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  • 1
    Keywords: Convection (Oceanography) Congresses ; Ocean circulation Computer simulation ; Congresses ; Convection (Oceanography) Congresses ; Ocean circulation Computer simulation ; Congresses ; Oceanography ; Konferenzschrift 1990 ; Tiefsee ; Konvektion ; Tiefsee ; Meeresströmung ; Meereskunde ; Thermohaline Zirkulation ; Meerwasser ; Zirkulation ; Tiefsee ; Konvektion ; Tiefsee ; Meeresströmung
    Type of Medium: Book
    Pages: XI, 382 S. , graph. Darst., Ill.
    ISBN: 0444887644
    Series Statement: Elsevier oceanography series 57
    DDC: 551.47
    Language: English
    Note: Literaturangaben
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  • 2
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Polar research 7 (1989), S. 0 
    ISSN: 1751-8369
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geography , Geosciences
    Notes: During the summer 1987 expedition of the polar research vessel‘Polarstern’in the Eurasian Basin of the Arctic Ocean, sea ice at about 84-86°N and 20-30°E was found to have high concentrations of particulate material. The particle-laden ice occurred in patches which often darkened more than half the ice surface at our northernmost positions. Much of this ice appeared to be within the Siberian Branch of the Transpolar Drift stream, which transports deformed, multi-year ice from the Siberian shelves westward across the Eurasian Basin. Lithogenic sediment, which is the major component of the particulate material, may have been incorporated during ice formation on the shallow Siberian seas. Diatoms collected from the particle-rich ice surfaces support this conclusion, as assemblages were dominated by a marine benthic species similar to that reported from sea ice off the coast of northeast Siberia. Based on drift trajectories of buoys deployed on the ice it appears that much of the particle-laden ice exited the Arctic Ocean through the Fram Strait and joined the East Greenland Current.Very different sea ice characteristics were found east of the Yermak Plateau and north of Svalbard and Frans Josef Land up to about 83-84°N. Here sea ice was thinner, less deformed, with lower amounts of lithogenic sediment and diatoms. The diatom assemblage was dominated by planktonic freshwater species. Trajectories of buoys deployed on sea ice in this region indicated a tendency for southward transport to the Yermak Plateau or into the Barents Sea.
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The Greenland Sea is one of a few sites in the world ocean where convection to great depths occurs—a process that forms some of the densest waters in the ocean. But the role of deep convective eddies, which result from surface cooling and mixing across density surfaces ...
    Type of Medium: Electronic Resource
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  • 4
    Publication Date: 2018-04-12
    Description: Analysis of modern and historical observations demonstrates that the temperature of the intermediate-depth (150–900 m) Atlantic water (AW) of the Arctic Ocean has increased in recent decades. The AW warming has been uneven in time; a local 1°C maximum was observed in the mid-1990s, followed by an intervening minimum and an additional warming that culminated in 2007 with temperatures higher than in the 1990s by 0.24°C. Relative to climatology from all data prior to 1999, the most extreme 2007 temperature anomalies of up to 1°C and higher were observed in the Eurasian and Makarov Basins. The AW warming was associated with a substantial (up to 75–90 m) shoaling of the upper AW boundary in the central Arctic Ocean and weakening of the Eurasian Basin upper-ocean stratification. Taken together, these observations suggest that the changes in the Eurasian Basin facilitated greater upward transfer of AW heat to the ocean surface layer. Available limited observations and results from a 1D ocean column model support this surmised upward spread of AW heat through the Eurasian Basin halocline. Experiments with a 3D coupled ice–ocean model in turn suggest a loss of 28–35 cm of ice thickness after 50 yr in response to the 0.5 W m−2 increase in AW ocean heat flux suggested by the 1D model. This amount of thinning is comparable to the 29 cm of ice thickness loss due to local atmospheric thermodynamic forcing estimated from observations of fast-ice thickness decline. The implication is that AW warming helped precondition the polar ice cap for the extreme ice loss observed in recent years.
