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  • 2010-2014  (14)
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  • 1
    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
    Location Call Number Limitation Availability
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  • 2
    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
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2014-04-22
    Description: As our current knowledge of biological and biogeochemical processes in the Arctic Ocean is mostly based on snapshots measurements obtained during summer and mostly limited to shelf regions, baseline information is missing to assess the impact of climate change on the biological carbon pump, particularly in the Central Arctic Ocean. Measurements on larger spatial and temporal scales are therefore urgently needed to monitor the response of the carbon cycle to warmer conditions in the Arctic Ocean. In this context, a call to maintain, develop and coordinate observing activities relying on bio-mooring arrays and long-term sequential sediment traps, key tools to detect change in the biogeochemical and ecological functioning of Arctic marine ecosystems, was made in a community white paper presented at the Arctic Observing Summit in 2013 (Forest et al., 2013). To answer this call, international cooperation for the development of an Arctic biogeochemical observatory network is needed. The development of such an international observatory network may be implemented through joint projects among existing programs and expanded to joint deployments of multidisciplinary moorings to fill geographical gaps, combine efforts and expertise, and share instruments and costs. To highlight the relevance of international collaboration, results from an ongoing joint project comparing export fluxes obtained in the Siberian Arctic Ocean by the Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research in Germany and ArcticNet, a Network of Centre of Excellence in Canada are presented. The combination of export flux measurements obtained at different periods and locations help to accurately assess the impact of reduced ice cover on primary productivity and carbon export in the Siberian Arctic Ocean. The Arctic Observing Summit 2014 represents a good opportunity to identify additional potential partners and discuss future collaborative projects.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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  • 4
    Publication Date: 2014-09-17
    Description: The unprecedented sea ice retreat that occurred in recent years in the Siberian Arctic Ocean possibly led to rapid changes in primary production and export fluxes of biogenic matter in this rarely sampled region. In 2011-2012, long-term sediment traps were deployed near the Gakkel Ridge in the Siberian sector of the Arctic Ocean. Export fluxes of biogenic matter obtained from this deployment indicated the export of a large quantity of Melosira arctica in June 2012. These export fluxes will be compared to fluxes obtained from previous long-term sediment traps deployments conducted over the shelf break of the northern Laptev Sea in 2005-2007, and over the Lomonosov Ridge in 1995-1996. This comparison of export fluxes obtained from the only 3 long-term sediment trap deployments performed in the Siberian Arctic Ocean will allow us to assess the factors affecting the timing, magnitude, and composition of the biogenic matter exported from upper waters to the seafloor in this region, and to estimate how earlier ice melt affected the export fluxes of biogenic matter in this sector of the Arctic Ocean.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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  • 5
    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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  • 6
    Publication Date: 2023-01-13
    Keywords: Abundance per volume; Date/Time of event; Depth, bottom/max; Depth, top/min; DEPTH, water; Event label; Latitude of event; Longitude of event; PLA; Plankton net; Sable-Island19910315_01; Sable-Island19910315_02; Sable-Island19910415_01; Sable-Island19910415_02; Sable-Island19910515_01; Sable-Island19910515_02; Sable-Island19910615_01; Sable-Island19910615_02; Sable-Island19910715_01; Sable-Island19910715_02; Sable-Island19910815_01; Sable-Island19910815_02; Sable-Island19910915_01; Sable-Island19910915_02; Sable-Island19911015_01; Sable-Island19911015_02; Sable-Island19911115_01; Sable-Island19911115_02; Sable-Island19911215_01; Sable-Island19911215_02; Sable-Island19920115_01; Sable-Island19920115_02; Sable-Island19920215_01; Sable-Island19920215_02; Sable-Island19920315_01; Sable-Island19920315_02; Scotian Shelf; Taxon/taxa; Type; Uniform resource locator/link to reference
