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