"On a geological time scale, climate cycles are believed to be driven by changes in insolation (solar radiation received at the top of the atmosphere) as a result of variations in Earth's orbit around the Sun. Over the next 100,000 years, the amplitude of insolation variations will be small (see the
figure), much smaller than during the Eemian. For example, at 65°N in June, insolation will vary by less than 25 Wm[SUP]−2[/SUP] over the next 25,000 years, compared with 110 Wm[SUP]−2[/SUP] between 125,000 and 115,000 years ago. From the standpoint of insolation, the Eemian can hardly be taken as an analog for the next millennia, as is often assumed.
The small amplitude of future insolation variations is exceptional. One of the few past analogs (
13) occurred at about 400,000 years before the present, overlapping part of MIS-11. Then and now, very low eccentricity values coincided with the minima of the 400,000-year eccentricity cycle.
Eccentricity will reach almost zero within the next 25,000 years, damping the variations of precession considerably.
Simulations with a two-dimensional climate model (
14), forced with insolation and CO[SUB]2[/SUB] variations over the next 100,000 years, provide an insight into the possible consequences of this rare phenomenon. Most CO[SUB]2[/SUB] scenarios (
15) led to an exceptionally long interglacial from 5000 years before the present to 50,000 years from now (see the bottom panel of the figure), with the next glacial maximum in 100,000 years. Only for CO[SUB]2[/SUB] concentrations less than 220 ppmv was an early entrance into glaciation simulated (
15). "
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http://www.sciencemag.org/content/297/5585/1287.full