Permafrost as a critical factor in palaeoclimate modelling: the Younger Dryas case in Europe.

H. Renssen, R.F.B. Isarin, J. Vandenberghe, M. Lautenschlager, U. Schlese

    Research output: Contribution to JournalArticleAcademicpeer-review

    Abstract

    Simulations with an atmospheric climate model of the Younger Dryas climate, a distinct cooling event around 12 kyr cal B.P., were compared with temperature reconstructions based on fossil plant data. In one experiment we forced the model to maintain a wet and frozen soil at high latitudes to reproduce the effect of permafrost in the model. This measure resulted in a climate similar to the reconstructions with a depression of the summer temperatures in Eurasia by 4-8°C and an increase in precipitation. This suggests that permafrost may have played a more important role in driving paleoclimates (such as the Younger Dryas climate) than believed until now. This calls for re-evaluation of (paleo)climate simulations in which permafrost was not explicitly included. (C) 2000 Elsevier Science B.V. All rights reserved.
    Original languageEnglish
    Pages (from-to)1-5
    JournalEarth and Planetary Science Letters
    Volume176
    DOIs
    Publication statusPublished - 2000

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