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  • 1
    Electronic Resource
    Electronic Resource
    Hydrographic and current measurements in the Fram Strait, August 1981 (1983)
    Oxford, UK : Blackwell Publishing Ltd
    Polar research 1 (1983), S. 0 
    Details
    ISSN: 1751-8369
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geography , Geosciences
    Notes: The hydrographic (CTD) observations and pendulum current measurements obtained with M/S ‘Lance’ in August 1981 in the area west and north of Spitsbergen, are presented. The warm and saline northward flow, known as the West Spitsbergen Current, is found to follow the shelf break. In the Fram Strait the hydrographic structure is complicated because of eddies and other transient movements. The current measurements suggest a two-layer structure where the velocity vector rotates in opposite directions in the two layers with a period near the semidiurnal tidal period.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1751-8369.1983.tb00696.x
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    Paper (German National Licenses)
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  • 2
    Electronic Resource
    Electronic Resource
    The θ-S relations in the northern seas: Implications for the deep circulation (1986)
    Oxford, UK : Blackwell Publishing Ltd
    Polar research 4 (1986), S. 0 
    Details
    ISSN: 1751-8369
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geography , Geosciences
    Notes: The θ-S relations for the cold, saline deep and bottom waters in the Greenland and Norwegian Seas and the Polar Ocean are displayed and discussed. The differences in θ-S curves are explained by a mixing of the deep water masses and by the injection of waters from above consisting of cold dense water formed by cooling and ice formation at the sea surface and entrained warm water from the intermediate layers. Estimates of the strength of the deep water circulation are based upon the changes in θ-S curves and on some assumptions about the transformations of the Bering Strait inflow in the Chukchi Sea and on the Alaskan shelf.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1751-8369.1986.tb00527.x
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  • 3
    Electronic Resource
    Electronic Resource
    The outflow of polar water through the Arctic Archipelago and the oceanographic conditions in Baffin Bay (1986)
    Oxford, UK : Blackwell Publishing Ltd
    Polar research 4 (1986), S. 0 
    Details
    ISSN: 1751-8369
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geography , Geosciences
    Notes: The transports of mass, heat, and salt through the Arctic Archipelago are estimated by two different approaches. First: A baroclinic, rotationally controlled flow is assumed through the Arctic Archipelago and the Davis Strait, with all passages transporting at maximum capacity. Second: Mass, salt, and energy balances are considered for the upper ‘cold core’ in Baffin Bay. The mass transport in the first case decreases and in the second case increases with increasing salinity in the Beaufort Sea. It is thus possible to determine a salinity at which both approaches give the same mass transport. The outflow in the upper layers is estimated at 0.7 · 109 kg s−1 with a salinity of 32.9. The amount of water from the Polar Ocean entering the deeper (Atlantic) layer in Baffin Bay is more difficult to assess. A tentative value of 0.3 10·kg s−1 with a salinity cf 34.3 is proposed.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1751-8369.1986.tb00528.x
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  • 4
    Electronic Resource
    Electronic Resource
    Atlantic sources of the Arctic Ocean surface and halocline waters (2004)
    Oxford, UK : Blackwell Publishing Ltd
    Polar research 23 (2004), S. 0 
    Details
    ISSN: 1751-8369
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geography , Geosciences
    Notes: Data obtained during the last 20 years from selected hydrographic stations throughout the Arctic Ocean basins and at the continental slopes and northern parts of the surrounding shelf seas are examined to estimate the contribution of Atlantic water to the upper part of the Arctic Ocean water column, and to follow the circulation of the Atlantic derived halocline waters around the Arctic Ocean basins. A substantial fraction of the Atlantic water entering the Arctic Ocean in the two inflow branches, the Fram Strait branch and the Barents Sea branch, is transformed into less dense waters. The inflow through Fram Strait encounters and melts sea ice. Its upper part becomes less saline, and in winter, ice formation homogenizes this low salinity upper part into a winter mixed layer, which follows the boundary flow eastward. The inflow over the Barents Sea mainly becomes colder, less saline and denser due to cooling and net precipitation, but melting of sea ice also here creates a less dense upper layer, which is subsequently homogenized by haline convection. Both these components enter the Nansen Basin via the St. Anna Trough and flow eastward along the Siberian continental slope. A third component of the Barents Sea inflow, mainly comprising Norwegian Coastal Current water, remains on the shelf, where it absorbs the runoff from the large Siberian rivers and evolves into low salinity shelf water. This part