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      A European aerosol phenomenology—1: physical characteristics of particulate matter at kerbside, urban, rural and background sites in Europe

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          Global warming in the twenty-first century: an alternative scenario.

          A common view is that the current global warming rate will continue or accelerate. But we argue that rapid warming in recent decades has been driven mainly by non-CO(2) greenhouse gases (GHGs), such as chlorofluorocarbons, CH(4), and N(2)O, not by the products of fossil fuel burning, CO(2) and aerosols, the positive and negative climate forcings of which are partially offsetting. The growth rate of non-CO(2) GHGs has declined in the past decade. If sources of CH(4) and O(3) precursors were reduced in the future, the change in climate forcing by non-CO(2) GHGs in the next 50 years could be near zero. Combined with a reduction of black carbon emissions and plausible success in slowing CO(2) emissions, this reduction of non-CO(2) GHGs could lead to a decline in the rate of global warming, reducing the danger of dramatic climate change. Such a focus on air pollution has practical benefits that unite the interests of developed and developing countries. However, assessment of ongoing and future climate change requires composition-specific long-term global monitoring of aerosol properties.
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            The Relationship between Mass and Mobility for Atmospheric Particles: A New Technique for Measuring Particle Density

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              PM10 and PM2.5 source apportionment in the Barcelona Metropolitan area, Catalonia, Spain

              X Querol (2001)
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                Author and article information

                Journal
                Atmospheric Environment
                Atmospheric Environment
                Elsevier BV
                13522310
                May 2004
                May 2004
                : 38
                : 16
                : 2561-2577
                Article
                10.1016/j.atmosenv.2004.01.040
                65bcbd21-f88e-45ab-8db4-cca98625c717
                © 2004

                http://www.elsevier.com/tdm/userlicense/1.0/

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