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Verstärkung der Klimaänderung im Holozän durch die Wechselwirkung zwischen Atmosphäre, Vegetation und Ozean: Dargestellt sind Temperatur- und Niederschlagsdifferenzen zwischen dem voll gekoppelten Modell und einer Simulation mit konstanter Vegetation
Verstärkung der Klimaänderung im Holozän durch die Wechselwirkung zwischen Atmosphäre, Vegetation und Ozean: Dargestellt sind Temperatur- und Niederschlagsdifferenzen zwischen dem voll gekoppelten Modell und einer Simulation mit konstanter Vegetation

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