continues as far east as the Laptev Sea before a major inflow to the deep Arctic Ocean basins occurs. Winter convection, which in most of the Nansen Basin extends to the Atlantic layer, then becomes limited to the injected low salinity shelf water, and the more saline upper layers of the Fram Strait and the Barents Sea branches are transformed into halocline waters. The Fram Strait branch supplies the halocline water of the Amundsen, Makarov and part of the Canada basins, while the upper part of the Barents Sea branch, initially confined to the Siberian continental slope, becomes the main source of the lower halocline below the Pacific water in the Canada Basin beyond the Chukchi Cap. Less dense Pacific water close to the North American continent prevents the Atlantic derived upper layers from flowing through the Canadian Arctic Archipelago and their main exit is Fram Strait. Only some of the Barents Sea branch halocline water passes through Nares Strait and may occasionally renew the deep and bottom waters of Baffin Bay.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1751-8369.2004.tb00007.x
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  • 5
    Electronic Resource
    Electronic Resource
    The early Miocene onset of a ventilated circulation regime in the Arctic Ocean (2007)
    [s.l.] : Nature Publishing Group
    Nature 447 (2007), S. 986-990 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Deep-water formation in the northern North Atlantic Ocean and the Arctic Ocean is a key driver of the global thermohaline circulation and hence also of global climate. Deciphering the history of the circulation regime in the Arctic Ocean has long been prevented by the lack of data from cores ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/nature05924
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  • 6
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    Unknown
    Physical oceanography during POLARSTERN cruise ARK-XIII/2 (2010)
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Details
    Publication Date: 2023-03-16
    Keywords: ARK-XIII/2; AWI_PhyOce; Barents Sea; Calculated; Computed; Conductivity; CTD, SEA-BIRD SBE 911plus, SN 313; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; East Greenland continental slope; Elevation of event; Event label; Latitude of event; Longitude of event; Physical Oceanography @ AWI; Polarstern; Pressure, water; PS44; PS44/039-1; PS44/040-1; PS44/041-1; PS44/042-1; PS44/043-1; PS44/044-1; PS44/045-1; PS44/046-1; PS44/047-1; PS44/048-1; PS44/049-1; PS44/050-1; PS44/051-1; PS44/052-1; PS44/053-1; PS44/054-1; PS44/055-1; PS44/056-1; PS44/057-1; PS44/058-1; PS44/059-1; PS44/060-1; PS44/061-1; PS44/062-1; PS44/063-1; PS44/064-1; PS44/065-1; PS44/066-1; PS44/067-1; PS44/068-1; PS44/069-1; PS44/070-1; PS44/072-1; PS44/073-1; PS44/074-1; PS44/075-1; PS44/076-1; PS44/077-1; PS44/078-1; PS44/079-1; PS44/082-1; PS44/084-1; PS44/086-1; PS44/087-1; PS44/088-1; PS44/089-1; PS44/090-1; PS44/091-1; PS44/092-1; PS44/093-1; PS44/094-1; PS44/096-1; PS44/097-1; PS44/098-1; PS44/099-1; Salinity; Temperature, water; Temperature, water, potential; W Spitzbergen; Yermak Plateau
    Type: Dataset
    Format: text/tab-separated-values, 381714 data points
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    DATA PANGAEA
  • 7
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    Unknown
    Data compilation of ESOP
    PANGAEA
    In:  International Council for the Exploration of the Sea, Copenhagen
    Details
    Publication Date: 2023-05-12
    Description: The work in this sub-project of ESOP focuses on the advective and convective transforma-tion of water masses in the Greenland Sea and its neighbouring areas. It includes observational work on the sub-mesoscale and analysis of hydrographic data up to the gyre-scale. Observations of active convective plumes were made with a towed chain equipped with up to 80 CTD sensors, giving a horizontal and vertical resolution of the hydrographic fields of a few metres. The observed scales of the penetrative convective plumes compare well with those given by theory. On the mesoscale the structure of homogeneous eddies formed as a result of deep convection was observed and the associated mixing and renewal of the intermediate layers quantified. The relative importance and efficiency of thermal and haline penetrative convection in relation to the surface boundary conditions (heat and salt fluxes and ice cover) and the ambient stratification are studied using the multi year time series of hydro-graphic data in the central Greenland Sea. The modification of the water column of the Greenland Sea gyre through advection from and mixing with water at its rim is assessed on longer time scales. The relative contributions are quantified using modern water mass analysis methods based on inverse techniques. Likewise the convective renewal and the spreading of the Arctic Intermediate Water from its formation area is quantified. The aim is to budget the heat and salt content of the water column, in particular of the low salinity surface layer, and to relate its seasonal and interannual variability to the lateral fluxes and the fluxes at the air-sea-ice interface. This will allow to estimate residence times for the different layers of the Greenland Sea gyre, a quantity important for the description of the Polar Ocean carbon cycle.
