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 change the total amount of sunlight reaching the Earth by up to 25% at mid-latitudes (from 400 to 500 Wm−2 at latitudes of 60 degrees). In this context, the term "forcing" signifies a physical process that affects the Earth's climate.
This mechanism is believed to be responsible for the timing of the ice age cycles. A strict application of the Milankovitch theory does not allow the prediction of a "sudden" ice age (rapid being anything under a century or two), since the fastest orbital period is about 20,000 years. 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.
It is sometimes asserted that the length of the current interglacial temperature peak will be similar to the length of the preceding interglacial peak (Sangamonian/Eem Stage), and that therefore we might be nearing the end of this warm period. However, this conclusion is probably mistaken: the lengths of previous interglacials were not particularly regular (see graphic at right). Berger and Loutre (2002) argue that “with or without human perturbations, the current warm climate may last another 50,000 years. The reason is a minimum in the eccentricity of Earth's orbit around the Sun.” Also, Archer and Ganopolski (2005) report that probable future CO2 emissions may be enough to suppress the glacial cycle for the next 500 kyr.
Note in the graphic the strong 100,000 year periodicity of the cycles, and the striking asymmetry of the curves. This asymmetry is believed to result from complex interactions of feedback mechanisms. It has been observed that ice ages deepen by progressive steps, but the recovery to interglacial conditions occurs in one big step.
Orbital mechanics require that the length of the seasons be proportional to the swept areas of the seasonal quadrants, so when the eccentricity is extreme, the seasons on the far side of the orbit can last substantially longer. Today, when autumn and winter in the northern hemisphere occur at closest approach, the earth is moving at its maximum velocity and therefore autumn and winter are slightly shorter than spring and summer.
Today, northern hemisphere summer is 4.66 days longer than winter and spring is 2.9 days longer than autumn. As axial precession changes the place in the Earth's orbit where the solstices and equinoxes occur, Northern hemisphere winters will get longer and summers will get shorter, eventually creating conditions believed to be favorable for triggering the next glacial period.
The arrangements of land masses on the Earth's surface are believed to reinforce the orbital forcing effects. Comparisons of plate tectonic continent reconstructions and paleoclimatic studies show that the Milankovitch cycles have the greatest effect during geologic eras when landmasses have been concentrated in polar regions, as is the case today. Greenland, Antarctica, and the northern portions of Europe, Asia, and North America are situated such that a minor change in solar energy will tip the balance between year-round snow/ice preservation and complete summer melting. The presence of snow and ice is a well-understood positive feedback mechanism for climate.
- ^ Berger, A.; Loutre, M. F. (2002). "An Exceptionally Long Interglacial Ahead?". Science 297 (5585): 1287–1288. doi:10.1126/science.1076120. PMID 12193773.
- ^ Archer, David; Ganopolski, Andrey (2005). "A Movable Trigger: Fossil Fuel CO2 And The Onset Of The Next Glaciation". Geochemistry Geophysics Geosystems 6 (5): Q05003. doi:10.1029/2004GC000891.
- ^ Benson, Gregory (2007-12-11). "Global Warming, Ice Ages, and Sea Level Changes: Something new or an astronomical phenomenon occurring in present day?". https://sites.google.com/site/bensonfamilyhomepage/Home/ice-age-and-global-warming.
- 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.
- Hays, James D. (1996). Schneider, Stephen H.. ed. Encyclopedia of Weather and Climate. New York: Oxford University Press. pp. 507–508. ISBN 0195094859.
- Lutgens, Frederick K.; Tarbuck, Edward J. (1998). The Atmosphere. An Introduction to Meteorology. Upper Saddle River, N.J.: Prentice-Hall. ISBN 0137429746.
- National Research Council (1982). Solar Variability, Weather, and Climate. Washington, D.C.: National Academy Press. p. 7. ISBN 0309032849.
- The NOAA page on Climate Forcing Data includes (calculated) data on orbital variations over the last 50 million years and for the coming 20 million years
- The orbital simulations by Varadi, Ghil and Runnegar (2003) provide another, slightly different series for orbital eccentricity
Climate oscillations Climate oscillations8.2 kiloyear event · Antarctic Circumpolar Wave · Antarctic oscillation · Arctic dipole anomaly · Arctic oscillation · Atlantic Equatorial mode · Atlantic multidecadal oscillation · Bond event · Dansgaard–Oeschger event · Diurnal cycle · El Niño-Southern Oscillation · Equatorial Indian Ocean oscillation · Glacial cycles · Indian Ocean Dipole · Madden–Julian oscillation · Milankovitch cycles · North Atlantic oscillation · North Pacific Oscillation · Orbital forcing · Pacific decadal oscillation · Pacific-North American teleconnection pattern · Quasi-biennial oscillation · Seasons · Solar variability
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