bester, Marthán Nieuwoudt; McIntyre, Trevor; Muelbert, Monica C; Hindell, Mark A; McMahon, Clive R; Williams, Guy; Harcourt, Robert; Field, Iain C; Chafik, Leon; Nicholls, Keith W; Boehme, Lars; Fedak, Mike A (2013): Estimates of the Southern Ocean general circulation improved by animal-borne instruments. Geophysical Research Letters, 40(23), 6176-6180, https://doi.org/10.1002/2013GL058304
    Publication Date: 2023-05-12
    Description: Over the last decade, several hundred seals have been equipped with conductivity-temperature-depth sensors in the Southern Ocean for both biological and physical oceanographic studies. A calibrated collection of seal-derived hydrographic data is now available, consisting of more than 165,000 profiles. The value of these hydrographic data within the existing Southern Ocean observing system is demonstrated herein by conducting two state estimation experiments, differing only in the use or not of seal data to constrain the system. Including seal-derived data substantially modifies the estimated surface mixedlayer properties and circulation patterns within and south of the Antarctic Circumpolar Current. Agreement with independent satellite observations of sea ice concentration is improved, especially along the East Antarctic shelf. Instrumented animals efficiently reduce a critical observational gap, and their contribution to monitoring polar climate variability will continue to grow as data accuracy and spatial coverage increase.
    Keywords: Marine Mammal Tracking; MMT
    Type: Dataset
    Format: application/zip, 29 datasets
    Location Call Number Limitation Availability
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  • 2
    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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  • 3
    Publication Date: 2022-10-26
    Description: Author Posting. © National Academy of Sciences, 2019. This article is posted here by permission of National Academy of Sciences for personal use, not for redistribution. The definitive version was published in Proceedings of the National Academy of Sciences 116(27), (2019): 13233-13238, doi: 10.1073/pnas.1904087116.
    Description: The overturning circulation of the global ocean is critically shaped by deep-ocean mixing, which transforms cold waters sinking at high latitudes into warmer, shallower waters. The effectiveness of mixing in driving this transformation is jointly set by two factors: the intensity of turbulence near topography and the rate at which well-mixed boundary waters are exchanged with the stratified ocean interior. Here, we use innovative observations of a major branch of the overturning circulation—an abyssal boundary current in the Southern Ocean—to identify a previously undocumented mixing mechanism, by which deep-ocean waters are efficiently laundered through intensified near-boundary turbulence and boundary–interior exchange. The linchpin of the mechanism is the generation of submesoscale dynamical instabilities by the flow of deep-ocean waters along a steep topographic boundary. As the conditions conducive to this mode of mixing are common to many abyssal boundary currents, our findings highlight an imperative for its representation in models of oceanic overturning.
    Description: The DynOPO project is supported by the UK Natural Environment Research Council (grants NE/K013181/1 and NE/K012843/1) and the US National Science Foundation (grants OCE-1536453 and OCE-1536779). A.C.N.G. acknowledges the support of the Royal Society and the Wolfson Foundation. S.L. acknowledges the support of award NA14OAR4320106 from the National Oceanic and Atmospheric Administration, US Department of Commerce. The statements, findings, conclusions, and recommendations are those of the authors, and do not necessarily reflect the views of the National Oceanic and Atmospheric Administration, or the US Department of Commerce. We are grateful to the scientific party, crew, and technicians on the RRS James Clark Ross for their hard work during data collection.
    Description: 2019-12-18
    Keywords: Ocean mixing ; Overturning circulation ; Submesoscale instabilities ; Turbulence
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Location Call Number Limitation Availability
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