    Keywords: 1; 10; 101; 11; 12; 13; 14; 15; 16; 162; 17; 18; 19; 2; 20; 21; 22; 23; 24; 25; 26; 262; 27; 28; 29; 3; 30; 31; 32; 33; 34; 35; 36; 362; 37; 38; 39; 4; 40; 41; 42; 43; 44; 45; 46; 462; 47; 48; 49; 5; 50; 51; 52; 53; 54; 55; 56; 57; 58; 59; 6; 60; 61; 62; 63; 64; 65; 66; 67; 68; 69; 7; 70; 71; 72; 73; 74; 75; 76; 77; 78; 79; 8; 80; 81; 82; 83; 84; 85; 87; 88; 89; 9; 90; 91; 92; 93; ARK-XIII/3; B02/98; B02/98-1001; B02/98-1011; B02/98-1021; B02/98-1031; B02/98-1061; B02/98-1062; B02/98-1071; B02/98-1081; B02/98-1101; B02/98-1111; B02/98-1121; B02/98-1131; B02/98-1141; B02/98-1151; B02/98-1181; B02/98-1191; B02/98-1221; B02/98-1222; B02/98-1231; B02/98-1241; B02/98-1251; B02/98-1261; B02/98-1271; B02/98-1281; B02/98-1291; B02/98-1292; B02/98-1293; B02/98-1301; B02/98-1311; B02/98-1321; B02/98-1361; B02/98-1371; B02/98-1381; B02/98-1391; B02/98-1401; B02/98-1411; B02/98-1421; B02/98-1431; B02/98-1441; B02/98-1451; B02/98-1461; B02/98-1471; B02/98-1481; B02/98-1491; B02/98-1501; B02/98-1511; B02/98-1521; B02/98-1531; B02/98-1541; B02/98-1551; B02/98-1561; B02/98-1571; B02/98-1581; B02/98-1591; B02/98-1601; B02/98-1611; B02/98-1622; B02/98-531; B02/98-541; B02/98-551; B02/98-561; B02/98-571; B02/98-581; B02/98-591; B02/98-601; B02/98-621; B02/98-622; B02/98-631; B02/98-641; B02/98-651; B02/98-661; B02/98-671; B02/98-681; B02/98-691; B02/98-701; B02/98-711; B02/98-721; B02/98-731; B02/98-751; B02/98-761; B02/98-771; B02/98-781; B02/98-791; B02/98-801; B02/98-811; B02/98-821; B02/98-831; B02/98-843; B02/98-845; B02/98-851; B02/98-861; B02/98-891; B02/98-901; B02/98-911; B02/98-921; B02/98-931; B02/98-941; B02/98-961; B02/98-971; B02/98-972; B02/98-973; B02/98-981; B02/98-991; B03/97; B03/97-531; B03/97-532; B03/97-551; B03/97-552; B03/97-711; B03/97-712; B03/97-751; B03/97-752; B03/97-753; B03/97-771; B03/97-772; B03/97-781; B03/97-782; B03/97-931; B03/97-932; B05/96; B05/96-1252; B05/96-252; B05/96-253; B05/96-254; B05/96-263; B05/96-278; B05/96-293-2; B06/97; B06/97-1431; B06/97-1441; B06/97-1451; B06/97-1461; B06/97-1471; B06/97-1481; B06/97-1492; B06/97-1501; B06/97-1511; B06/97-1512; B06/97-1513; B06/97-1521; B06/97-1531; B06/97-1541; B06/97-1551; B06/97-1561; B06/97-1571; B06/97-1581; B06/97-1591; B06/97-1601; B06/97-1611; B06/97-1621; B06/97-1631; B06/97-1643; B06/97-1644; B06/97-1651; B06/97-1661; B06/97-1671; B06/97-1681; B06/97-1691; B06/97-1701; B06/97-1711; B06/97-1721; B06/97-1731; B06/97-1741; B06/97-1751; B06/97-1761; B06/97-1772; B06/97-1773; B06/97-1781; B06/97-1791; B06/97-1801; B06/97-1811; B06/97-1821; B06/97-1831; B06/97-1841; B06/97-1851; B06/97-1861; B06/97-1871; B06/97-1881; B06/97-1891; B06/97-1901; B06/97-1911; B06/97-1912; B06/97-1921; B06/97-1931; B06/97-1941; B06/97-1951; B06/97-1971; B06/97-1981; B06/97-1991; B06/97-2001; B06/97-2011