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    Schlagwort(e): Geographic information systems. ; Climatology. ; Water. ; Hydrology. ; Geology. ; Thermodynamics. ; Geographical Information System. ; Climate Sciences. ; Water. ; Geology. ; Thermodynamics.
    Beschreibung / Inhaltsverzeichnis: Chapter 1. Introduction -- Chapter 2. Sea Ice in the Arctic Paleoenvironments -- Chapter 3. Marginal Ice Zone and Ice-Air-Ocean Interactions -- Chapter 4. Changes in Arctic Sea Ice Cover in the Twentieth and Twenty-First Centuries -- Chapter 5. Arctic Sea Ice Thickness and Volume Transformation -- Chapter 6. SAR Sea Ice Type Classification and Drift Retrieval in the Arctic -- Chapter 7. Sea Ice Drift in the Arctic -- Chapter 8. Sea Ice Modelling -- Chapter 9. Operational Forecasting of Sea Ice in the Arctic Using TOPAZ System -- Chapter 10. Current and Projected Sea Ice in the Arctic in the Twenty-First Century -- Chapter 11. Climate Change Impact on the Arctic Economy -- Chapter 12. Annex: SAR Sea Ice Interpretation Guide.
    Kurzfassung: This book provides in-depth information about the sea ice in the Arctic at scales from paleoenvironmental variability to more contemporary changes during the past and present centuries. The book is based on several decades of research related to sea ice in the Arctic and its variability, sea ice process studies as well as implications of the sea ice variability on human activities. The chapters provide an extensive overview of the research results related to sea ice in the Arctic at paleo-scales to more resent scales of variations as well as projections for changes during the 21st century. The authors have pioneered the satellite remote sensing monitoring of sea ice and used other monitoring data in order to study, monitor and model sea ice and its processes.
    Materialart: Online-Ressource
    Seiten: X, 575 p. 246 illus., 154 illus. in color. , online resource.
    Ausgabe: 1st ed. 2020.
    ISBN: 9783030213015
    Serie: Springer Polar Sciences,
    DDC: 910.285
    Sprache: Englisch
    Standort Signatur Erwartet Verfügbarkeit
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