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HUMAN INFLUENCES ON CLIMATE CHANGE   7


                       FOSSIL FUELS

                       Carbon dioxide variations over the last 400,000 years have shown a rise since the
                       industrial revolution. Beginning in the 1850s and accelerating ever since, the
                       human consumption of fossil fuels has elevated CO levels from a concentration
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                       of 280 ppm to more than 380 ppm today. These increases have been projected to
                       reach more than 560 ppm before the end of the twenty-first century. It is known
                       that CO levels are substantially higher now than at any other time in the last
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                       800,000 years. Along with rising levels of atmospheric pollutants, it is anticipated
                       that there will be an increase in global temperature by 1.4–5.6°F between 1990
                       and 2100 (Fig. 1.6).



                       MILLENNIAL PERSPECTIVE OF CARBON DIOXIDE
                       VARIATIONS
                       Organic materials such as plants (mainly formed from hydrocarbons and water molecules)
                       under certain conditions, such as natural disasters, fires, volcanic activity, tectonic plate
                       displacement, and extreme geoclimatic changes, lose significant amounts of their water
                       content and are left with solely carbon and mineral materials. It is because of the sun’s
                       energy that organic life, in accordance with certain chemical processes, is transformed
                       into various forms of hydrocarbon organic structures.
































                 Figure 1.6  Projected changes in CO 2 and global temperature: summary of assumptions
                 in the IPCC 1992 alternative scenarios. Courtesy of United Nations Environmental Program/GRID-Arendal.
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