; B06/97-2021; B06/97-2031; B06/97-2041; B06/97-2051; B06/97-2061; B06/97-2071; B06/97-2081; B06/97-2091; B06/97-2101; B06/97-2121; B06/97-2122; B06/97-2131; B06/97-2141; B06/97-2142; B06/97-2151; B06/97-2161; B06/97-2171; B06/97-2181; B06/97-2191; B06/97-2211; B06/97-2221; B06/97-2231; B06/97-2241; B06/97-2251; B06/97-2261; B06/97-2271; B06/97-2281; B06/97-2291; B06/97-2301; B06/97-2311; B06/97-2321; B06/97-2331; B06/97-2341; B06/97-2351; B06/97-2361; B06/97-2371; B06/97-2381; B06/97-2391; B06/97-2401; B06/97-2411; B06/97-2421; B06/97-2431; B06/97-2441; B06/97-2451; B06/97-2461; B06/98; B06/98-2531; B06/98-2541; B06/98-2551; B06/98-2561; B06/98-2571; B06/98-2581; B06/98-2582; B06/98-2591; B06/98-2592; B06/98-2601; B06/98-2611; B06/98-2612; B06/98-2621; B06/98-2631; B06/98-2641; B06/98-2642; B06/98-2651; B06/98-2652; B06/98-2661; B06/98-2671; B06/98-2672; B06/98-2681; B06/98-2691; B06/98-2701; B06/98-2711; B06/98-2721; B06/98-2741; B06/98-2751; B06/98-2761; B06/98-2771; B06/98-2781; B06/98-2791; B06/98-2801; B06/98-2811; B06/98-2821; B06/98-2831; B06/98-2841; B06/98-2851; B06/98-2861; B06/98-2871; B06/98-2881; B06/98-2891; B06/98-2901; B06/98-2911; B06/98-2921; B06/98-2931; B06/98-2941; B06/98-2951; B06/98-2961; B06/98-2971; B06/98-2981; B06/98-2991; B06/98-3001; B06/98-3002; B06/98-3003; B06/98-3004; B06/98-3011; B06/98-3012; B06/98-3021; B06/98-3031; B06/98-3041; B06/98-3051; B06/98-3081; B06/98-3101; B06/98-3102; B06/98-3103; B06/98-3104; B06/98-3121; B06/98-3141; B06/98-3142; B06/98-3143; B06/98-3144; B06/98-3161; B06/98-3171; B06/98-3181; B06/98-3191; B06/98-3201; B06/98-3211; B06/98-3221; B06/98-3231; B06/98-3241; B06/98-3251; B06/98-3261; B06/98-3271; B06/98-3321; B06/98-3331; B06/98-3341; B06/98-3351; B06/98-3361; B06/98-3371; B06/98-3381; B06/98-3391; B06/98-3401; B06/98-3441; B06/98-3451; B06/98-3461; B06/98-3481; B06/98-3482; B06/98-3483; B06/98-3511; B06/98-3522; B06/98-3531; B06/98-3541; B06/98-3551; B06/98-3561; B06/98-3581; B06/98-3591; B06/98-3611; B06/98-3621; B06/98-3631; B06/98-3641; B06/98-3651; B06/98-3661; B06/98-3671; B06/98-3681; B06/98-3691; B06/98-3701; B06/98-3711; B06/98-3731; B06/98-3741; B06/98-3751; B06/98-3761; B06/98-3771; B06/98-3781; B06/98-3791; B09/96; B09/96-5311; B09/96-5312; B09/96-5321; B09/96-5322; B09/96-5351; B09/96-5352; B09/96-5353; B09/96-5451; B09/96-5452; B09/96-5481; B09/96-5482; B09/96-5511; B09/96-5512; B09/96-5521; B09/96-5522; B09/96-5531; B09/96-5532; B09/98; B09/98-5432; B09/98-5433; B09/98-5434; B09/98-5441; B09/98-5451; B09/98-5461; B09/98-5471; B09/98-5481; B09/98-5491; B09/98-5501; B09/98-5511; B09/98-5531; B09/98-5541; B09/98-5551; B09/98-5561; B09/98-5581; B09/98-5601; B09/98-5631; B09/98-5641; B09/98-5651; B09/98-5661; B09/98-5671; B09/98-5681; B09/98-5711; B09/98-5731; B09/98-5732; B09/98-5741; B09/98-5751