Transitivity of the climate–vegetation system in a warm climate

To date, the transitivity of the global system has been analysed for late Quaternary (glacial, interglacial, and present-day) climate. Here, we extend this analysis to a warm, almost ice-free climate with a different configuration of continents. We use the Earth system model of the Max Planck Instit...

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Bibliographic Details
Main Authors: U. Port, M. Claussen
Format: Article
Language:English
Published: Copernicus Publications 2015-11-01
Series:Climate of the Past
Online Access:http://www.clim-past.net/11/1563/2015/cp-11-1563-2015.pdf