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  • 2000-2004  (50)
  • 1985-1989  (3)
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  • 1
    Schlagwort(e): Hochschulschrift
    Materialart: Online-Ressource
    Seiten: 1 Online-Ressource (73 Blatt = 3 MB) , Diagramme
    Sprache: Deutsch
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    Materialart: Buch
    Seiten: 66 Bl., graph. Darst
    Sprache: Unbestimmte Sprache
    Anmerkung: Kiel, Univ., Dipl., 1989
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    Schlagwort(e): Datensammlung
    Beschreibung / Inhaltsverzeichnis: An extensive set of conductivity-temperature-depth (CTD)/lowered acoustic Doppler current profiler (LADCP) data obtained within the northwestern Weddell Sea in August 1997 characterizes the dense water outflow from the Weddell Sea and overflow into the Scotia Sea. Along the outer rim of the Weddell Gyre, there is a stream of relatively low salinity, high oxygen Weddell Sea Deep Water (defined as water between 0? and ?0.7?C), constituting a more ventilated form of this water mass than that found farther within the gyre. Its enhanced ventilation is due to injection of relatively low salinity shelf water found near the northern extreme of Antarctic Peninsula's Weddell Sea shelf, shelf water too buoyant to descend to the deep-sea floor. The more ventilated form of Weddell Sea Deep Water flows northward along the eastern side of the South Orkney Plateau, passing into the Scotia Sea rather than continuing along an eastward path in the northern Weddell Sea. Weddell Sea Bottom Water also exhibits two forms: a low-salinity, better oxygenated component confined to the outer rim of the Weddell Gyre, and a more saline, less oxygenated component observed farther into the gyre. The more saline Weddell Sea Bottom Water is derived from the southwestern Weddell Sea, where high-salinity shelf water is abundant. The less saline Weddell Sea Bottom Water, like the more ventilated Weddell Sea Deep Water, is derived from lower-salinity shelf water at a point farther north along the Antarctic Peninsula. Transports of Weddell Sea Deep and Bottom Water masses crossing 44?W estimated from one LADCP survey are 25 ? 10**6 and 5 ? 10**6 m**3/s, respectively. The low-salinity, better ventilated forms of Weddell Sea Deep and Bottom Water flowing along the outer rim of the Weddell Gyre have the position and depth range that would lead to overflow of the topographic confines of the Weddell Basin, whereas the more saline forms may be forced to recirculate within the Weddell Gyre.
    Materialart: Online-Ressource
    Seiten: 2 Datasets , Format: application/zip
    Sprache: Englisch
    Anmerkung: This dataset is supplement to doi:10.1029/2000JC000281
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 4
    Digitale Medien
    Digitale Medien
    Oxford, UK : Blackwell Publishing Ltd
    Polar research 22 (2003), S. 0 
    ISSN: 1751-8369
    Quelle: Blackwell Publishing Journal Backfiles 1879-2005
    Thema: Geographie , Geologie und Paläontologie
    Notizen: Historical winter sea ice concentration data are used to examine the relation between the Northern Annular Mode (NAM) and the sea ice concentration in the Nordic seas over the past 50 years. The well known basic response pattern of a seesaw between the Labrador Sea and the Greenland, Iceland and Barents seas is being reproduced. However, the response is not robust in the Greenland and Iceland seas. There the observed variability has a more complex relationship with surface temperatures and winds. We divide the sea ice response into three spectral bands: high (P〈 year), band (5〈P〈15 year), and low pass (P〉15 year) filtered NAM indices. This division is motivated by the expected slow response of the ocean circulation which might play a significant role in the Greenland and Iceland seas. The response to the NAM is also examined separately for the periods before and after 1976 to identify variations due to the relocation of the northern centre of the North Atlantic Oscillation.
    Materialart: Digitale Medien
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 5
    Digitale Medien
    Digitale Medien
    [s.l.] : Nature Publishing Group
    Nature 412 (2001), S. 605-606 
    ISSN: 1476-4687
    Quelle: Nature Archives 1869 - 2009
    Thema: Biologie , Chemie und Pharmazie , Medizin , Allgemeine Naturwissenschaft , Physik
    Notizen: [Auszug] One way of accounting for lowered atmospheric carbon dioxide concentrations during Pleistocene glacial periods is by invoking the Antarctic stratification hypothesis, which links the reduction in CO2 to greater stratification of ocean surface waters around Antarctica. As discussed ...
