F5-2 Shape of the Earth's Orbit

Recent ice ages appear to have occurred approximately every 100,000 years. Periodicity in ice ages would seem to imply some kind of repetitive mechanism or mechanisms. Milankovitch proposed that changes in the shape of the Earth’s orbit and in the Earth’s axis of rotation were, in fact, just these mechanisms. Milankovitch specifically proposed that changes in three of the Earth’s orbital characteristics could produce enough changes in insolation to trigger an ice age.

Eccentricity measures how far an orbit deviates from a perfect circle.

One of these orbital characteristics is the shape of the Earth’s orbit. The shape of a body’s orbit is defined by the term eccentricity. An orbit that is completely circular has an eccentricity of 0. The eccentricity of an orbit increases as it becomes more and more elliptical; the eccentricity value gradually approaches 1. Eventually, a body will achieve an escape trajectory; the eccentricity at this point equals 1 or is greater than 1.