A linear feedforward model driven by orbital eccentricity reproduces 800,000 years of glacial-interglacial cycles and accounts for the absence of the 400,000-year eccentricity period via oceanic and tropospheric phase lags.
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A First Principles Approach to the 100,000-year Problem
A linear feedforward model driven by orbital eccentricity reproduces 800,000 years of glacial-interglacial cycles and accounts for the absence of the 400,000-year eccentricity period via oceanic and tropospheric phase lags.