GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • 2015-2019  (4)
  • 2010-2014  (6)
Document type
Language
Years
Year
  • 1
    Keywords: Oceanography. ; Environmental sciences. ; Marine ecology -- Arctic Ocean. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (461 pages)
    Edition: 1st ed.
    ISBN: 9789401788632
    DDC: 577.82091632
    Language: English
    Note: Intro -- Contents -- Contributors -- Chapter 1: The Pacific Arctic Region: An Introduction -- 1.1 Introduction -- 1.2 The Pacific Arctic Region -- 1.3 Physical Processes, Hydrography and Sea Ice: Field and Modeling -- 1.4 Atmospheric Forcing and Sea Ice -- 1.5 Physical Processes and Modeling -- 1.6 Carbon Transformations and Cycling -- 1.7 Lower and Upper Trophic Levels and Ecosystem Modeling -- 1.8 Summary -- References -- Chapter 2: Recent and Future Changes in the Meteorology of the Pacific Arctic -- 2.1 Introduction -- 2.2 Climatological Fields -- 2.3 Storms and Temporal Variability -- 2.4 The Differences of the Pacific Sector Relative to the Larger Arctic System -- 2.5 The Future Climate of the Pacific Arctic -- 2.6 Summary -- References -- Chapter 3: Recent Variability in Sea Ice Cover, Age, and Thickness in the Pacific Arctic Region -- 3.1 Introduction -- 3.2 Sea Ice Cover -- 3.2.1 Trends in Sea Ice Cover -- 3.2.2 Interannual Variability in Sea Ice Cover -- 3.3 Sea Ice Age -- 3.3.1 Sea Ice Age Data and Analysis -- 3.3.2 Recent Variability in Sea Ice Age -- 3.4 Sea Ice Thickness -- 3.4.1 Sea Ice Thickness Data and Background -- 3.4.2 Sea Ice Thickness Model Description -- 3.4.3 Sea Ice Thickness Model Validation -- 3.4.4 Recent Variability in Modeled Sea Ice Thickness -- 3.4.5 Potential Mechanisms of Sea Ice Thinning -- 3.5 Implications and Possible Future States -- 3.6 Summary -- References -- Chapter 4: Abrupt Climate Changes and Emerging Ice- Ocean Processes in the Pacific Arctic Region and the Bering Sea -- 4.1 Introduction -- 4.2 Data and Methods -- 4.3 Leading Climate Forcing: Arctic Dipole (DA) Pattern -- 4.4 Investigating Mechanisms Responsible for Arctic Sea Ice Minima Using PIOMAS -- 4.5 Bering Strait Heat Transport and the DA -- 4.6 Modeling the Bering Sea Cold Pool Using CIOM. , 4.7 Modeling Landfast Ice in the Beaufort-Chukchi Seas Using CIOM -- 4.8 Possible Air-Ice-Sea Feedback Loops in the Western Arctic -- 4.9 Summary -- References -- Chapter 5: The Large Scale Ocean Circulation and Physical Processes Controlling Pacific-Arctic Interactions -- 5.1 Introduction -- 5.2 The Northern North Pacific, Gulf of Alaska, and Alaskan Stream -- 5.3 Western Subarctic Gyre -- 5.4 Bering Sea -- 5.5 Chukchi Sea -- 5.6 Beaufort Sea -- 5.7 Heat/Freshwater Content and Sea Ice -- 5.8 Summary -- References -- Chapter 6: Shelf-Break Exchange in the Bering, Chukchi and Beaufort Seas -- 6.1 Introduction -- 6.2 The Bering Shelf-Break -- 6.3 The Chukchi and Beaufort Shelf-Break -- 6.3.1 Shelf-Basin Connections -- 6.3.2 Instabilities of the Shelf-Break Jet -- 6.3.3 Wind-Driven Exchange -- 6.4 Undersea Canyons of the Chukchi and Beaufort Shelves -- 6.4.1 Herald Canyon -- 6.4.2 Barrow Canyon -- 6.4.3 Mackenzie Trough -- 6.5 Polynya-Formed Dense Shelf Water -- 6.6 Summary -- 6.6.1 Bering Shelf-Break -- 6.6.2 