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  • 2000-2004  (27)
  • 2001  (23)
  • 2000  (4)
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  • 2000-2004  (27)
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  • 1
    Keywords: Datensammlung
    Description / Table of Contents: 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.
    Type of Medium: Online Resource
    Pages: 2 Datasets , Format: application/zip
    Language: English
    Note: This dataset is supplement to doi:10.1029/2000JC000281
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  • 2
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 412 (2001), S. 605-606 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [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 ...
    Type of Medium: Electronic Resource
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  • 3
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    Unknown
    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
    Publication Date: 2023-12-12
    Description: 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.
    Keywords: 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
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 4
    Publication Date: 2023-12-12
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 14064 data points
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  • 5
    Publication Date: 2023-12-12
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 750603 data points
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  • 6
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    Unknown
    In:  The Climate Report, 3 (4). pp. 2-8.
    Publication Date: 2016-05-25
    Type: Article , NonPeerReviewed
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  • 7
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    Unknown
    AMS (American Meteorological Society)
    In:  Journal of Physical Oceanography, 31 (2). pp. 616-636.
    Publication Date: 2018-04-06
    Description: Transient eddies in the atmosphere induce a poleward transport of heat and moisture. A moist static energy budget of the surface layer is determined from the NCEP reanalysis data to evaluate the impact of the storm track. It is found that the transient eddies induce a cooling and drying of the surface layer with a monthly mean maximum of 60 W m−2. The cooling in the midlatitudes extends zonally over the entire basin. The impact of this cooling and drying on surface heat fluxes, sea surface temperature (SST), water mass transformation, and vertical structure of the Pacific is investigated using an ocean model coupled to an atmospheric mixed layer model. The cooling by atmospheric storms is represented by adding an eddy-induced transfer velocity to the mean velocity in an atmospheric mixed layer model. This is based on a parameterization of tracer transport by eddies in the ocean. When the atmospheric mixed layer model is coupled to an ocean model, realistic SSTs are simulated. The SST is up to 3 K lower due to the cooling by storms. The additional cooling leads to enhanced transformation rates of water masses in the midlatitudes. The enhanced shallow overturning cells affect even tropical regions. Together with realistic SST and deep winter mixed layer depths, this leads to formation of homogeneous water masses in the upper North Pacific, in accordance to observations.
    Type: Article , PeerReviewed
    Format: text
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  • 8
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    Unknown
    AMS (American Meteorological Society)
    In:  Journal of Physical Oceanography, 31 . pp. 1287-1303.
    Publication Date: 2018-04-06
    Description: A general circulation ocean model has been used to study the formation and propagation mechanisms of North Atlantic Oscillation (NAO)-generated temperature anomalies along the pathway of the North Atlantic Current (NAC). The NAO-like wind forcing generates temperature anomalies in the upper 440 m that propagate along the pathway of the NAC in general agreement with the observations. The analysis of individual components of the ocean heat budget reveals that the anomalies are primarily generated by the wind stress anomaly-induced oceanic heat transport divergence. After their generation they are advected with the mean current. Surface heat flux anomalies account for only one-third of the total temperature changes. Along the pathway of the NAC temperature anomalies of opposite signs are formed in the first and second halves of the pathway, a pattern called here the North Atlantic dipole (NAD). The response of the ocean depends fundamentally on Rt = (L/υ)/τ, the ratio between the time it takes for anomalies to propagate along the NAC [(L/υ) 10 years] compared to the forcing period τ. The authors find that for NAO periods shorter than 4 years (Rt 〉 1) the response in the subpolar region is mainly determined by the local forcing. For NAO periods longer than 32 years (Rt 〈 1); however, the SST anomalies in the northeastern part of the NAD become controlled by ocean advection. In the subpolar region maximal amplitudes of the temperature response are found for intermediate (decadal) periods (Rt 1) where the propagation of temperature anomalies constructively interferes with the local forcing. A comparison of the NAO-generated propagating temperature anomalies with those found in observations will be discussed.
    Type: Article , PeerReviewed
    Format: text
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  • 9
    Publication Date: 2015-11-09
    Type: Article , NonPeerReviewed
    Format: text
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  • 10
    Publication Date: 2015-11-09
    Type: Article , NonPeerReviewed
    Format: text
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