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  • 2020-2024  (25)
  • 1980-1984  (3)
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  • 1
    Publikationsdatum: 2023-11-13
    Beschreibung: We assessed the spatial and temporal variability of the Arctic Boundary Current (ABC) using seven oceanographic moorings, deployed across the continental slope north of Severnaya Zemlya in 2015–2018. Transports and individual water masses were quantified based on temperature and salinity recorders and current profilers. Our results were compared with observations from the northeast Svalbard and the central Laptev Sea continental slopes to evaluate the hydrographic transformation along the ABC pathway. The highest velocities (〉0.30 m s〈sup〉−1〈/sup〉) of the ABC occurred at the upper continental slope and decreased offshore to below 0.03 m s〈sup〉−1〈/sup〉 in the deep basin. The ABC showed seasonal variability with velocities two times higher in winter than in summer. Compared to upstream conditions in Svalbard, water mass distribution changed significantly within 20 km of the shelf edge due to mixing with‐ and intrusion of shelf waters. The ABC transported 4.15 ± 0.3 Sv in the depth range 50–1,000 m, where 0.88 ± 0.1, 1.5 ± 0.2, 0.61 ± 0.1 and 1.0 ± 0.15 Sv corresponded to Atlantic Water (AW), Dense Atlantic Water (DAW), Barents Sea Branch Water (BSBW) and Transformed Atlantic Water (TAW). 62–70% of transport was constrained to within 30–40 km of the shelf edge, and beyond 84 km, transport increases were estimated to be 0.54 Sv. Seasonality of TAW derived from local shelf‐processes and advection of seasonal‐variable Fram Strait waters, while BSBW transport variability was dominated by temperature changes with maximum transport coinciding with minimum temperatures. Further Barents Sea warming will likely reduce TAW and BSBW transport leading to warmer conditions along the ABC pathway.
    Beschreibung: Plain Language Summary: We assessed the structure and seasonal variability of the flow and water masses of the Arctic Boundary Current (ABC) in the region north of Severnaya Zemlya. This current is important in the Arctic Ocean as it transports relatively warm and saline waters along the Eurasian Arctic continental slope. We quantified the flow, transport and hydrographic variability of the ABC. Compared to observations from upstream, our results indicate that the water masses away from the shelf break maintained the hydrographic characteristics from upstream. In contrast, the water masses near the shelf break were significantly cooled and freshened due to intrusion of‐ and mixing with shelf waters. The water masses near the shelf break showed a seasonal signal in volume transport and temperature which derives from local shelf processes, advection of seasonal‐variable waters along the ABC pathway and the seasonal cooling of the Barents Sea. If the warming trend in the Barents Sea continues, warmer waters are expected to be advected eastward along the Eurasian continental slope by the ABC.
    Beschreibung: Key Points: We quantify the Arctic Boundary Current (ABC) transport north of Severnaya Zemlya with a 2015–2018 mooring array. Hydrographic changes along the ABC pathway are most prominent at the continental slope due to the interaction with shelf water. Seasonality of water masses from the shelf sea was observed in transport, temperature and off‐shelf excursions within the ABC.
    Beschreibung: Bundesministerium für Bildung und Forschung http://dx.doi.org/10.13039/501100002347
    Beschreibung: EC Horizon 2020 Framework Programme http://dx.doi.org/10.13039/100010661
    Beschreibung: Russian Science Foundation http://dx.doi.org/10.13039/501100006769
    Beschreibung: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Beschreibung: https://doi.pangaea.de/10.1594/PANGAEA.951363
    Beschreibung: https://doi.pangaea.de/10.1594/PANGAEA.951394
    Beschreibung: https://doi.pangaea.de/10.1594/PANGAEA.951394
    Beschreibung: https://doi.pangaea.de/10.1594/PANGAEA.954244
    Beschreibung: https://doi.pangaea.de/10.1594/PANGAEA.954249
    Beschreibung: https://doi.pangaea.de/10.1594/PANGAEA.954299
    Beschreibung: https://doi.pangaea.de/10.1594/PANGAEA.954352
    Schlagwort(e): ddc:551.48 ; Arctic Boundary Current ; seasonal transport variability ; water mass transport ; along‐slope current
    Sprache: Englisch
    Materialart: doc-type:article
    Standort Signatur Erwartet Verfügbarkeit
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  • 2
    Publikationsdatum: 2024-04-22
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , isiRev
    Standort Signatur Erwartet Verfügbarkeit
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  • 3
    facet.materialart.