Chukchi/Beaufort Shelf-Break -- References -- Chapter 7: On the Flow Through Bering Strait: A Synthesis of Model Results and Observations -- 7.1 Introduction -- 7.2 Model Descriptions -- 7.2.1 Bering Ecosystem Study Ice-Ocean Modeling and Assimilation System (BESTMAS) -- 7.2.2 Estimating the Circulation and Climate of the Ocean, Phase II (ECCO2) -- 7.2.3 Naval Postgraduate School Arctic Modeling Effort (NAME) -- 7.2.4 Nucleus for European Modelling of the Ocean (NEMO) with ORCA Configuration -- 7.2.5 Pan-Arctic Ice-Ocean Modeling and Assimilation System (PIOMAS) -- 7.3 Bering Strait Observational Mooring Data -- 7.4 Results -- 7.5 Discussion -- 7.6 Summary -- References -- Chapter 8: Carbon Fluxes Across Boundaries in the Pacific Arctic Region in a Changing Environment -- 8.1 Introduction -- 8.2 Geographic and Water Mass Features. , 8.2.1 Geographic Definition and Description -- 8.2.2 Water-Mass Characterizations -- 8.3 Pacific Ocean Inflow -- 8.4 Fluxes Across the Arctic Land-Sea Interface -- 8.5 CO 2 Flux Across the Air-Sea Boundary -- 8.5.1 Sea Surface p CO 2 Distribution -- 8.5.2 Air-Sea CO 2 Flux -- 8.6 Impact of Seasonal Sea-Ice Cycle -- 8.7 Overall DIC Budget -- 8.8 Summary -- References -- Chapter 9: Carbon Biogeochemistry of the Western Arctic: Primary Production, Carbon Export and the Controls on Ocean Acidification -- 9.1 Introduction -- 9.2 Primary Production -- 9.2.1 Northern Bering Sea -- 9.2.2 Chukchi Sea -- 9.2.3 Deep Canada Basin -- 9.3 DOC Production -- 9.3.1 Spatial Variability -- 9.3.2 The Use of DOC/Salinity Relationships -- 9.3.3 Dynamical Characterization of tDOC-Inputs & -- Sinks -- 9.4 Export Flux of Particulate Organic Carbon -- 9.4.1 Regional Case Studies -- 9.4.1.1 Chukchi Sea: The Shelf Basin Interaction Study (SBI-II) -- 9.4.1.2 Mackenzie Shelf: Canadian Arctic Shelf Exchange Study (CASES) -- 9.4.1.3 Laptev Sea, Northern Baffin Bay and the Beaufort Sea Shelves -- 9.4.1.4 Eastern and Central Arctic Ocean: Polarstern ARK-XXII/2 Expedition -- 9.4.2 Conclusions -- 9.5 Grazing -- 9.6 Benthic Carbon Cycling -- 9.6.1 Sediment Nutrient Efflux -- 9.7 Contribution of Heterotrophic Bacteria to Carbon Cycling -- 9.7.1 Respiration by Heterotrophic Bacteria -- 9.7.2 Biomass Production by Heterotrophic Bacteria and Phytoplankton -- 9.7.3 Growth Efficiency in the Arctic Ocean -- 9.7.4 Implications for Shelf-Basin Exchange -- 9.8 Ocean Acidification -- 9.8.1 The Bering Sea -- 9.8.2 The Western Arctic Ocean -- 9.9 Summary -- References -- Chapter 10: Biodiversity and Biogeography of the Lower Trophic Taxa of the Pacific Arctic Region: Sensitivities to Climate Change -- 10.1 General Introduction -- 10.2 Phytoplankton in the PAR -- 10.2.1 Introduction. , 10.2.2 Phytoplankton and Sea Ice Algae: An Overview -- 10.2.3 Latitudinal Variation of Phytoplankton Biodiversity and Community Composition in the Western Arctic Ocean -- 10.2.4 Synechococcus -- 10.2.5 Sensitivities to Habitat Changes -- 10.3 Heterotrophic Microbes in the PAR -- 10.3.1 Introduction -- 10.3.2 Viruses -- 10.3.3 Bacterial Diversity -- 10.3.4 Bacterial and Archaeal Diversity Levels in the Arctic Ocean Versus Lower-Latitude Oceans -- 10.3.5 Diversity and Distribution of Heterotrophic Protists -- 10.3.5.1 Diversity