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PETROLEUM AND THE ENVIRONMENT                                    17




                                           Reflected
                                                ‘‘Greenhouse’’
                                               Gas absorbs and
                                                 re-emits IR
                        Incident solar
                          radiation                          Infrared
                                                            radiation









                                                        Atmosphere


            FIGURE 1.5  The greenhouse effect. (Source: Fanchi (2004). Reproduced with permission
            of Elsevier Academic Press.)

            (often abbreviated as NOx). The by‐products of unconfined combustion, including
            water vapor, are emitted into the atmosphere in gaseous form.
              Some gaseous combustion by‐products are called greenhouse gases because they
            absorb heat energy. Greenhouse gases include water vapor, carbon dioxide, methane,
            and nitrous oxide. Greenhouse gas molecules can absorb infrared light. When a
            greenhouse gas molecule in the atmosphere absorbs infrared light, the energy of the
            absorbed photon of light is transformed into the kinetic energy of the gas molecule.
            The associated increase in atmospheric temperature is the greenhouse effect illus-
            trated in Figure 1.5.
              Much of the solar energy arriving at the top of the atmosphere does not pass through
            the atmosphere to the surface of the Earth. A study of the distribution of light energy
            arriving at the surface of the Earth shows that energy from the sun at certain frequencies
            (or, equivalently, wavelengths) is absorbed in the atmosphere. Several of the gaps are
            associated with light absorption by a greenhouse gas molecule.
              One way to measure the concentration of greenhouse gases is to measure the
            concentration of a particular greenhouse gas. Charles David Keeling began
            measuring atmospheric carbon dioxide concentration at the Mauna Loa Observatory
            on the Big Island of Hawaii in 1958. Keeling observed a steady increase in carbon
            dioxide concentration since he began his measurements. His curve, which is now
            known as the Keeling curve, is shown in Figure 1.6. It exhibits an annual cycle in
            carbon dioxide concentration overlaying an increasing average. The initial carbon
            dioxide concentration was measured at a little over 310 parts per million. Today it
            is approximately 400 parts per million.  These measurements show that carbon
            dioxide concentration in the atmosphere has been increasing since the middle of the
              twentieth century.
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