Climate of the Past Discussions www.clim-past-discuss.net 1814-9340 1814-9359 5 1 2009 10.5194/cpd-5-595-2009 http://www.clim-past-discuss.net/5/595/2009/ http://www.clim-past-discuss.net/5/595/2009/cpd-5-595-2009.html http://www.clim-past-discuss.net/5/595/2009/cpd-5-595-2009.pdf 595 633 2009-02-24 Mechanisms and time scales of glacial inception simulated with an Earth system model of intermediate complexity R. Calov calov@pik-potsdam.de A. Ganopolski C. Kubatzki M. Claussen Potsdam Institute for Climate Impact Research, Potsdam, Germany Max Planck Institute for Meteorology, Hamburg, Germany KlimaCampus University Hamburg, Hamburg, Germany We investigate glacial inception and glacial thresholds in the climate-cryosphere system utilising the Earth system model of intermediate complexity CLIMBER-2, which includes modules for atmosphere, terrestrial vegetation, ocean and interactive ice sheets. The latter are described by the three-dimensional polythermal ice-sheet model SICOPOLIS. A bifurcation which represents glacial inception is analysed with two different model setups: one setup with dynamical ice-sheet model and another setup without it. The respective glacial thresholds differ in terms of maximum boreal summer insolation at 65° N (hereafter referred as Milankovich forcing (MF)). The glacial threshold of the configuration without ice-sheet dynamics corresponds to a much lower value of the MF compared to the full model. If MF attains values only slightly below the aforementioned threshold there is fast transient response. Depending on the value of MF relative to the glacial threshold, the transient response time of inland-ice volume in the model configuration with ice-sheet dynamics ranges from 10 000 to 100 000 years. We investigate implications of these time scales for past glacial inceptions and for the overdue Holocene glaciation hypothesis by Ruddiman (W. F. Ruddiman, Climatic Change 2003, Vol. 61, 261–293). 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