The dynamics are complex. The changes affect the 'insolation' (sunlight falling on parts of the Earth). This leads to cycles of climate on Earth, at about 21,000, 41,000 years, 100,000 and 400,000 years. This whole field is still under active research.
Similar astronomical theories had been advanced in the 19th century by Joseph Adhemar, James Croll and others. However, there was at first no reliable dated evidence. The issue was not settled until deep-ocean cores were taken and a paper published in Science in 1976.
The cycles[change | change source]
Orbital shape (eccentricity)[change | change source]
Earth's orbit is an ellipse. The eccentricity is a measure of the departure of this ellipse from circularity. The shape of the Earth's orbit varies in time between nearly circular and mildly elliptical.
Axial tilt (obliquity)[change | change source]
The angle of the Earth's axial tilt varies with respect to the ecliptic plane, because perturbations from other planets shift the Earth's orbit.
When the obliquity increases, the summers in both hemispheres receive more heat and light from the Sun, and winters less. Conversely, when the obliquity decreases, summers receive less sunshine and winters more. These slow 2.4° obliquity variations are roughly periodic. They take about 41,000 years to shift between a tilt of 22.1° and 24.5° and back again.
Axial precession[change | change source]
Precession is the wobble of the Earth's axis. This gyroscopic motion is due to the tidal forces exerted by the sun and the moon on the solid Earth, which has the shape of an oblate spheroid rather than a sphere. The sun and moon contribute roughly equally to this effect. Its period is about 26,000 years.
When the axis points toward the Sun, one polar hemisphere has a greater difference between the seasons while the other has milder seasons. The hemisphere that is in summer at perihelion receives much of the corresponding increase in solar radiation, but that same hemisphere in winter at aphelion has a colder winter. The other hemisphere will have a relatively warmer winter and cooler summer.
Apsidal precession[change | change source]
Planets orbiting the Sun follow elliptical (oval) orbits that rotate gradually over time (apsidal precession).
In addition, the orbital ellipse itself precesses in space, primarily as a result of interactions with Jupiter and Saturn. This shortens the period of the precession of the equinoxes from 25,771.5 to ~21,636 years.
Orbital inclination[change | change source]
The inclination of Earth's orbit drifts up and down relative to its present orbit with a cycle having a period of about 70,000 years. Milankovitch did not study this three-dimensional movement. This movement is known as 'precession of the ecliptic' or 'planetary precession'.
Researchers noted this drift, and also that the orbit moves relative to the orbits of the other planets. The invariable plane, the plane that represents the angular momentum of the Solar System, is approximately the orbital plane of Jupiter. The inclination of the Earth's orbit has a 100,000 year cycle relative to the invariable plane. This is very similar to the 100,000 year eccentricity period. This 100,000-year cycle closely matches the 100,000-year pattern of ice ages.
It has been proposed that a disk of dust and other debris exists in the plane, which affects the Earth's climate. The Earth moves through this plane around January 9 and July 9, when there is an increase in radar-detected meteors and meteor-related noctilucent clouds.
A study of the Antarctic ice core, using oxygen-nitrogen ratios in air bubbles trapped in the ice, concluded that the climatic response documented in the ice cores was driven by Northern hemisphere insolation as proposed by the Milankovitch hypothesis. This is an additional validation of the Milankovitch hypothesis by a relatively new method. It is not consistent with the "inclination" theory of the 100,000-year cycle.
Related pages[change | change source]
References[change | change source]
- Milankovitch, Milutin (1998) . Canon of insolation and the Ice Age problem. Belgrade: Zavod za Udz̆benike i Nastavna Sredstva. ISBN 8617066199.; see also "Astronomical theory of climate change".
- Hays J.D; Imbrie J. & Shackleto, N.J. 1976. Variations in the Earth's orbit: pacemaker of the ice ages. Science 194 (4270): 1121–1132. 
- Richard A Muller & Gordon J MacDonald (1997). "Glacial cycles and astronomical forcing". Science 277 (1997/07/11): 215–8. doi:10.1126/science.277.5323.215.
- Richard A Muller. "Origin of the 100 kyr Glacial Cycle: eccentricity or orbital inclination?". Retrieved March 2, 2005.
- Kawamura et al. 2007. Nature. 448, p912-917