Abstract
Abstract Dansgaard–Oeschger events are warm events appearing and disappearing abruptly within the last glacial period. Several mechanisms have been put forward to explain these rapid climatic switches: forced oscillations of the atmosphere-ocean-ice-sheet system or instabilities of the ocean circulation, of the ice-sheets, or of the atmosphere-ocean-ice-sheet system. Here, this last hypothesis is examined through the use of the climate model of intermediate complexity CLIMBER2.3, coupled to a very simple ice-sheet model of the Fennoscandian ice-sheet. To cite this article: M. Kageyama, D. Paillard, C. R. Geoscience 337 (2005).
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