of Heterotrophic Protists Assessed by Microscopy -- 10.3.5.2 Diversity of Heterotrophic Protists Assessed by Molecular Genetics -- 10.3.5.3 Biogeographical and Depth Distribution of Heterotrophic Protists -- 10.3.5.4 Heterotrophic Microbes: Future Research -- 10.4 Benthic Fauna of the PAR -- 10.4.1 Introduction -- 10.4.2 Benthic Fauna of the Northern Bering, Chukchi, and Western Beaufort Seas -- 10.4.2.1 Environmental Setting -- 10.4.2.2 General Biogeography -- 10.4.3 Benthic Invertebrate Patterns in the Canadian Beaufort Sea Shelf -- 10.4.3.1 Environmental Setting -- 10.4.3.2 General Biogeography and Biodiversity -- 10.4.4 Deep-Sea Benthos -- 10.4.5 Effect of Climate Change on Benthic Fauna of the PAR -- 10.5 Sea Ice Associated Diversity and Production in the PAR -- 10.5.1 Introduction -- 10.5.2 Primary Producers: Diversity, Abundance and Activity -- 10.5.3 Sea Ice Meiofauna Abundance and Diversity -- 10.5.4 Effects of Climate Change -- 10.6 Biodiversity and Biogeography of Metazoan Zooplankton of the PAR -- 10.6.1 Introduction -- 10.6.2 Species Diversity -- 10.6.3 Zooplankton Advection: Expatriate Analysis -- 10.6.4 Horizontal Zooplankton Community Structure -- 10.6.5 Vertical Distribution of Zooplankton in the Deep Waters of the PAR -- 10.6.6 Long-Term Change -- 10.7 Summary -- References. , Chapter 11: Marine Fishes, Birds and Mammals as Sentinels of Ecosystem Variability and Reorganization in the Pacific Arctic Region -- 11.1 Introduction -- 11.1.1 Ecological Scale -- 11.2 Overview: Ecology of Upper Trophic Level (UTL) Species -- 11.2.1 Fishes and Crabs -- 11.2.1.1 Northern Bering and Chukchi Seas -- 11.2.1.2 Beaufort Sea -- 11.2.2 Marine Birds -- 11.2.2.1 At-Sea Distribution -- 11.2.2.2 Breeding Colonies -- 11.2.2.3 Seasonal Dynamics -- 11.2.3 Marine Mammals -- 11.2.3.1 Core Arctic Species -- 11.2.3.2 Seasonally Migrant Species -- 11.3 Case Studies: Responses of UTL Species to Environmental Variability -- 11.3.1 Fishes and Crabs -- 11.3.1.1 Salmon and Forage Fish in the Northern Bering Sea -- 11.3.1.2 Snow Crab in the Chukchi Sea -- 11.3.1.3 Demersal Fish and Crab in the Beaufort Sea -- 11.3.2 Marine Birds -- 11.3.2.1 Nesting Auklets and the Anadyr Current -- 11.3.3 Eiders During Winter and Migration -- 11.3.4 Marine Mammals -- 11.3.4.1 Timing and Relative Abundance of Bowhead Whales Feeding in the Canadian Beaufort Sea -- 11.3.4.2 Body Condition of Ringed Seals in the Western Canadian Arctic -- 11.3.4.3 Changes in Life-History and Diet of Walruses and Seals in the Northern Bering and Chukchi Seas -- 11.4 UTL Species as Ecosystem Sentinels -- 11.4.1 UTL-Focused Research Framework -- 11.4.1.1 Trophic Interactions -- 11.4.1.2 Foraging Dynamics -- 11.4.1.3 Species Composition -- 11.5 Summary -- 11.5.1 Tracking Biological Responses in an Era of Rapid Change and Extreme Events -- 11.5.2 Integration of Science and Local Knowledge -- 11.6 Personal Communications -- References -- Chapter 12: Progress and Challenges in Biogeochemical Modeling of the Pacific Arctic Region -- 12.1 Introduction -- 12.2 PAR Characteristics Particularly Relevant for Biogeochemical Modeling -- 12.3 A Brief History of PAR Biogeochemical Models. , 12.4 Modeling PAR in 1-D: Introduction and Locations.