    Materialart: Digitale Medien
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 6
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Gordon, Arnold L; Visbeck, Martin; Huber, Bruce (2001): Export of Weddell Sea deep and bottom water. Journal of Geophysical Research: Oceans, 106(C5), 9005-9017, https://doi.org/10.1029/2000JC000281
    Publikationsdatum: 2023-12-12
    Beschreibung: An extensive set of conductivity-temperature-depth (CTD)/lowered acoustic Doppler current profiler (LADCP) data obtained within the northwestern Weddell Sea in August 1997 characterizes the dense water outflow from the Weddell Sea and overflow into the Scotia Sea. Along the outer rim of the Weddell Gyre, there is a stream of relatively low salinity, high oxygen Weddell Sea Deep Water (defined as water between 0° and ?0.7°C), constituting a more ventilated form of this water mass than that found farther within the gyre. Its enhanced ventilation is due to injection of relatively low salinity shelf water found near the northern extreme of Antarctic Peninsula's Weddell Sea shelf, shelf water too buoyant to descend to the deep-sea floor. The more ventilated form of Weddell Sea Deep Water flows northward along the eastern side of the South Orkney Plateau, passing into the Scotia Sea rather than continuing along an eastward path in the northern Weddell Sea. Weddell Sea Bottom Water also exhibits two forms: a low-salinity, better oxygenated component confined to the outer rim of the Weddell Gyre, and a more saline, less oxygenated component observed farther into the gyre. The more saline Weddell Sea Bottom Water is derived from the southwestern Weddell Sea, where high-salinity shelf water is abundant. The less saline Weddell Sea Bottom Water, like the more ventilated Weddell Sea Deep Water, is derived from lower-salinity shelf water at a point farther north along the Antarctic Peninsula. Transports of Weddell Sea Deep and Bottom Water masses crossing 44°W estimated from one LADCP survey are 25 ? 10**6 and 5 ? 10**6 m**3/s, respectively. The low-salinity, better ventilated forms of Weddell Sea Deep and Bottom Water flowing along the outer rim of the Weddell Gyre have the position and depth range that would lead to overflow of the topographic confines of the Weddell Basin, whereas the more saline forms may be forced to recirculate within the Weddell Gyre.
    Schlagwort(e): Acoustic Doppler Current Profiler; ADCP; CTD/Rosette; CTD-RO; Nathaniel B. Palmer; NBP9705; NBP9705_00377; NBP9705/01; NBP9705/02; NBP9705/03; NBP9705/04; NBP9705/05; NBP9705/06; NBP9705/07; NBP9705/08; NBP9705/09; NBP9705/10; NBP9705/11; NBP9705/12; NBP9705/13; NBP9705/14; NBP9705/15; NBP9705/16; NBP9705/17; NBP9705/18; NBP9705/19; NBP9705/20; NBP9705/21; NBP9705/22; NBP9705/23; NBP9705/24; NBP9705/25; NBP9705/26; NBP9705/27; NBP9705/28; NBP9705/29; NBP9705/30; NBP9705/31; NBP9705/32; NBP9705/33; NBP9705/34; NBP9705/35; NBP9705/36; NBP9705/37; NBP9705/38; NBP9705/39; NBP9705/40; NBP9705/41; NBP9705/42; NBP9705/43; NBP9705/44; NBP9705/45; NBP9705/46; NBP9705/47; NBP9705/48; NBP9705/49; NBP9705/50; NBP9705/51; NBP9705/52; NBP9705/53; NBP9705/54; NBP9705/55; NBP9705/56; NBP9705/57; NBP9705/58; NBP9705/59; NBP9705/60; NBP9705/61; NBP9705/62; NBP9705/63; NBP9705/64; NBP9705/65; NBP9705/66; NBP9705/67; NBP9705/68; NBP9705/69; NBP9705/70; NBP9705/71; NBP9705/72; NBP9705/73; NBP9705/74; NBP9705/75; NBP9705/76; NBP9705/77; NBP9705/78; NBP9705/79; NBP9705/80; NBP9705/81; NBP9705/82; NBP9705/83; NBP9705/84; NBP9705/85; NBP9705/86; NBP9705/87; NBP9705/88; NBP9705/89; NBP9705/90; NBP9705/91; NBP9705/92; NBP9705/93; NBP9705/94; NBP9705/95; NBP9705/96; NBP9705/97; Scotia Sea, southwest Atlantic; Weddell Sea