; B09/98-5771; B09/98-5791; B09/98-5792; B09/98-5801; B09/98-5804; B09/98-5805; B10/97; B10/97-3601; B10/97-3602; B10/97-3851; B10/97-3871; B10/97-3881; B10/97-3891; B10/97-3892; B10/97-3911; B10/97-3912; B10/97-3921; B10/97-3922; B10/97-3923; B10/97-3931; B10/97-3932; B10/97-3941; B10/97-4011; B10/97-4012; B10/97-4031; B10/97-4032; B10/97-4041; B10/97-4042; B12/96; B12/96-7210; B12/96-7220; B12/96-7230; B12/96-7240; B12/96-8520; B12/96-8540; B12/96-8550; B12/98; B12/98-7811; B12/98-7812; B12/98-7813; B12/98-8391; B12/98-8392; B12/98-8393; B12/98-8394; B12/98-8621; B12/98-8622; B15/97; B15/97-6761; B15/97-6771; B15/97-6781; B15/97-6791; B15/97-6801; B15/97-6811; B15/97-6821; B15/97-6831; B15/97-6841; B15/97-6851; B15/97-6861; B15/97-6871; B15/97-6881; B15/97-6891; B15/97-6892; B15/97-6901; B15/97-6902; B15/97-6912; B15/97-6921; B15/97-6931; B15/97-6951; B15/97-6961; B15/97-6971; B15/97-6981; B15/97-6991; B15/97-7001; B15/97-7011; B15/97-7021; B15/97-7031; B15/97-7041; B15/97-7051; B15/97-7061; B15/97-7071; B15/97-7081; B15/97-7091; B15/97-7101; B15/97-7111; B15/97-7121; B15/97-7131; B15/97-7141; B15/97-7151; B15/97-7161; B15/97-7171; B15/97-7181; B15/97-7182; B15/97-7191; B15/97-7201; B15/97-7211; B15/97-7221; B15/97-7231; B15/97-7241; B15/97-7251; B15/97-7261; B15/97-7271; B15/97-7281; B15/97-7291; B15/97-7301; B15/97-7311; B15/97-7321; B15/97-7331; B15/97-7341; B15/97-7351; B15/97-7361; B15/97-7371; B15/97-7381; B15/97-7391; B15/97-7401; B15/97-7411; B15/97-7421; B15/97-7431; B15/97-7441; B15/97-7451; B15/97-7461; B15/97-7471; B15/97-7481; B15/97-7491; B15/97-7501; B15/97-7511; B15/97-7512; B15/97-7513; B15/97-7521; B15/97-7531; B15/97-7532; B15/97-7533; B15/97-7541; B15/97-7551; B15/97-7561; B15/97-7571; B15/97-7581; B15/97-7591; B15/97-7601; B15/97-7611; B15/97-7621; B15/97-7631; B15/97-7641; B15/97-7651; B15/97-7661; B15/97-7671; B15/97-7681; B15/97-7691; B15/97-7692; B15/97-7701; B15/97-7711; B15/97-7721; B15/97-7731; B15/97-7741; B15/97-7751; Bjarni Saemundsson; CARDEEP1/93; CARDEEP1/93-161; CARDEEP1/93-162; CARDEEP1/93-171; CARDEEP1/93-181; CARDEEP1/93-182; CARDEEP1/93-201; CARDEEP1/93-211; CARDEEP1/93-212; CARDEEP1/93-231; CARDEEP1/93-232; CARDEEP1/93-261; CARDEEP1/93-271; CARDEEP1/93-281; CARDEEP1/93-291; CARDEEP1/93-301; CARDEEP1/93-311; CARDEEP1/93-312; CARDEEP1/93-331; CARDEEP1/93-341; CARDEEP1/93-351; CARDEEP1/93-361;
    Type: Dataset
    Format: application/zip, 51 datasets
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    DATA PANGAEA
  • 8
    facet.materialart.
    Unknown
    Physical oceanography during ODEN cruise OD91 (2010)
    PANGAEA
    In:  Finnish Institute of Marine Research, Helsinki
    Details
    Publication Date: 2023-02-12
