| TEMPERATURE RISING
 Chapter 2. Signs of Stress: Climate and Water
 
 Lester R. Brown, Eco-Economy: Building an Economy for the Earth 
              (W.W. Norton & Co., NY: 2001).
 
 Since agriculture began, the earth's climate 
              has been remarkably stable. Now the earth's temperature is rising, 
              apparently due to the greenhouse effectthe 
              warming that results from the rising concentration of heat-trapping 
              gases, principally carbon dioxide (CO2), in the atmosphere. 
 This rise in CO2 concentration comes from two sources: the burning 
              of fossil fuels and deforestation. Each year, more than 6 billion 
              tons of carbon are released into the atmosphere as fossil fuels 
              are burned. Estimates of the net release of carbon from deforestation 
              vary widely, but they center on 1.5 billion tons per year.5
 
 The release of CO2 from these two sources is simply overwhelming 
              nature's capacity to fix carbon dioxide. When the Industrial Revolution 
              began in 1760, carbon emissions from the burning of fossil fuels 
              were negligible. But by 1950, they had reached 1.6 billion tons 
              per year, a quantity that was already boosting the atmospheric CO2 
              level. In 2000, they totaled 6.3 billion tons. (See Figure 2-1.) 
              This fourfold increase since 1950 is at the heart of the greenhouse 
              effect that is warming the earth.6
 
 The carbon emissions of individual fossil fuels vary. Coal burning 
              releases more carbon per unit of energy produced than oil does, 
              and oil more than natural gas. The global fleet of 532 million gasoline-burning 
              automobiles, combined with thousands of coal-fired power plants, 
              are literally the engines driving climate change.7
 
 In addition, in recent years the world has been losing 9 million 
              hectares of forest per year. Forests store easily 20 times as much 
              carbon per hectare as does land in crops. If the net loss of forests 
              can be eliminated, this source of carbon emissions will disappear. 
              In the northern hemisphere, the forested area is actually increasing 
              by 3.6 million hectares a year. The big challenge is to arrest and 
              reverse the deforestation in developing countries.8
 
 At the start of the Industrial Revolution in 1760, the atmospheric 
              CO2 concentration was estimated at 280 parts per million (ppm). 
              By 2000, it had reached 370 ppm, a rise of 32 percent from pre-industrial 
              levels. (See Figure 2-2.) The buildup of atmospheric CO2 from 1960 
              to 2000 of 54 ppm far exceeded the 36 ppm rise from 1760 to 1960.9
 
 Atmospheric CO2 levels have risen each year since annual measurements 
              began in 1959, making this one of the most predictable of all environmental 
              trends. Physics textbooks point out that as atmospheric CO2 levels 
              rise, so will the earth's temperature, and this is exactly what 
              is happening. As noted earlier, the 14 warmest years since recordkeeping 
              began have all come since 1980. Over the last three decades, global 
              average temperature has risen from 13.99 degrees Celsius in 1969-71 
              to 14.43 degrees in 1998-2000, a gain of 0.44 degrees Celsius (0.8 
              degrees Fahrenheit).10
 
 The dramatic rise in the earth's temperature since 1980 can be clearly 
              seen in Figure 2-3. Not only is it rising rapidly, but it is projected 
              to rise even faster in the next century. If CO2 concentrations in 
              the atmosphere double pre-industrial levels by the end of this century, 
              reaching 560 ppm, the temperature is projected to rise by 1.4-5.8 
              degrees Celsius. Rising temperatures lead to more extreme climatic 
              eventsrecord 
              heat waves, the melting of ice, rising sea level, and more destructive 
              storms.11
 
 Projected temperature rises will not be distributed evenly over 
              the earth's surface, but will be greater over land areas than over 
              the oceans and also greater in the higher latitudes than in the 
              equatorial regions. Inland regions in northern latitudes can expect 
              some of the biggest temperature jumps. A taste of what is to come 
              can be seen in the July 1995 heat wave in Chicago, when temperatures 
              reached 38-41 degrees Celsius (100-106 degrees Fahrenheit) on five 
              consecutive days. Although Chicago is a modern industrial city with 
              extensive air conditioning, this heat wave claimed more than 500 
              lives. And because Chicago is in the center of the U.S. Corn Belt, 
              the intense heat also helped shrink the 1995 U.S. corn harvest by 
              some 15 percent or $3 billion.12
 
                
 
              
 ENDNOTES:
 5. Fossil fuel-related carbon emissions figure from Seth Dunn, "Carbon 
              Emissions Continue Decline," in Worldwatch Institute, Vital Signs 
              2001 (New York: W.W. Norton & Company, 2001), p. 53; WRI estimates 
              emissions of 1.6 billion tons carbon per year from land use change, 
              most of which is related to deforestation, in WRI, op. cit. note 
              4, p. 101.
 
 6. Figure 2-1 from Dunn, op. cit. note 5.
 
 7. Carbon and fossil fuels information from Energy Information Administration, 
              Annual Energy Outlook 2001, with Projections to 2020 (Washington, 
              DC: U.S. Department of Energy, 2000), p. 48; Michael Renner, "Vehicle 
              Production Sets New Record," in Worldwatch Institute, op. cit. note 
              5, p. 68.
 
 8. Changing forest cover from U.N. Food and Agriculture Organization 
              (FAO), Forest Resources Assessment (FRA) 2000, www.fao.org/forestry/fo/fra/index.jsp, 
              updated 10 April 2001, but see note in Chapter 8 on variations among 
              estimates; forests store 20 to 100 times more carbon than cleared 
              land, according to Mohan Wali et al., "Assessing Terrestrial Ecosystem 
              Sustainability: Usefulness of Regional Carbon and Nitrogen Models," 
              Nature & Resources, October-December 1999, p. 27.
 
 9. Figure 2-2 from Dunn, op. cit. note 5, pp. 52-53.
 
 10. Hansen, op. cit. note 2; Seth Dunn, "Global Temperature Steady," 
              in Worldwatch Institute, op. cit. note 5, pp. 50-51.
 
 11. Intergovernmental Panel on Climate Change (IPCC), "Climate Change 
              2001: Impacts, Adaptation, and Vulnerability (Summary for Policy 
              Makers)" (draft Feb 2001), www.ipcc.ch/pub/wg2SPMfinal.pdf ; Figure 
              2-3 based on Hansen, op. cit. note 2.
 
 12. Cindy Schreuder and Sharman Stein, "Heat's Toll Worse Than Believed, 
              Study Says at Least 200 More Died," Chicago Tribune, 21 September 
              1995; corn harvest data from U.S. Department of Agriculture (USDA), 
              Production, Supply, and Distribution, electronic database, Washington, 
              DC, updated May 2001.
 
 Copyright 
              © 2001 Earth Policy Institute
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