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2014-03-01
    Description: With changing climate, delineation of protected areas for sensitive species must account for long-term variability and geographic shifts of key habitat elements. Projecting the future adequacy of protected areas requires knowing major factors that drive such changes, and how readily the animals adjust to altered resources. In the Arctic, the viability of habitats for marine birds and mammals often depends on sea ice to dissipate storm waves and provide platforms for resting. However, some wind conditions (including weak winds during extreme cold) can consolidate pack ice into cover so dense that air-breathing divers are excluded from the better feeding areas. Spectacled Eiders (Somateria fischeri) winter among leads (openings) in pack ice in areas where densities of their bivalve prey are quite high. During winter 2009, however, prevailing winds created a large region of continuous ice with inadequate leads to allow access to areas of dense preferred prey. Stable isotope and fatty acid biomarkers indicated that, under these conditions, the eiders did not diversify their diet to include abundant non-bivalve taxa but did add a smaller, less preferred, bivalve species. Consistent with a computer model of eider energy balance, the body fat of adult eiders in 2009 was 33?35% lower than on the same date (19 March) in 2001 when ice conditions allowed access to higher bivalve densities. Ice cover data suggest that the eiders were mostly excluded from areas of high bivalve density from January to March in about 30% of 14 winters from 1998 to 2011. Thus, even without change in total extent of ice, shifts in prevailing winds can alter the areal density of ice to reduce access to important habitats. Because changes in wind-driven currents can also rearrange the dispersion of prey, the potential for altered wind patterns should be an important concern in projecting effects of climate change on the adequacy of marine protected areas for diving endotherms in the Arctic. # doi:10.1890/13-0411.1
    Print ISSN: 1051-0761
    Electronic ISSN: 1939-5582
    Topics: Biology
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 3
    Publication Date: 2014-09-01
    Description: Climate warming in seasonally ice-covered seas is expected to reduce the extent and duration of annual sea ice. Resulting changes in sea ice related blooms of ice algae or phytoplankton may in turn alter the timing, magnitude, or quality of organic matter inputs to the sea floor. If benthic taxa rely differently on direct consumption of settling fresh microalgae for growth and reproduction, altered blooms may lead to reorganization of deposit-feeding assemblages. To assess the potential for such changes, we examined the diets of five abundant deposit-feeders (three infaunal bivalves, a polychaete, and a brittle star) with different feeding modes over the course of the spring bloom in May?June 2007 in the north-central Bering Sea (30?90 m depth). Short-term data from gut contents reflected feeding modes, with the bivalves Macoma calcarea, Ennucula tenuis, and Nuculana radiata, and the brittle star Ophiura sarsi, responding more quickly to deposition of fresh algae than did the head-down polychaete Pectinaria hyperborea. Fatty acid biomarkers also indicated rapid ingestion of settling algae by the bivalves (especially Macoma) and the brittle star, while Pectinaria continued to ingest mainly bacteria. Fatty acid biomarkers did not indicate any unique dietary importance of ice algae released from melting ice. Longer-term inference from stable isotopes suggested that fresh microalgae contributed little to overall carbon assimilated by any of these species. Instead, deposit-feeders appeared to select a consistent fraction from the pool of sediment organic matter, probably heterotrophic microbes, microbial products, and reworked phytodetritus that form a longer-term sediment ?food bank.? Redistribution