Page 109 - The Green Building Bottom Line The Real Cost of Sustainable Building
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88  CHAPTER 3



                     54 degrees Fahrenheit warmer than it would be without an atmosphere. 12  GHGs are
                     necessary for life on Earth—otherwise our planet would be freezing. The problem
                     occurs when the levels of greenhouse gases sharply increase, as has been occurring at
                     an accelerated rate over the past two hundred years. This dramatic increase in GHGs
                     throws off the delicate atmospheric balance and contributes to a host of climatic
                     changes, the most significant being an ever-warming planet, which in turn contributes
                     to the melting of the polar ice caps, rising sea levels, and a dramatic shift in weather
                     patterns.
                       Carbon dioxide (CO ) is the primary greenhouse gas of interest, as human activities
                                        2
                     are greatly increasing its concentration in the atmosphere, though there are six main
                     greenhouse gases that scientists measure. 13  In the past century, the concentration of
                     carbon dioxide in the atmosphere has risen almost 30 percent, methane levels have
                     more than doubled, and nitrous oxide concentrations have increased by 15 percent. 14
                     Furthermore, the growth in atmospheric greenhouse gas concentrations has been pro-
                     gressing at a more rapid rate over time. For example, concentrations of CO have
                                                                                       2
                     increased during the last forty years at a rate 50 percent higher than seen in the previ-
                     ous two hundred years (54 parts per million [ppm] increase from 1960 to 2000 vs. the





                      TABLE 3.1  COMMON GREENHOUSE GASES

                                                 ATMOSPHERIC       GLOBAL WARMING POTENTIAL
                      GAS                       LIFETIME (YEARS)          (100 YEAR)
                      Carbon Dioxide (CO )         50–200                     1
                                      2
                      Methane (CH )                 9–15                      21
                                 4
                      Nitrous Oxide (N O)           120                      310
                                    2
                      Hydrofluorocarbons (HFCs)
                       HFC-23                       260                     11,700
                       HFC-125                       29                      2,800
                       HFC-134a                     13.8                     1,300
                       HFC-143a                      52                      3,800
                       HFC-152a                      1.4                     140
                       HFC-227ea                     33                      2,900
                       HFC-236fa                     22                      6,300
                      Perfluorocarbons
                       Perfluoromethane (CF )       50,000                    6,500
                                         4
                       Perfluoroethane (C F )       10,000                    9,200
                                       2 6
                      Sulfur Hexafluoride (SF )      3,200                   23,900
                                         6
                      Source: Intergovernmental Panel on Climate Change. 16
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