    Type: Article , PeerReviewed
    Format: text
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  • 5
    Publication Date: 2019-09-23
    Description: The water mass structure of the Arctic Ocean is remarkable, for its intermediate (depth range ~150–900 m) layer is filled with warm (temperature 〉0°C) and salty water of Atlantic origin (usually called the Atlantic Water, AW). This water is carried into and through the Arctic Ocean by the pan-Arctic boundary current, which moves cyclonically along the basins’ margins (Fig. 1). This system provides the largest input of water, heat, and salt into the Arctic Ocean; the total quantity of heat is substantial, enough to melt the Arctic sea ice cover several times over. By utilizing an extensive archive of recently collected observational data, this study provides a cohesive picture of recent large-scale changes in the AW layer of the Arctic Ocean. These recent observations show the warm pulse of AW that entered the Arctic Ocean in the early 1990s finally reached the Canada Basin during the 2000s. The second warm pulse that entered the Arctic Ocean in the mid-2000s has moved through the Eurasian Basin and is en route downstream. One of the most intriguing results of these observations is the realization of the possibility of uptake of anomalous AW heat by overlying layers, with possible implications for an already-reduced Arctic ice cover.
    Type: Article , PeerReviewed
    Format: text
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  • 6
    Publication Date: 2017-02-10
    Description: The Arctic Ocean is the missing piece for any global model. Records of processes at both long and short timescales will be necessary to predict the future evolution of the Arctic Ocean through what appears to be a period of rapid climate change. Ocean monitoring is impoverished without the long-timescale records available from paleoceanography and the boundary conditions that can be obtained from marine geology and geophysics. The past and the present are the key to our ability to predict the future.
    Type: Article , NonPeerReviewed
    Format: text
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  • 7
    Publication Date: 2019-09-23
    Description: During the summer 1987 expedition of the polar research vessel‘Polarstern’in the Eurasian Basin of the Arctic Ocean, sea ice at about 84-86°N and 20-30°E was found to have high concentrations of particulate material. The particle-laden ice occurred in patches which often darkened more than half the ice surface at our northernmost positions. Much of this ice appeared to be within the Siberian Branch of the Transpolar Drift stream, which transports deformed, multi-year ice from the Siberian shelves westward across the Eurasian Basin. Lithogenic sediment, which is the major component of the particulate material, may have been incorporated during ice formation on the shallow Siberian seas. Diatoms collected from the particle-rich ice surfaces support this conclusion, as assemblages were dominated by a marine benthic species similar to that reported from sea ice off the coast of northeast Siberia. Based on drift trajectories of buoys deployed on the ice it appears that much of the particle-laden ice exited the Arctic Ocean through the Fram Strait and joined the East Greenland Current. Very different sea ice characteristics were found east of the Yermak Plateau and north of Svalbard and Frans Josef Land up to about 83-84°N. Here sea ice was thinner, less deformed, with lower amounts of lithogenic sediment and diatoms. The diatom assemblage was dominated by planktonic freshwater species. Trajectories of buoys deployed on sea ice in this region indicated a tendency for southward transport to the Yermak Plateau or into the Barents Sea.