of settled organic matter via scouring and accumulation by currents, as well as the multi-year life spans of macroinvertebrates, may further overwhelm effects of short-term variations in the timing, magnitude, and dispersion of blooms in the water column. More diet data are needed from midsummer to account for any lag in assimilation of fresh microalgae at these cold temperatures. Nevertheless, our results suggest that if annual sea ice cover is reduced, increased production of phytoplankton during longer ice-free periods could replace inputs of ice-associated microalgae to the sediment food bank used by deposit-feeders. # doi:10.1890/13-0486.1
    Print ISSN: 1051-0761
    Electronic ISSN: 1939-5582
    Topics: Biology
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 4
    Publication Date: 2023-12-18
    Keywords: Alpha Helix; Ampeliscidae, biomass, wet mass; Amphipoda; Amphipoda, biomass, wet mass; Chukchi Sea; Cruise1988_St045; Cruise1988_St061; Cruise1988_St072; Cruise1988_St089; Cruise1988_St100; Cruise1988_St104; Cruise2004_St011; Cruise2005_St013; Cruise2006_St043; Cruise2006_St044; Cruise2006_St045; Cruise2006_St046; Cruise2006_St047; Cruise2006_St048; Cruise2006_St049; Cruise2006_St050; Cruise2006_St051; Cruise2006_St052; Cruise2006_St053; Cruise2006_St054; Cruise2006_St055; Cruise2006_St056; Cruise2006_St057; Cruise2006_St058; Cruise2006_St059; Cruise2006_St060; Cruise2006_St061; Cruise2006_St062; Cruise2006_St063; Cruise2006_St064; Cruise2006_St065; Cruise2006_St076; Cruise59; Cruise59_59120_VG; Cruise59_59121_VG; Cruise59_59123_VG; Cruise73; Cruise73_73011_VG; Cruise73_73018_VG; Cruise73_73024_VG; Cruise73_73027_VG; Cruise73_73075_VG; Cruise73_73080_VG; Cruise73_73081_VG; Cruise73_73104_VG; Cruise73_7312_VG; Cruise74; Cruise74_74002_VG; Cruise74_74010_VG; Cruise85; Cruise85_85090_VG; DATE/TIME; DEPTH, sediment/rock; Elevation of event; Event label; Latitude of event; Longitude of event; Reference/source; Sample amount; Station label; van Veen Grab; VGRAB
    Type: Dataset
    Format: text/tab-separated-values, 274 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 5
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Heide-Jørgensen, Mads Peter; Laidre, Kristin L; Litovka, D; Villum Jensen, M; Grebmeier, Jacqueline M; Sirenko, Boris I (2012): Identifying gray whale (Eschrichtius robustus) foraging grounds along the Chukotka Peninsula, Russia, using satellite telemetry. Polar Biology, 35(7), 1035-1045, https://doi.org/10.1007/s00300-011-1151-6
    Publication Date: 2023-12-13
    Description: The purpose of this study was to evaluate summer and fall residency and habitat selection by gray whales, Eschrichtius robustus, together with the biomass of benthic amphipod prey on the coastal feeding grounds along the Chukotka Peninsula. Thirteen gray whales were instrumented with satellite transmitters in September 2006 near the Chukotka Peninsula, Russia. Nine transmitters provided positions from whales for up to 81 days. The whales travelled within 5 km of the Chukotka coast for most of the period they were tracked with only occasional movements offshore. The average daily travel speeds were 23 km/day (range 9-53 km/day). Four of the whales had daily average travel speeds 〈1 km/day suggesting strong fidelity to the study area. The area containing 95% of the locations for individual whales during biweekly periods was on average 13,027 km**2 (range 7,097-15,896 km**2). More than 65% of all locations were in water 〈30 m, and between 45 and 70% of biweekly kernel home ranges were located in depths between 31 and 50 m. Benthic density of amphipods within the Bering Strait at depths 〈50 m was on average ~54 g wet wt/m**2 in 2006. It is likely that the abundant benthic biomass is more than sufficient forage to support the current gray whale population. The use of satellite telemetry in this study quantifies space use and movement patterns of gray whales along the Chukotka coast and identifies key feeding areas.
