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  • 1
    Online Resource
    Online Resource
    Berlin, Heidelberg :Springer Berlin / Heidelberg,
    Keywords: Climatic changes. ; Geology. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (376 pages)
    Edition: 1st ed.
    ISBN: 9783662606629
    DDC: 551.34
    Language: German
    Note: Intro -- Vorwort -- Danksagung -- Inhaltsverzeichnis -- 1 Einführung: Eine blaue Arktis -- Literatur -- 2 Eis, der magische Kristall -- 2.1 Die Kristallstruktur von Eis -- 2.2 Gefrieren und Schmelzen -- 2.3 Die Bildung von Eis im Meer -- 2.4 Die Bedeutung der Sommerschmelze -- 2.5 Wie im Eis Rinnen und Presseisrücken entstehen -- 2.6 Eis im flachen Wasser -- 2.7 Polynjas -- Literatur -- 3 Eine kurze Geschichte des Eises auf der Erde -- 3.1 Das erste Eis -- 3.2 Das Paradoxon der Schneeball-Erde -- 3.3 Zwei weitere Schneebälle -- 3.4 Der Übergang zu astronomisch verursachten Eiszeiten -- Literatur -- 4 Der moderne Zyklus der Eiszeiten -- 4.1 Das Pliozän und die Eiszeiten -- 4.2 Daten über die letzten Vergletscherungen -- 4.3 Der astronomische Einfluss auf die Eiszeiten -- 4.4 Das Archiv der Eiskerne -- 4.5 Wie die letzten Eiszeit endete -- 4.6 Wie lange noch bis zur nächsten Eiszeit? -- Literatur -- 5 Der Treibhauseffekt -- 5.1 Der natürliche Treibhauseffekt -- 5.2 Kohlendioxid, der Bösewicht unter den Molekülen -- 5.3 Methan und Lachgas -- 5.4 Ozon und FCKW -- 5.5 Strahlungsantrieb -- 5.6 Klimasensitivität -- 5.7 Die jüngste Temperaturgeschichte der Erde -- 5.8 Arktische Verstärkung -- Literatur -- 6 Das Meereis beginnt zu schmelzen -- 6.1 Meereis im 19. Jahrhundert -- 6.2 Wir treten in die Neuzeit ein -- 6.3 Der Eiskollaps der letzten zehn Jahre -- 6.4 Ein persönliches Zwischenspiel, 2007 -- 6.5 Der nächste Schritt abwärts für das Eis, 2012 -- 6.6 Die letzten Jahre des sommerlichen Eises -- 6.7 Wellen im offenen Wasser -- Literatur -- 7 Die Zukunft des arktischen Meereises - die Todesspirale -- 7.1 Wie geht es für das Meereis weiter? -- 7.2 Haben wir einen Kipppunkt überschritten? -- 7.3 Woher wissen wir, dass all das passieren wird? -- 7.4 Unmittelbare Folgen des Eisrückzugs - Navigation in der Arktis. , 7.5 Unmittelbare Folgen des Eisrückzugs - Öl und der Meeresboden -- 7.6 Das Problem der Ölverschmutzung und wie man damit umgeht -- 7.7 Wahrscheinlicher Verlauf eines weiteren Eisrückzugs in diesem Jahrhundert -- Literatur -- 8 Die Beschleunigung durch arktische Rückkopplungen -- 8.1 Das Konzept der klimatischen Rückkopplungen -- 8.2 Eis-Albedo-Rückkopplung -- 8.3 Rückkopplung durch Rückgang der Schneegrenze -- 8.4 Wasserdampfrückkopplung -- 8.5 Schmelzende Eisschilde und Meeresspiegelanstieg -- 8.6 Rückkopplung bei arktischen Flüssen -- 8.7 Rückkopplung durch Ruß -- 8.8 Rückkopplung bei der Ozeanversauerung -- 8.9 Welche Rückkopplungen sind am stärksten? -- Literatur -- 9 Arktisches Methan, eine Katastrophe kündigt sich an -- 9.1 Submariner Permafrost und warmes Wasser -- 9.2 Globale Auswirkungen der Methanfreisetzung in der Arktis -- 9.3 Sofort handeln! -- 9.4 Die Bedrohung durch tauenden Permafrost an Land -- 9.5 Das Gebiet weitet sich aus -- Literatur -- 10 Seltsames Wetter -- 10.1 Das Wetter und der