Orbital changes affect the amount of sunlight on the Earth's surface and where it falls. On a timescale of thousands of years, the changes could start an ice age or stop one. The cycles are called Milankovitch cycles.
3 ways the Earth's orbit change:
- The Earth's orbit is sometimes circular, sometimes oval
- The Earth's axis tilts, sometimes it is upright, sometimes it's side
- The Earth's axis wobbles like a spinning top about to fall over
These cause cold periods 5-6 degrees colder than today and warm periods 2-3 degrees warmer than today.
It takes 100,000 years for the orbit to change from circular to oval and back
It takes 41,000 years for the axis to tilt, straighten and back
It takes 26,000 years for the axis to wobble, straighten and wobble again.
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