    Keywords: Arctic Ocean; Calculated; Conductivity; CTD, Neil Brown, Mark III B; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Elevation of event; Event label; Latitude of event; Longitude of event; OD91; OD91_005-1; OD91_008-1; OD91_009-1; OD91_010-1; OD91_011-1; OD91_012-1; OD91_013-1; OD91_014-1; OD91_015-1; OD91_016-1; OD91_017-1; OD91_018-1; OD91_019-1; OD91_020-1; OD91_021-1; OD91_022-1; OD91_023-1; OD91_024-1; OD91_025-1; OD91_026-1; OD91_027-1; OD91_028-1; OD91_029-1; OD91_030-1; OD91_031-1; OD91_032-1; OD91_033-1; OD91_034-1; OD91_035-1; OD91_036-1; OD91_037-1; OD91_038-1; OD91_039-1; OD91_040-1; OD91_041-1; OD91_043-1; OD91_044-1; OD91_045-1; OD91_046-1; OD91_047-1; OD91_048-1; OD91_049-1; OD91_050-1; OD91_051-1; OD91_052-1; OD91_054-1; OD91_055-1; OD91_056-1; OD91_058-1; OD91_059-1; OD91_060-1; OD91_061-1; Oden; Pressure, water; Salinity; Temperature, water; Temperature, water, potential
    Type: Dataset
    Format: text/tab-separated-values, 469884 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 9
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    Unknown
    Physical oceanography on board of POLARSTERN (1983-11-22 to 2016-02-14) (2016)
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven | Supplement to: Driemel, Amelie; Fahrbach, Eberhard; Rohardt, Gerd; Beszczynska-Möller, Agnieszka; Boetius, Antje; Budéus, Gereon; Cisewski, Boris; Engbrodt, Ralph; Gauger, Steffen; Geibert, Walter; Geprägs, Patrizia; Gerdes, Dieter; Gersonde, Rainer; Gordon, Arnold L; Grobe, Hannes; Hellmer, Hartmut H; Isla, Enrique; Jacobs, Stanley S; Janout, Markus A; Jokat, Wilfried; Klages, Michael; Kuhn, Gerhard; Meincke, Jens; Ober, Sven; Østerhus, Svein; Peterson, Ray G; Rabe, Benjamin; Rudels, Bert; Schauer, Ursula; Schumacher, Stefanie; Schröder, Michael; Sieger, Rainer; Sildam, Jüri; Soltwedel, Thomas; Stangeew, Elena; Stein, Manfred; Strass, Volker H; Thiede, Jörn; Tippenhauer, Sandra; Veth, Cornelis; von Appen, Wilken-Jon; Weirig, Marie-France; Wisotzki, Andreas; Wolf-Gladrow, Dieter A; Kanzow, Torsten (2017): From pole to pole: 33 years of physical oceanography onboard R/V Polarstern. Earth System Science Data, 9(1), 211-220, https://doi.org/10.5194/essd-9-211-2017
    Details
    Publication Date: 2023-10-18
    Description: Measuring temperature and salinity profiles in the world's oceans is crucial to understanding ocean dynamics and its influence on the heat budget, the water cycle, the marine environment and on our climate. Since 1983 the German research vessel and icebreaker Polarstern has been the platform of numerous CTD (conductivity, temperature, depth instrument) deployments in the Arctic and the Antarctic. We report on a unique data collection spanning 33 years of polar CTD data. In total 131 data sets (1 data set per cruise leg) containing data from 10 063 CTD casts are now freely available. During this long period five CTD types with