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  • 2020-2022  (3)
  • 1995-1999  (29)
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Language
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Year
  • 1
    Series available for loan
    Series available for loan
    Bremerhaven : Alfred-Wegener-Inst. für Polar- und Meeresforschung
    Associated volumes
    Call number: ZSP-168-199
    In: Berichte zur Polarforschung
    Type of Medium: Series available for loan
    Pages: 340 S. : überw. graph. Darst., Kt.
    ISSN: 0176-5027
    Series Statement: Berichte zur Polarforschung 199
    Language: English
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 2
    Publication Date: 1995-01-01
    Print ISSN: 0148-0227
    Electronic ISSN: 2156-2202
    Topics: Geosciences
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  • 3
    Publication Date: 1998-08-15
    Print ISSN: 0148-0227
    Electronic ISSN: 2156-2202
    Topics: Geosciences
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  • 4
    Publication Date: 1995-01-01
    Print ISSN: 0148-0227
    Electronic ISSN: 2156-2202
    Topics: Geosciences
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  • 5
    Publication Date: 1995-01-01
    Print ISSN: 0148-0227
    Electronic ISSN: 2156-2202
    Topics: Geosciences
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  • 6
    Publication Date: 1997-01-01
    Print ISSN: 0924-7963
    Electronic ISSN: 1879-1573
    Topics: Biology , Energy, Environment Protection, Nuclear Power Engineering , Geosciences , Physics
    Published by Elsevier
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  • 7
    Publication Date: 2024-02-01
    Keywords: AWI_PhyOce; Calculated from conductivity; CTD, Sea-Bird, SBE 911plus [SN: 0485]; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); 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; North Greenland Sea; Norwegian Sea; Number of observations; Petr Kottsov; Physical Oceanography @ AWI; PK-ARK-XII; PK-XII/01-1; PK-XII/01-2; PK-XII/02; PK-XII/03; PK-XII/04; PK-XII/05; PK-XII/06; PK-XII/07; PK-XII/08-1; PK-XII/08-2; PK-XII/09; PK-XII/10; PK-XII/11; PK-XII/12; PK-XII/13; PK-XII/14; PK-XII/15; PK-XII/16; PK-XII/17; PK-XII/18; PK-XII/19; PK-XII/20; PK-XII/21; PK-XII/22; PK-XII/23; PK-XII/24; PK-XII/25; PK-XII/26; PK-XII/27; PK-XII/28; PK-XII/29; PK-XII/33; PK-XII/34; PK-XII/35; PK-XII/36; PK-XII/37; PK-XII/38; PK-XII/39; PK-XII/40; PK-XII/41; PK-XII/42; PK-XII/43; PK-XII/44; PK-XII/45; PK-XII/46; PK-XII/47; PK-XII/48; PK-XII/49; PK-XII/50; PK-XII/51; PK-XII/52; Pressure, water; Salinity; Temperature, water; Temperature, water, potential
    Type: Dataset
    Format: text/tab-separated-values, 922560 data points
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  • 8
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Budéus, Gereon; Schneider, Wolfgang; Krause, Gunther (1998): Winter convective events and bottom water warming in the Greenland Sea. Journal of Geophysical Research: Oceans, 103(C9), 18513-18527, https://doi.org/10.1029/98JC01563
    Publication Date: 2024-06-25
    Description: From observations on yearly cruises to the central Greenland Sea between 1993 and 1996, conclusions are drawn with respect to winter convection and bottom water renewal. The data indicate that winter convection was extremely weak after 1993, not even ventilating the intermediate waters. This is remarkable, since the salinities in the upper layers increased considerably between 1993 and 1995, thus providing presumably favorable conditions for winter convection. With the absence of deep reaching winter convective events, the temperatures in the deeper waters of the Greenland Gyre increased steadily by about 0.03 K between 1993 and 1996. We conclude from the development of mainly the thermal structure on a zonal transect that an explanation for the temperature increase can be given by a large-scale downward water movement of about 150 m/yr in the central Greenland Sea. The data indicate that this process is independent of changes in the dynamically induced density distribution. It is therefore possible that a downward movement, perhaps masked by other processes, may continue for many years. If this is the case, resulting flushing times would be of the order of 20-30 years only. The presence of a large-scale circulation cell with downward movement in the central Greenland Gyre would explain the observed warming of the bottom waters without the demand for an actually active heat source. It is also in accordance with the observed increase of chemical tracer concentrations in the deep waters.
