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Thousands of years later download
Thousands of years later download






thousands of years later download

A.: 1994, ‘The Sensitivity of the Terrestrial Biosphere to Climatic Change: A Simulation of the Middle Holocene’, Global Biogeochem. Jr.: 1971, The Roots of Ancient India, MacMillan, NY.įoley, J. I.: 1996, ‘Natural and Anthropogenic Changes in Atmospheric CO2 over the Last 1000 Years from Air in Antarctic Ice and Firn’, J. (ed.), Cambridge Encyclopedia of Archeology, Cambridge Univ. Norton, NY.ĭjevsky, N.: 1980, ‘The Urbanization of Eastern Europe’, in Sherratt, A. F.: 2000, ‘The “Anthropocene”’, IGBP Newsletter 41, 12.ĭiamond, J.: 1997, Guns, Germs, and Steel, W. J.: 2000, ‘Causes of Climatic Change in the Last 1000 Years’, Science 289, 270.Ĭrutzen, P. J.: 1992, ‘Climate Forcing by Anthropogenic Aerosols’, Science 255, 423.ĬOHMAP Project Members: 1988, ‘Climatic Changes of the Last 18000 Years: observations and model simulations’, Science 241, 1043.Ĭrowley, T.

thousands of years later download

J., Schwarz, S.E.,Hales, J.M., Cess, R.D., Coakley, J. S., and Lorius, C.: 1990, ‘Atmospheric CH4 Record over the Last Climatic Cycle Revealed by the Vostok Ice Core’, Nature 345, 127.Ĭhappelaz, J., Blunier, T., Kints, S., Dallenbach, A., Barnola, J.–M., Schwander, J., Raynaud, D., and Stauffer, B.: 1997, ‘Change in the Atmospheric CH4 Gradient between Greenland and Antarctica during the Holocene’, J. London, B 275, 143.Ĭhappellaz, J., Barnola, J.–M., Raynaud, D., Korotkevitch, Y. E.: 1991, Disease and History, Dorsett Press, NY.Ĭhang, T.–T.: 1976, ‘The Rice Cultures’, Phil. J., Sowers, T., and Orchado, J.: 1996, ‘Rapid Variations in Atmospheric Methane Concentration during the Past 110,000 Years’, Science 273, 1087.Ĭartwright, F. M.: 2000, ‘On the Origin and Timing of Rapid Changes in Atmospheric Methane during the Last Glacial Period’, Global Biogeochem. J., Harder, S., Severinghaus, J., Steig, E., and Sucker, C. C., Peng, T.–H., Hajdas, I., and Bonani, G.: 1999, ‘Evidence for a Reduction in the Carbonate Ion Content of the Deep Sea during the Course of the Holocene’, Paleoceanogr. S.: 1996, Armies of the Pestilence, Barnes and Noble, N.Y.īroecker, W. Paris 323 (IIa) 1.īlunier, T., Chappellaz, J., Schwander, J., Stauffer, J., and Raynaud, D.: 1995, ‘Variations in Atmospheric Methane Concentration during the Holocene Epoch’, Nature 374, 46.īray, R. and Loutre, M.–F.: 1996, ‘Modeling the Climate Response to Astronomical and CO2 Forcings’, Geophys. 58A, 71.īard, E., Raisbeck, G., Yiou, F., and Jouzel, J.: 2000, ‘Solar Irradiance Changes during the Past 1200 Years Based on Cosmogenic Nuclides’, Tellus 52B, 985.īerger, A., Gallee, H., Fichefet, T., Marsiat, I., and Tricot, C.: 1990, ‘Testing the Astronomical Theory with a Coupled Climate–Ice–Sheet Model’, Palaeogeogr. Extent Mapped from LANDSAT–1 Imagery’, Geogr. T., and Wright, C.: 1976, ‘Little Ice Age Permanent Snowcover in the Eastern Canadian Arctic. H., Zangger, E., and Demitrack, A.: 1990, ‘Land Use and Soil Erosion in Prehistoric and Historical Greece’, J. Plague-driven CO 2 changes were also a significant causal factor in temperature changes during the Little Ice Age (1300–1900 AD). Forest regrowth on abandoned farms sequestered enough carbon to account for the observed CO 2decreases. CO 2 oscillations of ∼ 10 ppm in the last 1000 years are toolarge to be explained by external (solar-volcanic) forcing, but they can be explained by outbreaks of bubonic plague that caused historically documented farm abandonment in western Eurasia. In recent millennia, the estimated warming caused by these early gas emissions reached a global-mean value of ∼ 0.8 ☌ and roughly 2 ☌ at high latitudes, large enough to have stopped a glaciation of northeastern Canada predicted by two kinds of climatic models.

thousands of years later download

(3) A wide array of archeological, cultural, historical and geologic evidence points to viable explanations tied to anthropogenic changes resulting from early agriculture in Eurasia, including the start of forest clearance by 8000 years ago and of rice irrigation by 5000 years ago. (1) Cyclic variations in CO 2 andCH 4 driven by Earth-orbital changes during the last 350,000 years predict decreases throughout the Holocene, but the CO 2 trend began ananomalous increase 8000 years ago, and the CH 4 trend did so 5000 years ago.(2) Published explanations for these mid- to late-Holocene gas increases basedon natural forcing can be rejected based on paleoclimatic evidence. This hypothesis is based on three arguments. A different hypothesis is posed here: anthropogenic emissions of these gases first altered atmospheric concentrations thousands of years ago. The anthropogenic era is generally thought to have begun 150 to 200 years ago, when the industrial revolution began producing CO 2 andCH 4 at rates sufficient to alter their compositions in the atmosphere.








Thousands of years later download