Transient simulation of the last glacial inception. Part I: glacial inception as a bifurcation in the climate system

By R. Calov, A. Ganopolski, M. Claussen, V. Petoukhov, Ralf Greve. 2005

156 citations recorded by the source corpus.

Subfields: Atmospheric Science, Environmental Chemistry

View Paper: https://www.semanticscholar.org/paper/5136b944ab28182b4e9d856f2f7587a7bf42d19d

How researchers see this paper

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In Atmospheric Science

1. R. Calov
2. A. Ganopolski
3. Stefan Rahmstorf

In Environmental Chemistry

1. R. Calov
2. A. Ganopolski
3. Stefan Rahmstorf

Citations in the corpus

• Simulation of the last glacial cycle with a coupled climate ice-sheet model of intermediate complexity (2009, unknown): “In particular, several EMICs simulate the most recent glacial inception (around 120–115 kyr BP) with reasonable agreement with palaeodata, at least, in respect of the total ice volume (Wang and Mysak, 2002; Calov et al. 2005).”
• The role of orbital forcing, carbon dioxide and regolith in 100 kyr glacial cycles (2011, methodology): “The ice sheet model is only applied to the Northern Hemisphere and is coupled to the climate component via a high-resolution, physically-based surface energy and mass balance interface (Calov et al., 2005), which explicitly accounts for the effect of aeolian dust deposition on snow albedo.”