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Modelling the northern hemisphere and Antarctic ice sheet changes through the last glacial cycle

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Figure

Figure 2.2: Variations in eccentricity, obliquity and precession index over the past 800,000 years according to calculations by Berger (1978)
Figure 2.3: Summer half year (-) and total (...) radiation anomalies relative to present (1950) due to variations in the Earth's orbital characteristics
Figure 2.4: (a) Radiation anomalies at 65°N, over the last 200 ka (data from Berger (1978,1979))
Table 2.1: Approximate albedos for various surfaces. The generally high albedo of ice and its capacity to appear and disappear relatively quickly from a surface allows ice to significantly affect climate
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