Strahlstrom -- 10.2 Ist dieser Mechanismus real? -- 10.3 Wetterereignisse und Nahrungsproduktion -- 10.4 Das Problem des Wassers -- Literatur -- 11 Die geheimnisvollen Konvektionsschlote -- 11.1 Die globale thermohaline Zirkulation -- 11.2 Die Konvektion in der Grönlandsee -- 11.3 Das Geheimnis der Schlote -- 11.4 Die Zukunft im Kino -- 11.5 Die Zukunft -- Literatur -- 12 Was passiert in der Antarktis? -- 12.1 Die seltsame Geschichte des antarktischen Meereises -- 12.2 Warum das antarktische Eis anders ist -- 12.3 Schnee auf dem Eis -- 12.4 Der jährliche Eiszyklus und wie er sich ändert -- 12.5 Was passiert mit dem Eis? -- 12.6 Reaktion der Antarktis auf Veränderungen anderswo -- Literatur -- 13 Der Zustand der Erde -- 13.1 Was können wir tun? -- 13.1.1 Emissionsminderung -- 13.1.2 Geoengineering -- 13.1.3 Kohlenstoffabscheidung. , 13.2 Kann uns das Pariser Abkommen von 2015 retten? -- Literatur -- 14 Aufruf zum Kampf -- 14.1 Stärkung der Wissenschaft -- 14.2 Kriegsgefahr -- 14.3 Die Leugner des Klimawandels -- 14.4 Zeit zu kämpfen -- Literatur -- 15 Nachtrag zur deutschen Ausgabe -- 15.1 Internationale Organisationen -- 15.2 Methan im Arktischen Ozean -- 15.3 Der Meereisrückzug -- 15.4 Die nächste Eiszeit -- 15.5 Schifffahrtsrouten in der Arktis -- 15.6 Meeresspiegelanstieg -- 15.7 Absenkung der Kohlendioxidkonzentration -- 15.8 Abschließende Gedanken -- Anhang -- Stichwortverzeichnis.
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  • 2
    Online Resource
    Online Resource
    Dordrecht :Springer Netherlands,
    Keywords: Chemical oceanography-Arctic Ocean-Congresses. ; Salinity-Arctic Ocean-Congresses. ; Runoff-Arctic regions-Congresses. ; Electronic books.
    Description / Table of Contents: Proceedings of the NATO Advanced Research Workshop, Tallinn, Estonia, 27 April-1 May 1998.
    Type of Medium: Online Resource
    Pages: 1 online resource (630 pages)
    Edition: 1st ed.
    ISBN: 9789401141321
    Series Statement: NATO Science Partnership Subseries: 2 Series ; v.70
    DDC: 551.46/8
    Language: English
    Note: Intro -- TABLE OF CONTENTS -- PREFACE -- ACKNOWLEGDEMENTS -- INTRODUCTION.
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  • 3
    Online Resource
    Online Resource
    Boca Raton :Taylor & Francis Group,
    Keywords: Sea ice-Polar Regions. ; Icebergs. ; Climatic changes. ; Electronic books.
    Description / Table of Contents: Ice in the Ocean examines sea ice and icebergs and their role in the global climate system. It is comprehensive textbook suitable for students, pure and applied researchers, and anyone interested in the polar regions, the oceans, and climate. The author examines the distribution of sea ice, its mechanisms of growth, development and decay, the thermodynamics and dynamics of sea ice, sea ice deformation and ridge-building, the role of marginal ice zones, the characteristics of icebergs, and the part played by sea ice in the climate system and in the transport of pollutants. An extensive reference list, recommendations for further reading and numerous illustrations add to the value of the text.
    Type of Medium: Online Resource
    Pages: 1 online resource (366 pages)
    Edition: 1st ed.
