Large‐scale instabilities of the Laurentide ice sheet simulated in a fully coupled climate‐system model

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A geophysically constrained large ensemble analysis of the deglacial history of the North American ice-sheet complex (2004, background): “However, a recent analysis employing a different ISM, linear tilldeformation law, equilibrium conditions, and much larger glacial ice volume (Calov et al., 2002) has been able to obtain extensive draw-downs over both regions of the order required by model nn2059.”
Glacial CO2 cycle as a succession of key physical and biogeochemical processes (2011, background): “The largest fluctuations of the freshwater flux are associated with the internal instability of the Laurentide ice sheet and the development of fast ice streams over the Hudson Strait (Calov et al., 2002).”
Simulation of the last glacial cycle with a coupled climate ice-sheet model of intermediate complexity (2009, unknown): “Calov et al. (2009) showed that the climate component can be considerably accelerated without significant loss of accuracy in simulation of the glacial inception.”
Transient simulation of the last glacial inception. Part I: glacial inception as a bifurcation in the climate system (2005, methodology): “Recently, we presented a simulation of Heinrich events using SICOPOLIS with the climatological boundary conditions simulated by the CLIMBER-2 model (Calov et al. 2002).”