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Titlebook: Atmospheric Environmental Research; Critical Decisions B Detlev Möller Conference proceedings 1999 Springer-Verlag Berlin Heidelberg 1999 A

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Can Laboratory Data be Related with the Real World?ry data, such as absorption cross sections of pure compounds, wavelength-resolved quantum yields of photochemical processes, and rate constants of elementary chemical reactions, are measured in artificial systems which are considerably less complex than the real world, and under conditions (e.g., in
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An Example for a Man-Made Induced Feedback on the Global Oxidation Capacity: The Possible Increase os, with most of the increase occurring over the past 20 years (Sigg and Neftel 1991; Anklin and Bales 1997). Reasons for that finding have been related to human activities in general (Sigg and Neftel 1991), to the increase of emission rates of NO., CH. and CO (Sigg and Neftel 1991; Anklin and Bales
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Is the Oxidising Capacity of the Troposphere Changing?se compounds can have serious effects on the physical and chemical properties of the atmosphere to such an extent that far reaching environmental changes detrimental to both humans and vegetation can result. However, the atmosphere fortunately has the built-in capability for self-decontamination thr
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Five-Year Record of Ozone at Mt. Brocken (Germany) — Implications for Changing Heterogeneous Chemist20 years in the free troposphere suggest a yearly increase of about 1% yr. in the northern hemisphere (WMO 1991). Moreover, continuous records in the former East Germany show that ground-based ozone increased between 1955 and 1980 by about 2% yr..
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