    Unbekannt
    American Geophysical Union (AGU)
    In:  EPIC3Journal of Geophysical Research - Oceans, American Geophysical Union (AGU), 128(1), ISSN: 2169-9275
    Publikationsdatum: 2024-05-08
    Beschreibung: We assessed the spatial and temporal variability of the Arctic Boundary Current (ABC) using seven oceanographic moorings, deployed across the continental slope north of Severnaya Zemlya in 2015–2018. Transports and individual water masses were quantified based on temperature and salinity recorders and current profilers. Our results were compared with observations from the northeast Svalbard and the central Laptev Sea continental slopes to evaluate the hydrographic transformation along the ABC pathway. The highest velocities (〉0.30 m s−1) of the ABC occurred at the upper continental slope and decreased offshore to below 0.03 m s−1 in the deep basin. The ABC showed seasonal variability with velocities two times higher in winter than in summer. Compared to upstream conditions in Svalbard, water mass distribution changed significantly within 20 km of the shelf edge due to mixing with- and intrusion of shelf waters. The ABC transported 4.15 ± 0.3 Sv in the depth range 50–1,000 m, where 0.88 ± 0.1, 1.5 ± 0.2, 0.61 ± 0.1 and 1.0 ± 0.15 Sv corresponded to Atlantic Water (AW), Dense Atlantic Water (DAW), Barents Sea Branch Water (BSBW) and Transformed Atlantic Water (TAW). 62–70% of transport was constrained to within 30–40 km of the shelf edge, and beyond 84 km, transport increases were estimated to be 0.54 Sv. Seasonality of TAW derived from local shelf-processes and advection of seasonal-variable Fram Strait waters, while BSBW transport variability was dominated by temperature changes with maximum transport coinciding with minimum temperatures. Further Barents Sea warming will likely reduce TAW and BSBW transport leading to warmer conditions along the ABC pathway.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , isiRev
    Format: application/pdf
    Standort Signatur Erwartet Verfügbarkeit
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  • 4
    Publikationsdatum: 1984-11-19
    Print ISSN: 0014-5793
    Digitale ISSN: 1873-3468
    Thema: Biologie , Chemie und Pharmazie
    Standort Signatur Erwartet Verfügbarkeit
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  • 5
    Publikationsdatum: 1983-12-01
    Print ISSN: 0014-2956
    Digitale ISSN: 1432-1033
    Thema: Biologie , Chemie und Pharmazie , Medizin
    Standort Signatur Erwartet Verfügbarkeit
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  • 6
  • 7
    Publikationsdatum: 2023-02-08
    Beschreibung: A 15-yr duration record of mooring observations from the eastern (〉70°E) Eurasian Basin (EB) of the Arctic Ocean is used to show and quantify the recently increased oceanic heat flux from intermediate-depth (~150–900 m) warm Atlantic Water (AW) to the surface mixed layer and sea ice. The upward release of AW heat is regulated by the stability of the overlying halocline, which we show has weakened substantially in recent years. Shoaling of the AW has also contributed, with observations in winter 2017–18 showing AW at only 80 m depth, just below the wintertime surface mixed layer, the shallowest in our mooring records. The weakening of the halocline for several months at this time implies that AW heat was linked to winter convection associated with brine rejection during sea ice formation. This resulted in a substantial increase of upward oceanic heat flux during the winter season, from an average of 3–4 W m−2 in 2007–08 to 〉10 W m−2 in 2016–18. This seasonal AW heat loss in the eastern EB is equivalent to a more than a twofold reduction of winter ice growth. These changes imply a positive feedback as reduced sea ice cover permits increased mixing, augmenting the summer-dominated ice-albedo feedback.
