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ID: 3344.0, PIK / PIK Publications , full text not public
Kubatzki, C.; Claussen, M.; Calov, R.; Ganopolski, A.
Modelling the end of an interglacial (MIS 1, 5, 7, 9, 11)
In: The climate of past interglacials, Developments in quaternary science
Ed.: Sirocko, F.; Claussen, M.; Sanchez-Goi, M. F.; Litt, T.
Amsterdam : Elsevier
2007. 583-593 p.
Doctype: Article in book
Departments: Climate System
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ID: 3261.0, PIK / PIK Publications , full text not public
Claussen, M.; Berger, A.; Held, H.
A survey of hypotheses for the 100 ka cycle
In: The climate of past interglacials. Developments in quaternary science
Ed.: Sirocko, F.; Claussen, M.; Snchez Goi, M.; Litt, T.
Elsevier Publisher
2006. 29-35 p.
7
Doctype: Article in book
Departments: Integrated Systems Analysis
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ID: 2177.0, PIK / PIK Publications , full text not public
Rahmstorf, S.; Sirocko, F.
Modes of oceanic and atmospheric circulation during the quaternary
In: Earth system analysis for sustainability
Cambridge Massachusetts, London, UK : MIT Press
2004. 157-170 p.
Doctype: Article in book
Departments: Climate System
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ID: 2314.0, PIK / PIK Publications , full text not public
Sirocko, F.; Cubasch, U.; Kaspar, F.; von Storch, H.; Widmann, M.; Litt, T.; Khl, N.; Mangini, A.; Pachur, H.-J.; Claussen, M.; Kubatzki, C.; Junge, F. W.; Bttger, T.; Krbetschek, M.; Degering, D.
Climate change at the very end of a warm stage: First results from the last glacial inception at 117,000 yr BP
In: PAGES News, 12 , 2
2004. 18-23 p.
Doctype: Article (other journals)
Departments: Climate System
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ID: 2126.0, PIK / PIK Publications
Watson, A.; Brovkin, V.; Claussen, M.; Falkowski, P.; Held, H.; Payne, A.J.; Rahmstorf, S.; Scholes, R.J.; Schrag, D.P.; Sirocko, F.
Group Report: Possible states and modes of operation of the quaternary earth system
In: Earth system analysis for sustainability. Dahlem workshop report
Ed.: Schellnhuber, H.J.; Clark, W.C.; Crutzen, P.J.; Claussen, M.
Cambridge Massachusetts, London, UK : MIT Press
2004. 189-210 p.
Doctype: Article in book
Departments: Climate System
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