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  • 1
    Keywords: Oceanography-Arctic Ocean. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (538 pages)
    Edition: 1st ed.
    ISBN: 9780128169315
    DDC: 551.46
    Language: English
    Note: Front Cover -- The Physical Oceanography of the Arctic Mediterranean Sea -- Copyright Page -- Dedication -- Contents -- Preface -- Acknowledgment -- 1 From Nifelheim to Fram -- 1.1 In the Northern mist -- 1.2 The search for the Northeast and Northwest passages -- 1.3 A century of exploration -- 1.4 The circulation of the world ocean -- 1.5 The influence of warm ocean currents on the ice cover -- 1.6 The Fram expedition -- References -- 2 The Arctic environment -- 2.1 The global radiation balance and the high latitude climate -- 2.2 The atmospheric meridional energy transport -- 2.3 High-latitude atmospheric circulation patterns -- 2.4 The energy balance of the polar cap -- 2.5 Extent and major regions of the Arctic Mediterranean Sea -- 2.6 The surface currents, inflows, and outflows -- 2.7 The meridional freshwater transports and the sea ice cover -- References -- 3 Observing the Arctic Mediterranean Sea -- 3.1 In open water and at the ice edge (1900-40) -- 3.1.1 The Nordic Seas and the Barents Sea -- 3.1.2 Theoretical and technical advances -- 3.1.3 South and west of Greenland -- Baffin Bay, Davis Strait, and the Labrador Sea -- 3.1.4 Bering Strait -- 3.1.5 The Arctic Ocean boundaries, openings and shelves -- 3.2 Onto the ice and into the interior Arctic Ocean (1930-80) -- 3.2.1 Ice stations and ice islands -- 3.2.2 Airborne expeditions -- 3.3 Water mass distributions and the first interpretations and syntheses of the circulation in the Arctic Mediterranean -- 3.3.1 The Arctic Ocean -- 3.3.2 The connections between the Arctic Ocean and the Nordic Seas -- 3.3.3 Budgets -- 3.3.4 Overflows and the connections between the Arctic Mediterranean and the North Atlantic -- 3.3.5 The subpolar gyre and the North Atlantic -- 3.4 The development in observation, navigation, and communication techniques -- 3.5 Through, beneath, and above the ice (1980-2020). , 3.5.1 The first scientific icebreaker and submarine expeditions -- 3.6 The Nordic Seas, the overflows, and the North Atlantic -- 3.7 Variability and change -- 3.7.1 The Arctic Ocean -- 3.7.2 The Greenland Sea -- 3.7.3 The Labrador Sea -- 3.7.4 The subpolar gyre and the overflows -- 3.8 The beginning of large international projects, culminating in the fourth Polar Year and beyond -- References -- 4 External forcing and local response -- 4.1 Sea ice -- reflector and insulator -- 4.2 Sea ice thermodynamics, freezing, and melting -- 4.3 Sea ice growth during winter -- 4.4 The mechanics and dynamics of sea ice -- 4.5 Leads and polynyas -- 4.6 Haline convection and water mass transformations -- 4.7 The spreading of brine-enriched water on shelves and down slopes -- 4.8 Sea ice melting from below, sensible heat polynyas -- 4.9 Open ocean deep convection -- 4.10 Ice formation and deep ocean convection, the Weddell Sea and the Greenland Sea -- 4.10.1 The Weddell polynya -- 4.10.2 The Greenland Sea -- References -- 5 The circulation and transformations of Atlantic water in the Arctic Mediterranean Sea -- 5.1 The North Atlantic -- 5.2 Atlantic water in the Norwegian Sea and north of Svalbard -- 5.3 Atlantic water in the Barents Sea -- 5.4 The waters leaving the Barents Sea -- 5.5 Interactions in the Nansen Basin East of the St Anna Trough -- 5.6 The circulation and water masses in the Eurasian Basin -- 5.7 The Amerasian Basin and the interactions between Pacific and Atlantic waters -- 5.8 The variability and circulation of the Atlantic water -- 5.9 The deep and bottom waters -- 5.10 The outflow areas -- 5.11 East Greenland Current and the outflow through Fram Strait -- 5.12 The Greenland slope and the Greenland Sea -- 5.13 The Iceland Sea and the overflows -- 5.14 The Irminger Sea -- 5.15 The Labrador Sea -- References. , 6 The presence and importance of internal mixing processes in the Arctic Ocean -- 6.1 Diffusive interfaces and staircases in the Arctic Ocean -- 6.1.1 Laboratory and theoretical studies of diffusive interfaces -- 6.1.2 Diffusive staircases in the Arctic Ocean -- 6.2 Double-diffusive