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Ganopolski, A. & Rahmstorf, S. Rapid changes of glacial climate simulated in a coupled climate model.
One-to-one coupling of glacial climate variability in Greenland and Antarctica.
Zhang, X., Lohmann, G., Knorr, G. & Purcell, C. Abrupt glacial climate shifts controlled by ice sheet changes.
Arkoses were, therefore, presumed to be derived from the erosion of a granitic terrane characterized by an arid or glacial climate.
The harsh glacial climate appears to have been milder at Cava Muracci than at Tana delle Iene.
Peltier, W. R. & Vettoretti, G. Dansgaard-Oeschger oscillations predicted in a comprehensive model of glacial climate: a 'kicked' salt oscillator in the Atlantic.
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Bond, G. et al. A pervasive millennial-scale cycle in North Atlantic Holocene and glacial climates.
Adkins, J. F. The role of deep ocean circulation in setting glacial climates.
The data obtained made possible reconstructions of the Late Glacial climates and landscapes.
Glacial climates developed and dissipated at least twice, and each time excessive snows built snow and ice fields and deep glaciers.
This suggests that during glacial climates the stabilizing effect of vegetation determines eolian sedimentation rates, rather than wind speed.
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