    Type: Dataset
    Format: text/tab-separated-values, 152 data points
    Location Call Number Limitation Availability
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  • 7
    Publication Date: 2023-07-10
    Keywords: Amundsen Gulf, Canada; Area/locality; Beaufort Sea; CCGSA_4-10_CFL08; CCGS Amundsen; CFL08_D29-2; CFL08_D33-2; CFL08_D36-1; CFL08_D41-1; CFL08_F1-2; Circumpolar Flaw Lead Leg 4-10a; Cylindrotheca closterium; DATE/TIME; Elevation of event; Event label; Fragilariopsis cylindrus; Latitude of event; Longitude of event; MULT; Multiple investigations; Navicula directa; Navicula pelagica; Navicula septentrionalis; Nitzschia frigida; Nitzschia promare; Pauliella taeniata; Station label
    Type: Dataset
    Format: text/tab-separated-values, 60 data points
    Location Call Number Limitation Availability
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  • 8
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    PANGAEA
    In:  Supplement to: Wold, Anette; Darnis, Gerald; Søreide, Janne E; Leu, Eva; Philippe, Benoit; Fortier, Louis; Poulin, Michel; Kattner, Gerhard; Graeve, Martin; Falk-Petersen, Stig (2011): Life strategy and diet of Calanus glacialis during the winter–spring transition in Amundsen Gulf, south-eastern Beaufort Sea. Polar Biology, 34(12), 1929-1946, https://doi.org/10.1007/s00300-011-1062-6
    Publication Date: 2023-12-13
    Description: The copepod Calanus glacialis plays a key role in the lipid-based energy flux in Arctic shelf seas. By utilizing both ice algae and phytoplankton, this species is able to extend its growth season considerably in these seasonally ice-covered seas. This study investigated the impacts of the variability in timing and extent of the ice algal bloom on the reproduction and population success of C. glacialis. The vertical distribution, reproduction, amount of storage lipids, stable isotopes, fatty acid and fatty alcohol composition of C. glacialis were assessed during the Circumpolar Flaw Lead System Study. Data were collected in the Amundsen Gulf, south-eastern Beaufort Sea, from January to July 2008 with the core-sampling from March to April. The reduction in sea ice thickness and coverage observed in the Amundsen Gulf in 2007 and 2008 affected the life strategy and reproduction of C. glacialis. Developmental stages CIII and CIV dominated the overwintering population, which resulted in the presence of very few CV and females during spring 2008. Spawning began at the peak of the ice algal bloom that preceded the precocious May ice break-up. Although the main recruitment may have occurred later in the season, low abundance of females combined with a potential mismatch between egg production/development to the first feeding stage and phytoplankton bloom resulted in low recruitment of C. glacialis in the early summer of 2008.
    Keywords: AWI; International Polar Year (2007-2008); IPY
    Type: Dataset
    Format: application/zip, 5 datasets
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  • 9
    Publication Date: 2024-04-27
    Keywords: Amundsen Gulf, Canada; Beaufort Sea; Carbon, organic, particulate, flux; CCGSA_4-10_CFL08; CCGS Amundsen; CFL08_1208; CFL08_1216-2; CFL08_410; CFL08_421-1; CFL08_6006-1; CFL08_BS; CFL08_CA04; CFL08_CA05; CFL08_CA08; CFL08_CA16; CFL08_CA18; CFL08_D34-2; Circumpolar Flaw Lead Leg 4-10a; Date/Time of event; DEPTH, water; Event label; Latitude of event; Longitude of event; MOOR; Mooring; MULT; Multiple investigations; Northwestern Passages
    Type: Dataset
    Format: text/tab-separated-values, 12 data points
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  • 10
    Publication Date: 2024-05-15
    Keywords: all-cis-4,7,10,13,16,19-Docosahexaenoic acid of total fatty acids; all-cis-5,8,11,14,17-Eicosapentaenoic acid of total fatty acids; all-cis-6,9,12,15-Octadecatetraenoic acid of total fatty acids; Amundsen Gulf, Canada; Area/locality; Beaufort Sea; CCGSA_4-10_CFL08; CCGS Amundsen; CFL08_D36-1; CFL08_D38-1; CFL08_D41-1; CFL08_D43; CFL08_F1-2; CFL08_F2-3; Circumpolar Flaw Lead Leg 4-10a; cis-9-Hexadecenoic acid of total fatty acids (IUPAC: (9Z)-hexadec-9-enoic acid); DATE/TIME; Elevation of event; Event label; Fatty acids, standard deviation; High Performance Liquid Chromatography (HPLC); Latitude of event; Longitude of event; Monounsaturated fatty acids of total fatty acids; MULT; Multiple investigations; Polyunsaturated fatty acids of total fatty acids; Replicates; Sample type; Saturated fatty acids of total fatty acids; Station label
    Type: Dataset
    Format: text/tab-separated-values, 108 data points
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