    Keywords: ARK-IX/1b; ARK-X/1; ARK-XI/2; AWI_PhyOce; CTD/Rosette; CTD-RO; ESOP; European subpolar ocean programme : sea ice-ocean interactions; JGOFS; Joint Global Ocean Flux Study; MULT; Multiple investigations; North Greenland Sea; Norwegian Sea; Petr Kottsov; Physical Oceanography @ AWI; PK-ARK-XII; PK-XII/01-1; PK-XII/01-2; PK-XII/02; PK-XII/03; PK-XII/04; PK-XII/05; PK-XII/06; PK-XII/07; PK-XII/08-1; PK-XII/08-2; PK-XII/09; PK-XII/10; PK-XII/11; PK-XII/12; PK-XII/13; PK-XII/14; PK-XII/15; PK-XII/16; PK-XII/17; PK-XII/18; PK-XII/19; PK-XII/20; PK-XII/21; PK-XII/22; PK-XII/23; PK-XII/24; PK-XII/25; PK-XII/26; PK-XII/27; PK-XII/28; PK-XII/29; PK-XII/33; PK-XII/34; PK-XII/35; PK-XII/36; PK-XII/37; PK-XII/38; PK-XII/39; PK-XII/40; PK-XII/41; PK-XII/42; PK-XII/43; PK-XII/44; PK-XII/45; PK-XII/46; PK-XII/47; PK-XII/48; PK-XII/49; PK-XII/50; PK-XII/51; PK-XII/52; Polarstern; PS24; PS24/036; PS24/037; PS24/038; PS24/039; PS24/040; PS24/041; PS24/043; PS24/044; PS24/045; PS24/046; PS24/047; PS24/048; PS24/049; PS24/050; PS24/051; PS24/053; PS24/054; PS24/055; PS24/056; PS24/057; PS24/061; PS24/062; PS24/063; PS24/064; PS24/065; PS24/066; PS24/067; PS24/068; PS24/069; PS24/070; PS31; PS31/026; PS31/026a; PS31/027; PS31/028; PS31/029; PS31/030; PS31/031; PS31/032; PS31/033; PS31/034; PS31/035; PS31/036; PS31/037; PS31/038; PS31/039; PS31/040; PS31/041; PS31/042; PS31/043; PS31/044; PS31/045; PS31/046; PS31/048; PS31/049; PS31/050; PS31/051; PS31/052; PS31/053; PS31/054; PS31/055; PS31/056; PS31/057; PS31/058; PS31/059; PS31/060; PS31/061; PS31/062; PS31/063; PS31/064; PS31/065; PS31/066; PS31/067; PS31/068; PS31/069; PS31/070; PS31/071; PS31/072; PS31/073; PS31/074; PS31/075; PS31/076; PS31/077; PS31/078; PS31/079; PS31/080; PS31/081; PS31/082; PS31/083; PS31/084; PS31/085; PS31/087; PS31/089; PS31/090; PS31/091; PS31/092; PS31/093; PS31/094; PS31/095; PS31/096; PS31/096a; PS31/097; PS31/098; PS31/099; PS31/100; PS31/101; PS31/102; PS31/103; PS31/104; PS31/105; PS31/106; PS31/107; PS31/108; PS31/109; PS31/110; PS31/111; PS37; PS37/001-1; PS37/006-1; PS37/006-2; PS37/008-2; PS37/008-4; PS37/010; PS37/014-3; PS37/014-4; PS37/015; PS37/016-4; PS37/016-5; PS37/017; PS37/018; PS37/019; PS37/020-6; PS37/020-7; PS37/021-3; PS37/021-4; PS37/022-3; PS37/022-4; PS37/023; PS37/024; PS37/025-1; PS37/025-2; PS37/026-1; PS37/026-2; PS37/028; PS37/029; PS37/033; PS37/035; PS37/036; PS37/037; PS37/038; PS37/039; PS37/040; PS37/041; PS37/042; PS37/043; PS37/044; PS37/045; PS37/046; PS37/047; PS37/048; PS37/049; PS37/050; PS37/052; PS37/053; PS37/056; PS37/057; PS37/058; PS37/059; PS37/060; PS37/061; PS37/062; PS37/063; PS37/064; PS37/065; PS37/066; PS37/067; PS37/068; PS37/069; PS37/070; PS37/071; PS37/072; PS37/073; PS37/074; PS37/075; PS37/076; PS37/077; PS37/078; PS37/079; PS37/080; PS37/081; PS37/082; PS37/083; PS37/084; PS37/085; PS37/086; PS37/087; PS37/088; PS37/089; PS37/090; PS37/091; PS37/092; PS37/093; PS37/094; PS37/095; PS37/096; PS37/097; PS37/098; PS37/099; PS37/100; PS37/101; PS37/102; PS37/103; PS37/104; PS37/105; PS37/106; PS37/107; PS37/108; PS37/109; PS37/110; PS37/111; PS37/112; PS37/113; PS37/114; PS37/115; PS37/116; PS37/117
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 9
    Publication Date: 2024-06-25
    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
    Location Call Number Expected Availability
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  • 10
    Publication Date: 2024-06-25
    Keywords: ARK-IX/1b; AWI_PhyOce; Calculated from conductivity; Computed; CTD, Neil Brown, Mark III B, SN 1069; 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; North Greenland Sea; Norwegian Sea; Physical Oceanography @ AWI; Polarstern; Pressure, water; PS24; PS24/036; PS24/037; PS24/038; PS24/039; PS24/040; PS24/041; PS24/043; PS24/044; PS24/045; PS24/046; PS24/047; PS24/048; PS24/049; PS24/050; PS24/051; PS24/053; PS24/054; PS24/055; PS24/056; PS24/057; PS24/061; PS24/062; PS24/063; PS24/064; PS24/065; PS24/066; PS24/067; PS24/068; PS24/069; PS24/070; Salinity; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 52791 data points
    Location Call Number Expected Availability
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