intrusions and interleaving -- 6.2.1 Early theoretical studies of interleaving at wide fronts -- 6.2.2 Laboratory experiments with narrow fronts -- 6.2.3 Intrusions and interleaving in the Arctic Ocean -- 6.2.4 A conceptual approach to estimate the intrusion thickness at a narrow front -- 6.2.5 The transports across the interfaces and the spreading of the intrusions -- 6.3 Connections between thermohaline intrusions, staircases, and eddies -- 6.4 The relation of thermohaline intrusions and staircases to other mixing processes -- References -- 7 Observed, computed, and deduced transports through the main gateways -- 7.1 From early point measurements to coordinated monitoring -- 7.2 The northward flow across the Iceland-Scotland Ridge -- 7.3 The Barents Sea inflow -- 7.4 Fram Strait: inflow, recirculation, and outflow -- 7.5 The transports in the East Greenland Current -- 7.5.1 Yearlong current measurements north of Denmark Strait -- 7.5.2 Denmark Strait overflow -- 7.5.3 The overflow through the Faroe Bank Channel -- 7.6 The inflow through Bering Strait -- 7.7 The outflows west of Greenland, the Canadian Arctic Archipelago and Baffin Bay -- 7.7.1 Cardigan Strait and Hell Gate -- 7.7.2 Barrow Strait -- 7.7.3 Nares Strait -- 7.7.4 The exchanges through Davis Strait -- 7.7.5 The Canadian Arctic Archipelago-Baffin Bay system -- 7.8 Other openings -- 7.8.1 The Iceland-Faroe Ridge overflow -- 7.8.2 Wyville Thomson Ridge overflow -- 7.8.3 Denmark Strait upper water outflow -- 7.8.4 Atlantic inflow over the European shelf -- 7.9 The mass balance of the Arctic Mediterranean Sea. , 7.10 Volume, heat, and freshwater balances of the Arctic Ocean -- 7.11 Heat and freshwater transports into and out of the Arctic Ocean -- 7.11.1 Mass conservations and heat and freshwater transports -- 7.11.2 Heat and freshwater fluxes through individual Straits -- 7.12 Freshwater transports and storage in the Arctic Ocean -- 7.12.1 A theoretical estimate of the freshwater storage in the Arctic Ocean -- 7.12.2 Observations of freshwater storage and transports in the Arctic Ocean -- 7.13 A double estuary -- 7.14 The circulation in temperature space, salinity space, and TS space -- References -- 8 Theoretical descriptions and modeling of the Arctic Mediterranean Sea -- 8.1 Conceptual models of the circulation in marginal seas -- 8.1.1 Wind-driven circulation in the Arctic Mediterranean Sea -- 8.1.2 Thermally driven circulation in marginal seas with sloping bottom -- 8.1.3 Outflow of dense water over a shallow sill -- 8.2 Numerical modeling of the circulation in the Arctic Mediterranean Sea -- 8.2.1 The inflow of Atlantic water to the Arctic Ocean -- 8.2.2 Circulation in the central Arctic Ocean -- 8.2.3 The outflow from the Arctic Mediterranean to the North Atlantic -- References -- 9 Variability and change -- 9.1 The Arctic Ocean sea ice cover -- 9.2 Ocean advection and sea ice-ocean interaction -- 9.2.1 Variations in the Atlantic inflow -- 9.2.2 Conditions in the Barents Sea -- 9.2.3 The Eurasian Basin -- 9.2.4 The Amerasian Basin -- 9.3 Changes in freshwater storage -- 9.3.1 Freshwater inputs and exports -- 9.3.2 The freshwater storage -- 9.3.3 The effects on the deep water formation -- 9.3.4 Freshwater pathways in the Arctic Ocean -- 9.4 The Nordic Seas, the overflows, and the subpolar gyre -- 9.4.1 The Nordic Seas -- 9.4.2 The overflows and the subpolar gyre -- 9.5 The circulation in the Arctic Mediterranean during the ice ages -- References. , 10 The meridional overturning circulation and the impact of the Arctic Mediterranean on the world ocean -- 10.1 The thermodynamics of the overturning circulation -- 10.2 The global deep circulation -- 10.3 The mixing and upwelling of the deep and abyssal waters -- 10.4 The upper layer return flow to the North Atlantic -- 10.5 The North Atlantic subtropical gyre and the Northeastern North Atlantic -- 10.6 The combined effects of cooling and freshening: insights from box models -- 10.7 Extensions of conceptual and box models -- 10.8 The stability of the overturning circulation -- 10.9 Forcing exchanges between the ocean and semienclosed seas by density differences or by wind? -- 10.10 General principles and geographical details -- References -- Index -- Back Cover.
