Milankovitch Cycles: How Earth’s Orbital Wobbles Trigger Ice Ages

In 13,000 years Polaris will no longer mark true north, because Earth is not a perfectly spinning top. This episode unpacks the three orbital rhythms that Serbian geophysicist Milutin Milankovitch calculated by hand in the 1920s: eccentricity, the stretching of Earth’s orbit on roughly 100,000 and 400,000 year timescales that can change incoming solar radiation by up to 23 percent; obliquity, the axial tilt rocking between 22.1 and 24.5 degrees every 41,000 years; and precession, the 25,700 year wobble that decides which hemisphere faces the Sun at closest approach. Along the way the hosts explain why Northern Hemisphere winter is about four days shorter than summer thanks to Kepler’s second law.

The heart of the episode is Milankovitch’s counterintuitive trigger: not brutal winters but cool summers at 65 degrees north, where the continents sit, letting snow survive year after year and reflect sunlight in a runaway albedo feedback. The conversation then turns to the puzzles in the proxy record, including the mid-Pleistocene transition from 41,000 year to 100,000 year ice age cycles, competing explanations involving falling CO2, glacial removal of regolith and stochastic resonance, and a causality problem where warming appears to precede its orbital cause. The hosts finish with Mars tilting up to 70 degrees without a large moon, Titan’s migrating methane lakes, and why human greenhouse gas emissions are overriding the natural cooling phase Earth should be in.

  • Eccentricity, obliquity and precession explained with racetrack, rocking and spinning-top analogies
  • Why 65 degrees north latitude is the make-or-break line for global glaciation
  • The mid-Pleistocene transition and why the weakest orbital signal became the pacemaker
  • Ice cores, deep sea sediment and the 130,000 year timing anomaly
  • Mars, Titan and Triton as examples of orbital cycles without a stabilizing moon

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