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  • Elsevier  (2)
  • Dordrecht :Springer Netherlands,  (1)
  • 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.
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  • 2
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    Elsevier
    In:  Ocean Modelling, 137 . pp. 21-39.
    Publication Date: 2020-01-02
    Description: Oceanic fluxes through Fram Strait may significantly contribute to climate variations in the Arctic. However, their observations are difficult. Here, a 26-year numerical model simulation is used to derive oceanic proxies for interannual variability in heat fluxes through Fram Strait. It is found that variability in the cross-slope gradient of sea surface height (SSH) across the West Spitsbergen Current (WSC) can explain about 90% of the variance of winter and annual mean volume transports of Atlantic water at 79°N. Given the strong covariance between the simulated heat flux in the slope current along Svalbard and the corresponding volume transport, variability of the SSH gradient across the WSC is also found to account for about 80% of the variance of heat flux associated with the northward flow through Fram Strait. Moreover, variations in the SSH gradient across the Arctic Slope Current (ASC) northeast of Svalbard at 31°E explain about 85% of the variance of heat flux there and about 80% of the variance of the net heat flux upstream through Fram Strait. Finally, about 85% and 75% of the variance of the net heat flux through Fram Strait is associated with anomalies of the eastward volume transport and depth-averaged core velocity in the ASC, respectively. These relations indicate that monitoring of the flow in the ASC, even with a single current meter mooring, or of the SSH gradient across this current derived from either in situ or remote measurements may provide useful proxies for the heat import to the Arctic Ocean.
    Type: Article , PeerReviewed
    Format: text
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  • 3
    Publication Date: 2022-05-25
    Description: © The Author(s), 2014]. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Progress in Oceanography 136 (2015): 201-222, doi:10.1016/j.pocean.2014.08.012.
    Description: The Bering–Chukchi–Beaufort (BCB) population of bowhead whales (Balaena mysticetus) ranges across the seasonally ice-covered waters of the Bering, Chukchi, and Beaufort seas. We used locations from 54 bowhead whales, obtained by satellite telemetry between 2006 and 2012, to define areas of concentrated use, termed “core-use areas”. We identified six primary core-use areas and describe the timing of use and physical characteristics (oceanography, sea ice, and winds) associated with these areas. In spring, most whales migrated from wintering grounds in the Bering Sea to the Cape Bathurst polynya, Canada (Area 1), and spent the most time in the vicinity of the halocline at depths 〈75 m, which are within the euphotic zone, where calanoid copepods ascend following winter diapause. Peak use of the polynya occurred between 7 May and 5 July; whales generally left in July, when copepods are expected to descend to deeper depths. Between 12 July and 25 September, most tagged whales were located in shallow shelf waters adjacent to the Tuktoyaktuk Peninsula, Canada (Area 2), where wind-driven upwelling promotes the concentration of calanoid copepods. Between 22 August and 2 November, whales also congregated near Point Barrow, Alaska (Area 3), where east winds promote upwelling that moves zooplankton onto the Beaufort shelf, and subsequent relaxation of these winds promoted zooplankton aggregations. Between 27 October and 8 January, whales congregated along the northern shore of Chukotka, Russia (Area 4), where zooplankton likely concentrated along a coastal front between the southeastward-flowing Siberian Coastal Current and northward-flowing Bering Sea waters. The two remaining core-use areas occurred in the Bering Sea: Anadyr Strait (Area 5), where peak use occurred between 29 November and 20 April, and the Gulf of Anadyr (Area 6), where peak use occurred between 4 December and 1 April; both areas exhibited highly fractured sea ice. Whales near the Gulf of Anadyr spent almost half of their time at depths between 75 and 100 m, usually near the seafloor, where a subsurface front between cold Anadyr Water and warmer Bering Shelf Water presumably aggregates zooplankton. The amount of time whales spent near the seafloor in the Gulf of Anadyr, where copepods (in diapause) and, possibly, euphausiids are expected to aggregate provides strong evidence that bowhead whales are feeding in winter. The timing of bowhead spring migration corresponds with when zooplankton are expected to begin their spring ascent in April. The core-use areas we identified are also generally known from other studies to have high densities of whales and we are confident these areas represent the majority of important feeding areas during the study (2006–2012). Other feeding areas, that we did not detect, likely existed during the study and we expect core-use area boundaries to shift in response to changing hydrographic conditions.
    Description: This study is part of the Synthesis of Arctic Research (SOAR) and was funded in part by the U.S. Department of the Interior, Bureau of Ocean Energy Management, Environmental Studies Program through Interagency Agreement No. M11PG00034 with the U.S. Department of Commerce, National Oceanic and Atmospheric Administration (NOAA), Office of Oceanic and Atmospheric Research (OAR), Pacific Marine Environmental Laboratory (PMEL). Funding for this research was mainly provided by U.S. Minerals Management Service (now Bureau of Ocean Energy Management) under contracts M12PC00005, M10PS00192, and 01-05-CT39268, with the support and assistance from Charles Monnett and Jeffery Denton, and under Interagency Agreement No. M08PG20021 with NOAA-NMFS and Contract No. M10PC00085 with ADF&G. Work in Canada was also funded by the Fisheries Joint Management Committee, Ecosystem Research Initiative (DFO), and Panel for Energy Research and Development.
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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