    Type: Article , PeerReviewed
    Format: text
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  • 8
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    PANGAEA
    In:  Institut français de recherche pour l'exploitation de la mer - Siège social
    Publication Date: 2023-12-15
    Keywords: CONVHIV2; CTD, Sea-Bird; CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Event label; FI3519920060100010; FI3519920060100020; FI3519920060100030; FI3519920060100040; FI3519920060100050; FI3519920060100060; FI3519920060100070; FI3519920060100080; FI3519920060100090; FI3519920060100100; FI3519920060100110; FI3519920060100120; FI3519920060100130; FI3519920060100140; FI3519920060100150; FI3519920060100160; FI3519920060100170; FI3519920060100180; FI3519920060100190; FI3519920060100200; FI3519920060100210; FI3519920060100220; FI3519920060100230; FI3519920060100240; FI3519920060100250; FI3519920060100260; FI3519920060100270; FI3519920060100280; FI3519920060100290; FI3519920060100300; FI3519920060100310; FI3519920060100320; FI3519920060100330; FI3519920060100340; FI3519920060100350; FI3519920060100360; FI3519920060100370; FI3519920060100380; FI3519920060100390; FI3519920060100400; FI3519920060100410; Latitude of event; Le Suroît; Longitude of event; MEDAR/MEDATLAS; Mediterranean Data Archaeology and Rescue; Mediterranean Sea, Western Basin; Pressure, water; Salinity; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 218076 data points
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  • 9
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    Unknown
    PANGAEA
    In:  Institut français de recherche pour l'exploitation de la mer - Siège social
    Publication Date: 2023-12-15
    Keywords: CTD; CTD, pre-1978 standard (Fofonoff & Millard, 1983, UNESCO Tech Pap Marine Sci 44); CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Event label; FI3519740002100010; FI3519740002100021; FI3519740002100030; FI3519740002100040; FI3519740002100051; FI3519740002100060; FI3519740002100070; FI3519740002100090; FI3519740002100100; FI3519740002100121; FI3519740002100130; FI3519740002100140; FI3519740002100150; FI3519740002100160; FI3519740002100170; FI3519740002100180; FI3519740002100190; FI3519740002100200; FI3519740002100210; FI3519740002100220; FI3519740002100230; FI3519740002100240; FI3519740002100250; FI3519740002100261; FI3519740002100270; FI3519740002100280; FI3519740002100291; FI3519740002100300; FI3519740002100311; FI3519740002100331; FI3519740002100340; FI3519740002100350; FI3519740002100360; FI3519740002100370; FI3519740002100380; FI3519740002100390; FI3519740002100400; FI3519740002100410; FI3519740002100420; FI3519740002100430; FI3519740002100440; FI3519740002100450; FI3519740002100460; FI3519740002100470; FI3519740002100480; FI3519740002100490; FI3519740002100501; Latitude of event; Le Noroit; Longitude of event; MEDAR/MEDATLAS; Mediterranean Data Archaeology and Rescue; Mediterranean Sea, Western Basin; MEDOC_1974; Pressure, water; Salinity; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 298344 data points
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  • 10
    Publication Date: 2022-05-25
    Description: Author Posting. © American Meteorological Society, 2010. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Journal of Physical Oceanography 40 (2010): 2743–2756, doi:10.1175/2010JPO4339.1.
    Description: Analysis of modern and historical observations demonstrates that the temperature of the intermediate-depth (150–900 m) Atlantic water (AW) of the Arctic Ocean has increased in recent decades. The AW warming has been uneven in time; a local 1°C maximum was observed in the mid-1990s, followed by an intervening minimum and an additional warming that culminated in 2007 with temperatures higher than in the 1990s by 0.24°C. Relative to climatology from all data prior to 1999, the most extreme 2007 temperature anomalies of up to 1°C and higher were observed in the Eurasian and Makarov Basins. The AW warming was associated with a substantial (up to 75–90 m) shoaling of the upper AW boundary in the central Arctic Ocean and weakening of the Eurasian Basin upper-ocean stratification. Taken together, these observations suggest that the changes in the Eurasian Basin facilitated greater upward transfer of AW heat to the ocean surface layer. Available limited observations and results from a 1D ocean column model support this surmised upward spread of AW heat through the Eurasian Basin halocline. Experiments with a 3D coupled ice–ocean model in turn suggest a loss of 28–35 cm of ice thickness after 50 yr in response to the 0.5 W m−2 increase in AW ocean heat flux suggested by the 1D model. This amount of thinning is comparable to the 29 cm of ice thickness loss due to local atmospheric thermodynamic forcing estimated from observations of fast-ice thickness decline. The implication is that AW warming helped precondition the polar ice cap for the extreme ice loss observed in recent years.
    Description: This study was supported by JAMSTEC (IP and VI), NOAA (IP, VI, and ID), NSF (IP,VA,VI, ID, JT, andMS),NASA(IP andVI), BMBF (ID), and UK NERC (SB) grants.
    Keywords: Arctic ; Forcing ; Temperature ; Sea ice ; Heating ; Coupled models
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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