    Keywords: International Polar Year (2007-2008); IPY
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 6
    Publication Date: 2018-05-06
    Description: Polar marine regions are facing rapid changes induced by climate change, with consequences for local faunal populations, but also for overall ecosystem functioning, goods and services. Yet given the complexity of polar marine ecosystems, predicting the mode, direction and extent of these consequences remains challenging. Trait-based approaches are increasingly adopted as a tool by which to explore changes in functioning, but trait information is largely absent for the high latitudes. Some understanding of trait–function relationships can be gathered from studies at lower latitudes, but given the uniqueness of polar ecosystems it is questionable whether these relationships can be directly transferred. Here we discuss the challenges of using trait-based approaches in polar regions and present a roadmap of how to overcome them by following six interlinked steps: (1) forming an active, international research network, (2) standardizing terminology and methodology, (3) building and crosslinking trait databases, (4) conducting coordinated trait-function experiments, (5) implementing traits into models, and finally, (6) providing advice to management and stakeholders. The application of trait-based approaches in addition to traditional species-based methods will enable us to assess the effects of rapid ongoing changes on the functioning of marine polar ecosystems. Implementing our roadmap will make these approaches more easily accessible to a broad community of users and consequently aid understanding of the future polar oceans.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev , info:eu-repo/semantics/article
    Format: application/pdf
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 7
    facet.materialart.
    Unknown
    PERGAMON-ELSEVIER SCIENCE LTD
    In:  EPIC3Deep-Sea Research Part II-Topical Studies in Oceanography, PERGAMON-ELSEVIER SCIENCE LTD, online, pp. 1-14, ISSN: 0967-0645
    Publication Date: 2017-12-31
    Description: The snow crab Chionoecetes opilio and Arctic lyre crab Hyas coarctatus are prominent members of the Chukchi Sea epifaunal community. A better understanding of their life history will aid in determining their role in this ecosystem in light of the changing climate and resource development. In this study, the size frequency distribution, growth, and mortality of these two crab species was examined in 2009, 2010, 2012, and 2013 to determine temporal and spatial patterns within the eastern Chukchi Sea, and to identify potential environmental drivers of the observed patterns. Temporally, the mean size of both sexes of C. opilio and H. coarctatus decreased significantly from 2009 to 2013, with the number of rare maximum sized organisms decreasing significantly to near absence in the latter two study years. Spatially, the mean size of male and female crabs of both species showed a latitudinal trend, decreasing from south to north in the investigation area. Growth of both sexes of C. opilio and H. coarctatus was linear over the sampled size range, and mortality was highest in the latter two study years. Life history features of both species related to different environmental parameters in different years, ranging from temperature, the sediment carbon to nitrogen ratio of the organic content, and sediment grain size distribution. Likely explanations for the observed temporal and spatial variability are ontogenetic migrations of mature crabs to warmer areas possibly due to cooler water temperatures in the latter two study years, or interannual fluctuations, which have been reported for C. opilio populations in other areas where successful waves of recruitment were estimated to occur in eight year intervals. Further research is suggested to determine if the spatial and temporal patterns found in this study are part of the natural variability in this system or if they are an indication of long-term trends.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 8
    Publication Date: 2015-06-11
    Description: On-going climate warming is causing a dramatic loss of sea-ice in the Arctic Ocean and it is projected that the Arctic Ocean will become seasonally ice-free by 2040. Many studies of local Arctic food webs now exist and with this review paper we aim to synthesize these into a large-scale assessment of the current status of knowledge on the structure of various Arctic marine food webs, and their response to climate change, and to sea-ice retreat in particular. Key drivers of ecosystem change and potential consequences for ecosystem functioning and Arctic marine food webs are identified along the sea-ice gradient with special emphasis on the following regions: seasonally ice free Barents and Chukchi Seas, loose ice pack zone of the Polar Front (PF) and Marginal Ice Zone (MIZ), and permanently sea-ice covered high Arctic. Finally, we identify gaps existing in the knowledge of different Arctic marine food webs and provide recommendations for future studies.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 9
    facet.materialart.
