2003 | OriginalPaper | Chapter
Tropospheric Aerosols
Authors : Jost Heintzenberg, Frank Raes, Stephen E. Schwartz, Ingmar Ackermann, Paulo Artaxo, Timothy S. Bates, Carmen Benkovitz, Keith Bigg, Tami Bond, Jean-Louis Brenguier, Fred L. Eisele, Johann Feichter, Andrea I. Flossman, Sandra Fuzzi, Hans-F. Graf, Jeremy M. Hales, Hartmut Herrmann, Thorsten Hoffmann, Barry Huebert, Rudolf B. Husar, Ruprecht Jaenicke, Bernd Kärcher, Yoram Kaufman, Geoffrey S. Kent, Markku Kulmala, Caroline Leck, Catherine Liousse, Ulrike Lohmann, Beatrice Marticorena, Peter McMurry, Kevin Noone, Colin O’Dowd, Joyce E. Penner, Alex Pszenny, Jean-Philipe Putaud, Patricia K. Quinn, Ulrich Schurath, John H. Seinfeld, Herman Sievering, Jeffrey Snider, Irina Sokolik, Frank Stratmann, Rita van Dingenen, Douglas Westphal, Anthony S. Wexler, Alfred Wiedensohler, David M. Winker, Julian Wilson
Published in: Atmospheric Chemistry in a Changing World
Publisher: Springer Berlin Heidelberg
Included in: Professional Book Archive
Activate our intelligent search to find suitable subject content or patents.
Select sections of text to find matching patents with Artificial Intelligence. powered by
Select sections of text to find additional relevant content using AI-assisted search. powered by
Between 1970 and 1990 the major advances in atmospheric chemistry were made in gas-phase photochemistry, except perhaps for a brief intermezzo of “nuclear winter” studies. This focus is now shifting, as it is recognised that natural and anthropogenic aerosols play a substantial role in the radiative properties of the atmosphere and Earth’s climate. In addition, studies on the causes of the Antarctic ozone hole have demonstrated the large role of reactions that take place on ice and particulate surfaces. If such reactions occur in the stratosphere, they must take place also in the troposphere, with its abundance of various types of aerosol. Considering these factors, and especially because of various break-throughs in experimental techniques, it is likely that aerosol research will be prominent in atmospheric chemistry in the coming decades. This research will involve process studies both in the atmosphere and in laboratories, studies on the sources and sinks of aerosols, chemical analyses of the particulate matter (PM), modelling, and especially regional (campaigns) and global (satellites) observations on the distribution of the atmospheric aerosol. This is all the more important because climate models, which in most cases currently consider only sulphur chemistry, cannot be tested sufficiently for want of data, despite the potentially great climate effects of aerosols. Aerosol particles may already be significantly counteracting the radiative forcing by the greenhouse gases (Ramaswamy et al. 2001).