What caused the Ice Age to begin in the first place?

No single cause flipped the switch on an Ice Age; the main driver is a slow, predictable wobble in Earth's orbit and tilt that changes how much sunlight reaches the planet and where.

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The Milankovitch cycles

A Serbian mathematician named Milutin Milankovitch worked out in the early 20th century that Earth's path around the sun is not perfectly constant. Three things drift over long timescales:

  • Eccentricity: Earth's orbit stretches from nearly circular to slightly elliptical and back, over roughly 100,000 years.
  • Axial tilt: Earth tilts between about 22° and 24.5° relative to its orbital path, cycling over roughly 41,000 years. More tilt means stronger seasons.
  • Precession: Earth wobbles on its axis like a spinning top, over about 26,000 years, which shifts which hemisphere faces the sun at which time of year.

When these three cycles line up so that summers in the Northern Hemisphere become cooler, snow from the previous winter fails to melt completely. That leftover snow reflects sunlight back into space rather than absorbing it, cooling the climate further. That feedback loop, called the ice-albedo feedback, is where a nudge becomes a glacier. The cycle then locks in: more ice means more reflection, which means more cooling, which means more ice.

Why the Northern Hemisphere leads

The big continental landmasses where ice sheets can actually build up, North America, Europe and Asia, sit mostly in the Northern Hemisphere. There is nowhere in the Southern Hemisphere with enough land at the right latitudes for the same runaway buildup, which is why northern summer insolation (the amount of solar energy hitting that region) is the critical variable.

Other amplifiers

Orbital wobbles alone are not quite powerful enough to explain the full 5 to 8°C of global cooling seen in a full glacial period. Other feedbacks pile on once the cooling starts:

  • CO₂ drops: A cooler ocean absorbs more carbon dioxide, pulling it out of the atmosphere, which weakens the greenhouse effect and deepens the cold.
  • Vegetation shifts: Forests give way to tundra and ice, which are more reflective, reinforcing the cooling.
  • Ocean circulation changes: The same Atlantic Meridional Overturning Circulation that the earlier answer connected to the Younger Dryas also shifts heat distribution globally during glacial cycles.

The last Ice Age's glacial maximum, when ice sheets covered much of North America and Scandinavia, peaked roughly 20,000 years ago. The slow warming that followed, interrupted by cold snaps like the Younger Dryas, was driven by the orbital cycles swinging back the other way, with feedbacks running in reverse.

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This follows on from
What are the younger drayas?

The Younger Dryas was a rapid, severe cold snap that struck the Northern Hemisphere roughly 12,900 years ago and lasted about 1,200 years, interrupting what had been a warming trend at the end of the last Ice Age.

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