different characteristics and accuracies have been used. Therefore the instruments and processing procedures (sensor calibration, data validation, etc.) are described in detail. This compilation is special not only with regard to the quantity but also the quality of the data - the latter indicated for each data set using defined quality codes. The complete data collection includes a number of repeated sections for which the quality code can be used to investigate and evaluate long-term changes. Beginning with 2010, the salinity measurements presented here are of the highest quality possible in this field owing to the introduction of the OPTIMARE Precision Salinometer.
    Keywords: Author(s); AWI_PhyOce; Campaign; Date/time end; Date/time start; Method comment; Number of observations; Ocean and sea region; Persistent Identifier; Physical Oceanography @ AWI; Principal investigator; Quality code; Uniform resource locator/link to image; Uniform resource locator/link to reference
    Type: Dataset
    Format: text/tab-separated-values, 1695 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 10
    facet.materialart.
    Unknown
    Physical oceanography during VALDIVIA cruise VA136 (1998)
    PANGAEA
    Details
    Publication Date: 2024-02-01
    Keywords: 10; 11; 12; 13; 14; 15; 16; 17; 18; 19; 2; 20; 21; 22; 23; 24; 25; 26; 27; 28; 29; 3; 30; 31; 32; 33; 34; 35; 36; 37; 38; 39; 4; 40; 41; 42; 43; 44; 45; 46; 47; 48; 49; 5; 50; 51; 52; 54; 55; 56; 57; 58; 59; 6; 60; 61; 62; 63; 64; 65; 66; 67; 68; 69; 7; 70; 71; 72; 73; 74; 75; 76; 8; 9; CTD; CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Elevation of event; ESOP; European subpolar ocean programme : sea ice-ocean interactions; Event label; JGOFS; Joint Global Ocean Flux Study; Latitude of event; Longitude of event; MULT; Multiple investigations; Pressure, water; Salinity; Temperature, water; UniHH_CTD; VA136; VA136_10; VA136_11; VA136_12; VA136_13; VA136_14; VA136_15; VA136_16; VA136_17; VA136_18; VA136_19; VA136_2; VA136_20; VA136_21; VA136_22; VA136_23; VA136_24; VA136_25; VA136_26; VA136_27; VA136_28; VA136_29; VA136_3; VA136_30; VA136_31; VA136_32; VA136_33; VA136_34; VA136_35; VA136_36; VA136_37; VA136_38; VA136_39; VA136_4; VA136_40; VA136_41; VA136_42; VA136_43; VA136_44; VA136_45; VA136_46; VA136_47; VA136_48; VA136_49; VA136_5; VA136_50; VA136_51; VA136_52; VA136_54; VA136_55; VA136_56; VA136_57; VA136_58; VA136_59; VA136_6; VA136_60; VA136_61; VA136_62; VA136_63; VA136_64; VA136_65; VA136_66; VA136_67; VA136_68; VA136_69; VA136_7; VA136_70; VA136_71; VA136_72; VA136_73; VA136_74; VA136_75; VA136_76; VA136_8; VA136_9; Valdivia (1961)
    Type: Dataset
    Format: text/tab-separated-values, 644959 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
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