In the eyes of Milutin Milankovitch, there’s been a noticeable trend in climate, temperature and seasons due to this cycle.
And we can accredit these long-term climate changes to 3 variations in geometry between the Earth and sun:
- How the Earth orbits the sun (Eccentricity)
- What angle Earth faces the sun (Obliquity)
- How Earth’s axis of rotation changes (Precession)
If you put these 3 interactions of Earth and the sun together, they form the Milankovitch Cycle. Let’s explore with more detail.
1 Orbital eccentricity
Earth revolves around the sun in a roughly circular orbit. But roughly every 100,000 years, its orbit becomes more eccentric.
So it starts as a circular orbit like it is in its current state. But like a pendulum, eccentricity will swing it back the other way with a more elliptical orbit.
Because Venus is so close to Earth, its gravitational interactions slightly pulls Earth in its orbit. Then, colossal Jupiter pulls Earth slightly outside its orbit at the opposite end.
So Earth periodically goes from a circular orbit to a more elliptical one (high eccentricity). This is due to the gravitational pull of neighboring planets.
Because of its orbital eccentricity, Earth varies in distance from the sun. As a result, it receives less solar radiation causing it to cool.
2 Obliquity variation
The next piece of the puzzle is obliquity. Right now, Earth’s obliquity is 23.5°. But during the Milankovitch Cycle, it varies from 22.1° to 24.5° and takes 40,000 years to complete a full cycle.
Earth’s changing obliquity doesn’t alter the total amount of incoming solar radiation. Instead it affects the geographic distribution of where sunlight hits the Earth.
For example, if axial tilt increases, winters are colder in both hemispheres. And vice versa for when axial tilt decreases.
In summary, more tilt signifies more severe seasons. For instance, this can cause longer periods of glaciation. And for Earth as a system, it enters positive and negative climate feedback loops.
The effects are drastic for long-term climate change. And this is all because of Earth’s change in axial tilt that gradually shifts every 40,000 years.
3 Axial precession
Axial precession is the movement of the rotational axis of Earth. According to the Milankovitch Cycle, precession has a cycle of roughly 23,000.
Precession occurs because the Earth is not a perfect sphere. It flattens out at the poles and widens at the equator. In addition, the gravitational pull from the sun and moon cause precession.
Similar to obliquity, precession doesn’t change the total amount of solar radiation that hits Earth. But precession primarily alters the perihelion and aphelion.
Overall, this increases the seasonal differences from one hemisphere to the other.