F5-4 Earth's Wobble
Precession is the wobbling of the Earth’s axis of rotation.

The Earth’s axis of rotation wobbles slowly and periodically over time in a process known as precession. Precession is the third orbital parameter that Milankovitch claimed would affect insolation values for the Earth.

Precession would affect climate because a change in the direction of the Earth’s axis of rotation would result in changes in the location and duration of the seasons. The northern hemisphere experiences winter when the Earth’s axis points away from the sun, and summer when the Earth’s axis points toward the sun (the seasons are reversed in the southern hemisphere). Currently, winter in the northern hemisphere occurs roughly during the months of December, January, and February. As a result of precession, however, this situation will have reversed itself in approximately 13,000 years. Winter will instead occur in June, July, and August because this is when the Earth’s axis will be pointing away from the sun. The Earth will also be at its most distant point from the sun in its orbit during these months. Together these two factors would result in more extreme winters and a gradual build-up of snow and ice over time.

How precession will affect the seasons.

The three orbital cycles that Milankovitch identified (eccentricity, obliquity, and precession) are today together known as Milankovitch cycles. Scientists today are in general agreement that the Milankovitch cycles are a major factor in the formation of ice ages. Other feedback mechanisms on the Earth, however, are also believed to contribute to the emergence of ice ages.