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+d- <br />t <br />tt., t 'S5S k _ ? <br />? S,P i F i Flt qt, <br />1. INTRODUCTION <br />6 <br />A. UNDERSTANDING CLIMATE CHANGE <br />Scientists around the globe have been working to- <br />gether for decades to track the increase of greenhouse <br />gases in the Earth's atmosphere, rising temperatures <br />and extreme weather. They agree that the planet is <br />warming much more than under natural conditions, <br />and the cause is human activity - primarily the <br />burning of fossil fuels. <br />Earlier this year, the Intergovernmental Panel on <br />Climate Change (IPCC), which includes hundreds <br />of scientists worldwide and was awarded the Nobel <br />Peace Prize last month, issued three new reports on <br />climate change. The key statements are: <br />"Warming of the climate system is unequivocal, as is <br />now evident from observations of increases in global <br />average air and ocean temperatures, widespread <br />melting of snow and ice, and rising global average <br />sea level." <br />"Most of the observed increase in globally averaged <br />temperatures since the mid-201h Century is very like- <br />ly due to the observed increase in [human-caused] <br />greenhouse gas concentrations." <br />How greenhouse gases work to raise temperatures: <br />Three greenhouse gases produced by natural <br />processes and human activity - carbon dioxide, <br />methane and nitrous oxide - make up less than <br />I percent of Earth's atmosphere, but they exert <br />powerful control over global temperatures. The <br />greenhouse gases absorb the sun's heat as it radiates <br />back from the Earth's surface toward space, and trap <br />that heat in the atmosphere. <br />Over the past 650,000 years, the average concentra- <br />tions of greenhouse gases maintained by nature gave <br />the planet a balanced climate that fostered bountiful <br />ecosystems and eventually civilization and agricul- <br />ture. Greenhouse gas concentrations went up and <br />down with the natural cycle of ice ages, but were <br />never higher than 300 parts per million (ppm). <br />The last century and a half of industrialization <br />changed the balance. Billions of tons of carbon, once <br />safely stored deep underground in the form of coal, oil <br />and gas, are being released into the atmosphere. About <br />80 percent of human-produced greenhouse gases are <br />released from the burning of fossil fuels. The other 20 <br />percent comes from burning tropical forests and from <br />agriculture and landfills. <br />In the air or by combustion, carbon mixes with <br />oxygen to form carbon dioxide, or COV Of all <br />greenhouse gas emissions resulting from human <br />activity, CO2 makes up about 75 percent. Worldwide, <br />we are releasing 7 billion tons of carbon per year into <br />the atmosphere. <br />Ice cores drilled in Antarctica show that greenhouse <br />gas concentrations started spiking in the late 1800s, <br />at the time of the Industrial Revolution. At that time, <br />the atmosphere held 280 ppm of CO 2' By 2006, <br />CO2 concentrations reached 382 ppm, a 35 percent <br />increase and by far the highest level in all of human <br />history. In the last decade alone, we increased the <br />concentration of CO2 in the atmosphere by 19 ppm. <br />As a result, the global average temperature increased <br />by 1.4 degrees Fahrenheit (F.) in the last century. That <br />may not seem like much, but scientists are observ- <br />ing many examples of rapid, destructive changes in <br />ecosystems worldwide from that increase. <br />Scientists project the global temperature will continue <br />to rise - the question is by how much. The IPCC <br />developed a range of future scenarios based on no <br />new policies to stabilize or reduce greenhouse gas <br />emissions. Under these "business as usual" scenarios, <br />greenhouse gas concentrations could reach 600 to <br />1,000 ppm by the end of this century, resulting in <br />global temperature increases of 3.6 to 10.4 degrees F.