Orbital forcing

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Ice core data. Note length of glacial cycles averages ~100,000 years. Blue curve is temperature, green curve is CO2, and red curve is windblown glacial dust (loess).[1]
An average of several samples of δ18O, a proxy for temperature, for the last 600,000 years

Orbital forcing is the effect on climate of slow changes in the tilt of the Earth's axis and shape of the orbit (see Milankovitch cycles). These orbital changes alter the amount of sunlight reaching the Earth by up to 25% at mid-latitudes. In this context, the term "forcing" is a physical process that affects the Earth's climate.

This mechanism is believed to be responsible for the timing of the ice age cycles. The timing of past glacial periods coincides very well with the predictions of the Milankovitch theory, and these effects can be calculated into the future.

Note in the graphic the strong 100,000 year periodicity of the cycles, and the striking asymmetry of the curves. Ice ages deepen by progressive steps, but the recovery to interglacial conditions occurs in one big step.

References[change | edit source]

  1. Hays J.D.; Imbrie John; Shackleton N.J. (1976). "Variations in the Earth's orbit: pacemaker of the ice ages". Science 194 (4270): 1121–1132. doi:10.1126/science.194.4270.1121. PMID 17790893.