    Materialart: Article , PeerReviewed
    Format: text
    Standort Signatur Erwartet Verfügbarkeit
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  • 8
    Publikationsdatum: 2023-02-08
    Beschreibung: A 15-year (2004–2018) record of mooring observations from the upper 50 m of the ocean in the eastern Eurasian Basin reveals increased current speeds and vertical shear, associated with an increasing coupling between wind, ice, and the upper ocean over 2004–2018, particularly in summer. Substantial increases in current speeds and shears in the upper 50 m are dominated by a two times amplification of currents in the semidiurnal band, which includes tides and wind-forced near-inertial oscillations. For the first time the strengthened upper ocean currents and shear are observed to coincide with weakening stratification. This coupling links the Atlantic Water heat to the sea ice, a consequence of which would be reducing regional sea ice volume. These results point to a new positive feedback mechanism in which reduced sea ice extent facilitates more energetic inertial oscillations and associated upper-ocean shear, thus leading to enhanced ventilation of the Atlantic Water.
    Materialart: Article , PeerReviewed
    Format: text
    Format: text
    Standort Signatur Erwartet Verfügbarkeit
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  • 9
    Publikationsdatum: 2023-10-28
    Beschreibung: A standard Sea-Bird Electronics SBE911+ CTD system with a temperature and conductivity sensor was used to measure temperature, conductivity, and pressure at 180 stations during the Russian-international expedition Transarktika-2019 Leg 1 in the Barents Sea in March-May 2019 aboard the research vessel Akademik Tryoshnikov. We followed the manufacturer's recommendation to calculate salinity using Seabird processing software. The salinity is reported as Practical Salinity (PSU). Data were averaged at depth ranges of 1 m. Data are provided by the Antarctic and Arctic Research Institute (AARI) and reprocessed at the Helmholtz Centre for Polar and Marine Research, Alfred Wegener Institute. The Transarktika-2019 expedition was made possible by funding from the Russian Federal Service for Hydrometeorology and Environmental Monitoring (Roshydromet). The scientific research was also supported by RFBR grants No. 18-05-60048 and 18-05-60083.
    Schlagwort(e): Akademik Tryoshnikov; Arctic Ocean; AT19001-1; AT19002-1; AT19004-1; AT19005-1; AT19006-1; AT19007-1; AT19008-1; AT19009-1; AT19010-1; AT19011-1; AT19012-1; AT19013-1; AT19014-1; AT19015-1; AT19016-1; AT19017-1; AT19018-1; AT19019-1; AT19020-1; AT19021-1; AT19022-1; AT19023-1; AT19024-1; AT19025-1; AT19026-1; AT19027-1; AT19028-1; AT19029-1; AT19030-1; AT19031-1; AT19032-1; AT19033-1; AT19034-1; AT19035-1; AT19036-1; AT19037-1; AT19038-1; AT19039-1; AT19040-1; AT19041-1; AT19042-1; AT19043-1; AT19044-1; AT19045-1; AT19046-1; AT19047-1; AT19048-1; AT19049-1; AT19050-1; AT19051-1; AT19052-1; AT19053-1; AT19054-1; AT19055-1; AT19056-1; AT19057-1; AT19058-1; AT19059-1; AT19060-1; AT19061-1; AT19062-1; AT19063-1; AT19064-1; AT19065-1; AT19066-1; AT19067-1; AT19068-1; AT19069-1; AT19070-1; AT19071-1; AT19072-1; AT19073-1; AT19074-1; AT19075-1; AT19076-1; AT19077-1; AT19078-1; AT19079-1; AT19080-1; AT19081-1; AT19082-1; AT19083-1; AT19084-1; AT19085-1; AT19086-1; AT19086-2; AT19086-3; AT19087-1; AT19088-1; AT19089-1; AT19089-2; AT19089-3; AT19090-1; AT19091-1; AT19092-1; AT19092-2; AT19092-3; AT19093-1; AT19094-1; AT19095-1; AT19095-2; AT19095-3; AT19096-1; AT19097-1; AT19098-1; AT19099-1; AT19100-1; AT19101-1; AT19102-1; AT19103-1; AT19104-1; AT19105-1; AT19106-1; AT19107-1; AT19108-1; AT19109-1; AT19110-1; AT19111-1; AT19112-1; AT19113-1; AT19114-1; AT19115-1; AT19116-1; AT19117-1; AT19118-1; AT19119-1; AT19120-1; AT19121-1; AT19122-1; AT19123-1; AT19124-1; AT19125-1; AT19126-1; AT19127-1; AT19128-1; AT19130-1; AT19131-1; AT19132-1; AT19133-1; AT19134-1; AT19135-1; AT19136-1; AT19137-1; AT19138-1; AT19139-1; AT19140-1; AT19141-1; AT19142-1; AT19148-1; AT19149-1; AT19150-1; AT19151-1; AT19152-1; AT19153-1; AT19154-1; AT19155-1; AT19156-1; AT19157-1; AT19158-1; AT19159-1; AT19160-1; AT19161-1; AT19162-1; AT19163-1; AT19164-1; AT19165-1; AT19166-1; AT19167-1; AT19168-1; AT19169-1; AT19170-1; AT19171-1; AT19172-1; AT19173-1; AT19174-1; AT19175-1; AT19176-1; AT19177-1; AT19178-1; AT19179-1; Barents Sea; Calculated; CATS; CATS - The Changing Arctic Transpolar System; Conductivity; CTD, Sea-Bird, SBE 911plus; CTD/Rosette; DATE/TIME; Density, sigma-theta (0); DEPTH, water; ELEVATION; Event label; Ice drift experiment SEVERNYI POLYUS 2019; Kara Sea; LATITUDE; LONGITUDE; Number of scans; Pressure, water; Salinity; St. Anna Trough; Temperature, water; Temperature, water, potential; Transarktika-2019_Leg1
    Materialart: Dataset
    Format: text/tab-separated-values, 288309 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 10
    Publikationsdatum: 2024-04-20
    Beschreibung: Shipboard loosely-tethered free-falling microstructure (MSS) measurements were carried out during expedition Transdrift-XXIV to the eastern Arctic Ocean onboard the Akademik Tryoshnikov (AT2018). The expedition was jointly organized between the US-Russian NABOS (Nansen and Amundsen Basin Observational System), the German-Russian CATS (Changing Arctic Transpolar System, funded by BMBF), and the TICE-project funded by the Alfred-Wegener-Institute. 236 stations were carried out between 25 August and 23 September 2018. The profiler MSS90L manufactured by Sea and Sun Technology samples at 1024 Hz and was equipped with temperature, salinity, shear, and fluorescence sensors. Details on data processing can be found in Schulz et al. (2021). Additional parameters and metadata are provided in the attached netcdf file.
    Schlagwort(e): Akademik Tryoshnikov; Arctic Ocean; AT18_009_2; AT18_009_5; AT18_016_2; AT18_017_1; AT18_018_2; AT18_019_2; AT18_020_2; AT18_022_4; AT18_023_2; AT18_024_2; AT18_025_4; AT18_044_2; AT18_045_2; AT18_046_2; AT18_047_3; AT18_048_2; AT18_049_2; AT18_050_2; AT18_060_3; AT18_061_2; AT18_062_2; AT18_063_2; AT18_085_4; AT18_093_2; AT18_094_2; AT18_095_2; AT18_102; AT18_103; AT18_116_2; AT18_117_2; AT18_118_2; AT18_119_2; AT18_120_2; AT18_122_2; AT2018, TICE, NABOS; AWI_PhyOce; Cast number; DATE/TIME; DEPTH, water; Dissipation rate; Event label; Laptev Sea; LATITUDE; LONGITUDE; microstructure; Micro structure probe; MSS; ocean heat flux; Physical Oceanography @ AWI; Pressure, water; Profile; Salinity; System Laptev-Sea: Transdrift; Temperature, water, potential; TRANSDRIFT; Transdrift-XXIV; turbulence; Turbulence probe MSS90L, Sea and Sun Technology
    Materialart: Dataset
    Format: text/tab-separated-values, 447242 data points
    Standort Signatur Erwartet Verfügbarkeit
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