    Unknown
    PERGAMON-ELSEVIER SCIENCE LTD
    In:  EPIC3Deep-Sea Research Part II-Topical Studies in Oceanography, PERGAMON-ELSEVIER SCIENCE LTD, 65-70, pp. 141-162, ISSN: 0967-0645
    Publication Date: 2015-01-13
    Description: The northern Bering Sea shelf is dominated by soft-bottom infauna and ecologically significant epifauna that are matched by few other marine ecosystems in biomass. The likely basis for this high benthic biomass is the intense spring bloom, but few studies have followed the direct sedimentation of organic material during the bloom peak in May. Satellite imagery, water column chlorophyll concentrations and surface sediment chlorophyll inventories were used to document the dynamics of sedimentation to the sea floor in both 2006 and 2007, as well as to compare to existing data from the spring bloom in 1994. An atmospherically-derived radionuclide, 7Be, that is deposited in surface sediments as ice cover retreats was used to supplement these observations, as were studies of light penetration and nutrient depletion in the water column as the bloom progressed. Chlorophyll biomass as sea ice melted differed significantly among the three years studied (1994, 2006, 2007). The lowest chlorophyll biomass was observed in 2006, after strong northerly and easterly winds had distributed relatively low nutrient water from near the Alaskan coast westward across the shelf prior to ice retreat. By contrast, in 1994 and 2007, northerly winds had less northeasterly vectors prior to sea ice retreat, which reduced the westward extent of low-nutrient waters across the shelf. Additional possible impacts on chlorophyll biomass include the timing of sea-ice retreat in 1994 and 2007, which occurred several weeks earlier than in 2006 in waters with the highest nutrient content. Late winter brine formation and associated water column mixing may also have impacts on productivity that have not been previously recognized. These observations suggest that interconnected complexities will prevent straightforward predictions of the influence of earlier ice retreat in the northern Bering Sea upon water column productivity and any resulting benthic ecosystem re-structuring as seasonal sea ice retreats in the northern Bering Sea.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 10
    Publication Date: 2022-05-25
    Description: Author Posting. © The Oceanography Society, 2015. This article is posted here by permission of The Oceanography Society for personal use, not for redistribution. The definitive version was published in Oceanography 28, no. 3 (2015): 68-83, doi:10.5670/oceanog.2015.58.
    Description: Using data from a number of summer surveys of the Chukchi Sea over the past decade, we investigate aspects in which the benthic fauna, sediment structure, and zooplankton there are related to circulation patterns and shelf hydrographic conditions. A flow speed map is constructed that reveals the major pathways on the shelf. Regions of enhanced flow speed are dictated by lateral constrictions—in particular, Bering Strait and Barrow and Herald Canyons—and by sloping topography near coastlines. For the most part, benthic epifaunal and macrofaunal suspension feeders are found in high flow regimes, while deposit feeders are located in regions of weaker flow. The major exceptions are in Bering Strait, where benthic sampling was underrepresented, and in Herald Canyon where the pattern is inexplicably reversed. Sediment grain size is also largely consistent with variations in flow speed on the shelf. Data from three biophysical surveys of the Chukchi Sea, carried out as part of the Russian-American Long-term Census of the Arctic program, reveal close relationships between the water masses and the zooplankton communities on the shelf. Variations in atmospheric forcing, particularly wind, during the three sampling periods caused significant changes in the lateral and vertical distributions of the summer and winter water masses. These water mass changes, in turn, were reflected in the amounts and species of zooplankton observed throughout the shelf in each survey. Our study highlights the close relationship between physical drivers (wind forcing, water masses, circulation, and sediment type) in the Chukchi Sea and the biological signals in the benthos and the plankton on a variety of time scales.
    Description: MP, RP, and CA were supported by Cooperative Agreement NA17RJ1223 between the National Oceanic and Atmospheric Administration (NOAA) and the Cooperative Institute for Climate and Ocean Research (CICOR) and Cooperative Agreements NA09OAR4320129 and NA14OAR4320158 between NOAA and the Cooperative Institute for the North Atlantic Region. This publication is the result in part of research sponsored by the Cooperative Institute for Alaska Research with funds from NOAA under cooperative agreements NA17RJ1224, NA13OAR4320056, and NA08OAR4320870 with the University of Alaska. KNK and EAE received financial support from the Russian Foundation for Basic Research under Grant 13-04-00551 and Russian Scientific Foundation Grant No. 14-50-00095. JG and LC received financial support from the NOAA Arctic Office (2004: NOAA-CIFAR 10-067; 2004, 2005, 2009 and 2012: NA08OAR4310608), along with NOAA Cooperative Agreement #NA09OAR4320129: WHOI CINAR #19930.00 UMCES.
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...