    ISBN: 9781482283082
    DDC: 551.34/2
    Language: English
    Note: Cover -- Half Title -- Title Page -- Copyright Page -- Dedication -- Table of Contents -- PREFACE -- 1: THE FROZEN OCEANS -- 1.1. A world of white -- 1.2. The physical structure of the polar oceans -- 1.2.1. The topography -- 1.2.2. The water masses -- 1.2.3. The current systems -- 1.2.4. Water mass transformations -- 1.3. The distribution of ice in the oceans -- 1.3.1. The Arctic -- 1.3.2. The Antarctic -- 1.3.3. Icebergs -- 1.4. Mapping the frozen oceans -- 1.5. Sea ice and the history of exploration -- 2: FORMATION, GROWTH AND DECAY OF SEA ICE -- 2.1. The structure of the ice crystal -- 2.2. The density and freezing point of sea water -- 2.3. The initial stages of ice formation -- 2.3.1. Ice formation in calm water -- 2.3.2. Ice formation in rough water: The frazil-pancake cycle -- 2.4. Crystal growth and brine rejection -- 2.4.1. Crystal fabric -- 2.4.2. Brine cells -- 2.4.3. Brine cell migration and drainage -- 2.4.4. Solid salts in ice -- 2.4.5. Lake and river ice -- 2.5. Snow loading and meteoric ice formation -- 2.6. Summer melt processes -- 2.7. Multi-year ice -- 2.8. Formation of leads and pressure ridges -- 2.9. Ice in shallow water -- 2.9.1. Grounded landfast ice -- 2.9.2. Ice scour -- 2.10. Polynyas and their role -- 3: THE THERMODYNAMICS OF SEA ICE -- 3.1. Thermophysical properties of sea ice -- 3.1.1. Thermal conductivity -- 3.1.2. Specific heat -- 3.1.3. Latent heat of fusion -- 3.1.4. Radiation extinction coefficient -- 3.2. Early models of ice growth and decay -- 3.3. The Maykut-Untersteiner model -- 3.3.1. Formulation -- 3.3.2. Input parameters -- 3.3.3. Results -- 4: ICE IN MOTION -- 4.1. The momentum balance -- 4.1.1. Air stress -- 4.1.2. Water stress -- 4.1.3. Coriolis force -- 4.1.4. Internal ice stress -- 4.1.5. Sea surface tilt -- 4.2. A free drift solution -- 4.2.1. Inertial motion. , 4.2.2. Free drift in response to geostrophic wind -- 4.3. The motion of compact ice -- 4.3.1. Ice rheology -- 4.3.2. Sea ice models -- 4.4. Dynamics and thermodynamics of coastal polynyas -- 4.5. Tidal ice motion -- 4.5.1. Tidal amplitudes and currents -- 4.5.2. Effect of sea ice on tides -- 4.5.3. Effect of tides on sea ice -- 5: PRESSURE RIDGES AND THE ICE THICKNESS DISTRIBUTION -- 5.1. Statistical properties of a sea ice cover -- 5.1.1. Importance of the ice thickness distribution -- 5.1.2. Ice thickness distribution - Definitions -- 5.1.3. Ice thickness distribution - Typical shapes -- 5.1.4. The distribution of morphological features -- 5.1.5. Pressure ridge depths -- 5.1.6. Pressure ridge spacings -- 5.1.7. Pressure ridge slopes and widths -- 5.1.8. Lead widths and spacings -- 5.1.9. Fractal properties of ice surfaces -- 5.1.10. Summary -- 5.2. The measurement of ice thickness -- 5.2.1. Current techniques -- 5.2.2. Possible future techniques -- 5.3. Present knowledge of ice thickness distribution -- 5.3.1. Mean ice thickness in the Arctic -- 5.3.2. Mean ice thickness in the Antarctic -- 5.3.3. The differences between Arctic and Antarctic sea ice -- 5.4. Applications of the ice thickness distribution -- 5.4.1. Sound propagation -- 5.4.2. Microwave signatures -- 5.4.3. Stimulation of internal waves by ice keels -- 5.4.4. The under-ice drag coefficient -- 5.4.5. Differential melt rates -- 5.4.6. Ice scour rates and pipeline burial depths -- 6: THE MARGINAL ICE ZONE -- 6.1. The structure of the ice margin -- 6.2. Marginal ice zones of the world -- 6.2.1. Greenland Sea -- 6.2.2. Labrador Sea -- 6.2.3. Bering Sea -- 6.2.4. Antarctic Ocean -- 6.3. Wave-ice interaction and the floe size distribution -- 6.3.1. A review of observations -- 6.3.2. Models of wave attenuation -- 6.3.3. Wave decay and floe break-up -- 6.4. Ice edge bands. , 6.5. Eddies and meanders -- 6.5.1. Some eddy observations -- 6.5.2. Generating mechanisms -- 6.6. Ambient noise at the ice edge -- 6.7. The Odden ice tongue and Greenland Sea convection -- 7: ICEBERGS -- 7.1. Mode of formation -- 7.2. Physical characteristics -- 7.2.1. Sizes -- 7.2.2. Shapes -- 7.2.3. Geographical distribution -- 7.3. Glaciological properties -- 7.4. Iceberg dynamics and drift -- 7.4.1. Iceberg motion -- 7.4.2. Patterns of iceberg drift -- 7.5. Decay mechanisms -- 7.5.1. Erosion and melt -- 7.5.2. Breakup by flexure -- 7.6. Iceberg scour -- 7.7. Climatic role of icebergs -- 7.8. Icebergs as a fresh water source -- 8: SEA ICE, CLIMATE AND THE ENVIRONMENT -- 8.1. Sea ice and biology -- 8.2. Sea ice and environmental threats -- 8.2.1. Oil spills and blowouts -- 8.2.2. The transport of pollutants by sea ice -- 8.3. Sea ice and climate -- 8.3.1. Climate change and the polar regions -- 8.3.2. Climate change and sea ice extent -- 8.3.3. Climate change and fast ice thickness -- 8.3.4. Climate change and moving pack ice thickness -- 8.3.5. Recent changes in the Arctic Ocean -- 8.4. The future course of research on sea ice -- FURTHER READING -- REFERENCES -- INDEX.
