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Arktische Schmelze und Zukunft des Meereises

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Zusammenfassung

Die frühe arktische Erwärmung zwischen 1920 und 1945 wird mit intern generierter Variabilität in Verbindung gebracht und durch die CMIP-Modelle nicht reproduziert.

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Abbildungen

  • ERA-20C Data/Figures 8.1 and 8.2 from Climate Reanalyzer (https://ClimateReanalyzer.org), Climate Change Institute, University of Maine, USA.

  • NCEP/NCAR Reanalyses Data/Figure 8.3 from Climate Reanalyzer (https://ClimateReanalyzer.org), Climate Change Institute, University of Maine, USA.

  • ECMWF ERA5 Data/Figure 8.4 from Climate Reanalyzer (https://ClimateReanalyzer.org), Climate Change Institute, University of Maine, USA.

  • CCSM4 RCP8.5 Ensemble Avg Data/Figures 8.5, 8.6, 8.7, 8.8 from Climate Reanalyzer (https://ClimateReanalyzer.org), Climate Change Institute, University of Maine, USA.

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© 2022 Der/die Autor(en), exklusiv lizenziert durch Springer-Verlag GmbH, DE, ein Teil von Springer Nature

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Dethloff, K. (2022). Arktische Schmelze und Zukunft des Meereises. In: Unberechenbares Klima. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-64900-8_8

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