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发表于 2009-12-27 06:50:09
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Background Imformation
Milankovitch Cycles Theory Milankovitch Theory describes the collective effects of changes in the Earth's movements upon its climate, named after Serbian civil engineer and mathematician Milutin Milankovi?. Milankovi? mathematically theorised that variations in eccentricity, axial tilt, and precession of the Earth's orbit determined climatic patterns on Earth, resulting in 100,000-year ice age cycles of the Quaternary glaciation over the last few million years. The Earth's axis completes one full cycle of precession approximately every 26,000 years. At the same time, the elliptical orbit rotates, more slowly, leading to a 23,000-year cycle between the seasons and the orbit. In addition, the angle between Earth's rotational axis and the normal to the plane of its orbit moves from 22.1 degrees to 24.5 degrees and back again on a 41,000-year cycle. Currently, this angle is 23.44 degrees and is decreasing.
The Milankovitch theory of climate change is not perfectly worked out; in particular, the largest observed response is at the 100,000-year timescale, but the forcing is apparently small at this scale, in regard to the ice ages.[1] The frequency modulation[2] or various feedbacks (from carbon dioxide, cosmic rays or from ice sheet dynamics) explain this discrepancy.
Milankovitch-like theories were advanced by Joseph Adhemar, James Croll and others, but verification was difficult due to the absence of reliably dated evidence and doubts as to exactly which periods were important. Not until the advent of deep-ocean cores and a seminal paper by Hays, Imbrie and Shackleton, "Variations in the Earth's Orbit: Pacemaker of the Ice Ages", in Science, 1976,[3] did the theory attain its present state. Milankovitch cycles theory is about the frequency of ice age. Milankovich proposed that the temperature of earth has something to do with the position of the earth in the orbit around sun. However it did not gain acceptance until 1968 when Dr. Imbrie presented additional evidence for M theory. He measured the isotope level in small seashell deposit and the change of isotope abundance corresponds with the temperature change.
However, later on, a geochemist tested the samples from Devil's Hole, a place in south Nevada and the results did not match with the previous results. Even thought Dr. Imbrie still think M theory was valid, he conceded that many other factors contribute to the isotope level. It may be why the results did not match.
Can We Date the Ice Ages? Following improvements in the ability to measure isotope ratios which came about as a spin-off of the wartime Manhattan project, physical chemist Harold Urey began to examine the possibility that the ratio of the two principal isotopes of oxygen found in the atmosphere might provide a clue as to past temperatures. It was based on the idea that the ratio of the heavier isotope (oxygen-18) to the more prevalent isotope (oxygen-16) found at the sea surface would change depending on the temperature of the ocean water near the surface. Urey thought that a careful study of the oxygen isotope ratio in the shells of sea creatures, which build their calcium carbonate shells from oxygen available in the seawater, might serve to indicate the temperature of the water in which they formed. During warmer periods, it was thought, evaporation from the ocean surface would tend to enrich the sea surface water with the heavier isotope of oxygen.
Perhaps, Urey reasoned, the isotope ratios found in the layers of discarded shells of sea organism which form the ocean bottom could thus serve as a record for the past temperatures of the ocean. The theory is fraught with many ifs, but it was pursued with persistence, starting in the 1950s, by Italian-educated micro paleontologist Cesare Emiliani, a one-time collaborator of Urey at the Argonne Laboratory then associated with University of Chicago. Emiliani identified certain species of small shell-forming sea organisms known as foraminifera有孔虫类, which he thought suitable for oxygen-isotope analysis to determine past climates. The conclusions he drew as to the dating of the ice ages were constantly challenged by leading oceanographers, who found them in contradiction with their studies of ocean bottom cores海底内核学说. The method was also attacked on the grounds that it wasn't clear that the creatures formed their shells壳, known as tests, near enough to the surface to reflect changes in isotope ratios.
p.s.: Quaternary glaciation:第四纪 一段地质时期,距今180万年至现代。第四纪继第三纪之后,是两个新生代中较近的一个。划分为更新世和全新世。第四纪的特征是气候在全球规模上有大的周期变化。这些变化引起了广大地区遭到冰盖的反复侵袭,所以这个纪常被称为大冰期。从生物学看,第四纪的主要特点是人类的进化和扩散。第四纪气候和环境的激烈变化引起了特别是哺乳类的迅速演化和灭绝。大型哺乳动物的灭绝可能也同当时人类领土的迅速扩大有关。 Earth’s movements As the Earth spins around its axis and orbits around the Sun, several quasi-periodic variations occur. Although the curves have a large number of sinusoidal components, a few components are dominant[1]. Milankovitch studied changes in the orbital eccentricity, obliquity, and precession of Earth's movements. Such changes in movement and orientation change the amount and location of solar radiation reaching the Earth. This is known as solar forcing (an example of radiative forcing). Changes near the north polar area are considered important due to the large amount of land, which reacts to such changes more quickly than the oceans do. |
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