    Materialart: Dataset
    Format: application/zip, 2 datasets
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 7
    Publikationsdatum: 2023-12-12
    Schlagwort(e): Acoustic Doppler Current Profiler; ADCP; Current velocity, east-west; Current velocity, north-south; DATE/TIME; DEPTH, water; LATITUDE; LONGITUDE; Nathaniel B. Palmer; NBP9705; NBP9705_00377; Shipboard Acoustic Doppler Current Profiling (SADCP); Ship velocity, absolute east-west, standard deviation; Ship velocity, absolute east-west components means; Ship velocity, absolute north-south components mean; Ship velocity, absolute north-south standard deviation; Temperature, technical; Temperature, technical, standard deviation; WOCE; World Ocean Circulation Experiment
    Materialart: Dataset
    Format: text/tab-separated-values, 14064 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 8
    Publikationsdatum: 2023-12-12
    Schlagwort(e): Calculated; CTD, SEA-BIRD SBE 9 plus; CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Elevation of event; Event label; Latitude of event; Longitude of event; Nathaniel B. Palmer; NBP9705; NBP9705/01; NBP9705/02; NBP9705/03; NBP9705/04; NBP9705/05; NBP9705/06; NBP9705/07; NBP9705/08; NBP9705/09; NBP9705/10; NBP9705/11; NBP9705/12; NBP9705/13; NBP9705/14; NBP9705/15; NBP9705/16; NBP9705/17; NBP9705/18; NBP9705/19; NBP9705/20; NBP9705/21; NBP9705/22; NBP9705/23; NBP9705/24; NBP9705/25; NBP9705/26; NBP9705/27; NBP9705/28; NBP9705/29; NBP9705/30; NBP9705/31; NBP9705/32; NBP9705/33; NBP9705/34; NBP9705/35; NBP9705/36; NBP9705/37; NBP9705/38; NBP9705/39; NBP9705/40; NBP9705/41; NBP9705/42; NBP9705/43; NBP9705/44; NBP9705/45; NBP9705/46; NBP9705/47; NBP9705/48; NBP9705/49; NBP9705/50; NBP9705/51; NBP9705/52; NBP9705/53; NBP9705/54; NBP9705/55; NBP9705/56; NBP9705/57; NBP9705/58; NBP9705/59; NBP9705/60; NBP9705/61; NBP9705/62; NBP9705/63; NBP9705/64; NBP9705/65; NBP9705/66; NBP9705/67; NBP9705/68; NBP9705/69; NBP9705/70; NBP9705/71; NBP9705/72; NBP9705/73; NBP9705/74; NBP9705/75; NBP9705/76; NBP9705/77; NBP9705/78; NBP9705/79; NBP9705/80; NBP9705/81; NBP9705/82; NBP9705/83; NBP9705/84; NBP9705/85; NBP9705/86; NBP9705/87; NBP9705/88; NBP9705/89; NBP9705/90; NBP9705/91; NBP9705/92; NBP9705/93; NBP9705/94; NBP9705/95; NBP9705/96; NBP9705/97; Salinity; Scotia Sea, southwest Atlantic; Temperature, water; Temperature, water, potential; Weddell Sea
    Materialart: Dataset
    Format: text/tab-separated-values, 750603 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 9
    facet.materialart.
    Unbekannt
    In:  (Diploma thesis), Christian-Albrechts-Universität Kiel, Kiel, Germany, 65 pp
    Publikationsdatum: 2020-12-14
    Materialart: Thesis , NonPeerReviewed
    Format: text
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 10
    facet.materialart.
    Unbekannt
    In:  CLIVAR Exchanges, 25 (7 (3/4)). pp. 4-5.
    Publikationsdatum: 2015-11-09
    Materialart: Article , NonPeerReviewed
    Format: text
    Standort Signatur Einschränkungen Verfügbarkeit
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