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  • 2
    Book
    Book
    Göteborg : Department of Oceanography
    Type of Medium: Book
    Pages: 17 Bl
    Series Statement: Report / Oceanografiska Institutionen 42
    Language: English
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  • 3
    Book
    Book
    Bergen : Univ. of Bergen
    Type of Medium: Book
    Pages: 20 Bl. , graph. Darst. , 4°
    Series Statement: Report / Geophysical Institute 53
    Language: English
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  • 4
    Type of Medium: Book
    Series Statement: Technical report / Institut für Meereskunde Hamburg 90,4
    Language: Undetermined
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  • 5
    Type of Medium: Book
    Pages: 56 S , graph. Darst
    ISBN: 9515320828
    Series Statement: Meri 39
    Language: English
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  • 6
    Keywords: Oceanography ; Climatic changes ; Climatic changes ; Oceanography ; Arctic Ocean ; Arctic Ocean ; Nordpolarmeer ; Meereskunde
    Type of Medium: Book
    Pages: xv, 520 Seiten , Illustrationen, Karten, Diagramme , 24 cm
    ISBN: 9780128169308 , 0128169303
    DDC: 551.46
    RVK:
    Language: English
    Note: Literaturangaben
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  • 7
    Book
    Book
    Hamburg : Institut für Meereskunde
    Type of Medium: Book
    Pages: 8 S , Kt
    Series Statement: Technical report / Institut für Meereskunde im Zentrum für Meeres- und Klimaforschung der Universität Hamburg 94,2
    Language: German
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  • 8
    Book
    Book
    Göteborg : Göteborgs Univ., Oceanografiska Institutionen
    Type of Medium: Book
    Pages: 17 Bl
    Series Statement: Report / Oceanografiska Institutionen 34
    Language: English
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  • 9
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Polar research 4 (1986), S. 0 
    ISSN: 1751-8369
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geography , Geosciences
    Notes: The transports of mass, heat, and salt through the Arctic Archipelago are estimated by two different approaches. First: A baroclinic, rotationally controlled flow is assumed through the Arctic Archipelago and the Davis Strait, with all passages transporting at maximum capacity. Second: Mass, salt, and energy balances are considered for the upper ‘cold core’ in Baffin Bay. The mass transport in the first case decreases and in the second case increases with increasing salinity in the Beaufort Sea. It is thus possible to determine a salinity at which both approaches give the same mass transport. The outflow in the upper layers is estimated at 0.7 · 109 kg s−1 with a salinity of 32.9. The amount of water from the Polar Ocean entering the deeper (Atlantic) layer in Baffin Bay is more difficult to assess. A tentative value of 0.3 10·kg s−1 with a salinity cf 34.3 is proposed.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Polar research 1 (1983), S. 0 
    ISSN: 1751-8369
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geography , Geosciences
    Notes: The hydrographic (CTD) observations and pendulum current measurements obtained with M/S ‘Lance’ in August 1981 in the area west and north of Spitsbergen, are presented. The warm and saline northward flow, known as the West Spitsbergen Current, is found to follow the shelf break. In the Fram Strait the hydrographic structure is complicated because of eddies and other transient movements. The current measurements suggest a two-layer structure where the velocity vector rotates in opposite directions in the two layers with a period near the semidiurnal tidal period.
    Type of Medium: Electronic Resource
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