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  • 4
    Keywords: Aufsatzsammlung ; Grönlandsee ; Meereskunde
    Type of Medium: Book
    Pages: IV S., S. 1011 - 1530 , Ill., graph. Darst., Kt
    Series Statement: Deep-sea research 46.1999,6/7
    Language: English
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  • 5
    Book
    Book
    Australia [u.a.] : Gordon and Breach Science Publishers
    Keywords: Sea ice ; Icebergs ; Climatic changes ; Sea ice ; Icebergs ; Polar regions ; Climatic changes ; Polargebiete ; Meereis ; Eisberg ; Klima ; Ökologie
    Type of Medium: Book
    Pages: XI, 351 S , Ill., graph. Darst., Kt
    ISBN: 9056992961
    DDC: 551.342
    Language: English
    Note: refs., index , Includes bibliographical references (p. 305-334) and index
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  • 6
    Type of Medium: Book
    Pages: 2 Bd
    Language: Undetermined
    Note: MAST-II Programme ; Contract MAS2-CT93-0057
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  • 7
    ISSN: 1751-8369
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geography , Geosciences
    Notes: In previous work, whaling catch positions were used as a proxy record for the position of the Antarctic sea ice edge and mean sea ice extent greater than the present one spanning 2.8° latitude was postulated to have occurred in the pre-1950s period, compared to extents observed since 1973 from microwave satellite imagery. The previous conclusion of an extended northern latitude for ice extent in the earlier epoch applied only to the January (mid-summer) period. For this summer period, however, there are also possible differences between ship and satellite-derived measurements. Our work showed a consistent summer offset (November-December), with the ship-observed ice edge 1 - 1.5° north of the satellite-derived ice edge. We further reexamine the use of whale catch as an ice edge proxy where agreement was claimed between the satellite ice edge (1973-1987) and the ship whale catch positions. This examination shows that, while there may be a linear correlation between ice edge position and whale catch data, the slope of the line deviates from unity and the ice edge is also further north in the whale catch data than in the satellite data for most latitudes. We compare the historical (direct) record and modern satellite maps of ice edge position accounting for these differences in ship and satellite observations. This comparison shows that only regional perturbations took place earlier, without significant deviations in the mean ice extents, from the pre-1950s to the post-1970s. This conclusion contradicts that previously stated from the analysis of whale catch data that indicated Antarctic sea ice extent changes were circumpolar rather than regional in nature between the two periods.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 305 (1983), S. 108-111 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] HM nuclear submarine Sovereign has obtained the first synoptic measurements of the ice thickness distribution in Fram Strait, the main outflow from the Arctic Ocean. The ice nearest the ice edge is of quite different character from ice in the interior of the Strait, with a greater proportion of ...
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 333 (1988), S. 161-164 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] A single previous instance of under-ice imaging was an attempt to obtain sidescan sonar imagery from HMS Sovereign in 19768'9, when a limited dataset was obtained from one channel of a sidescan transducer over a distance of 40 km before the transducer flooded. In May 1987 HMS Superb carried out an ...
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 345 (1990), S. 795-797 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Type of Medium: Electronic Resource
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