HIGHLIGHTS
SUMMARY
The authors focus on the variations of the carbon_dioxide concentration,, and the reconstructed temperature T, during glacial-interglacial oscillations. Assuming a sufficient time-scale separation between the astronomical forcing (with a typical time of the order of 20 kyr or more) and the internal climate variability on millennial or shorter time scales, the authors delineate a qualitative analysis of the causation relations between | Vol:(1234567890) 12:15320 | In the "Methods" section, the authors show that both the above difficulties can be circumvented as long as there is a sufficient scale separation between the (slow . . .
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