Q1845Milankovitch cycles—changes in orbital shape, axial tilt and wobble—alter the seasonal and geographic distribution of sunlight and help pace long-term glacial cycles.
Eccentricity, obliquity and precession unfold over tens to hundreds of thousands of years. Their importance lies less in changing total sunlight than in redistributing it by latitude and season, especially affecting whether northern snow survives summer. They explain ancient climate pacing; they do not explain the rapid modern warming driven by greenhouse gases.



