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The Southern Hemisphere commands an increasing interest among
atmospheric chemists. It has smaller and less industrialized
continents than the Northern Hemisphere and thus enjoys lower
emissions of anthropogenic and biogenic pollu tants. As a
consequence, the concentrations of trace species are lower in the
Sou thern Hemisphere, giving rise to significant inter-hemispheric
gradients. From an observation of the climatology of the various
trace gas gradients important conclu sions on the chemical
lifetimes, the distribution of sources and transport of trace
species can be derived. Thus it is only fitting that the CSIRO
Division of Atmos pheric Research, Aspendale, Australia, hosted the
Conference on the Scientific Application of Baseline Observations
of Atmospheric Composition (SABOAC). It was convened by Dr Graeme
Pearman of the CSIRO and sponsored by the CSIRO and the Australian
Bureau of Meteorology. Graeme Pearman and Ian Galbally of the CSIRO
also agreed to serve as Guest Editors. The Conference was well
attended and because of its location enjoyed an un usually large
number of participants from the Southern Hemisphere. About 40
papers were presented with a large share of original contributions.
At this point we would like to thank the reviewers who helped to
maintain strict standards. The con ference topics ranged from
Nonreactive Gases, Reactive Gases, Transport, Parti culates,
Precipitation Chemistry, to Radiation and Carbondioxide. The
present Proceedings do not quite maintain that sequence but partly
reflect the order of receipt. DIETER EHHALT 3 Journal of
Atmospheric Chemistry 3 (l985), 3-27."
The Southern Hemisphere commands an increasing interest among
atmospheric chemists. It has smaller and less industrialized
continents than the Northern Hemisphere and thus enjoys lower
emissions of anthropogenic and biogenic pollu tants. As a
consequence, the concentrations of trace species are lower in the
Sou thern Hemisphere, giving rise to significant inter-hemispheric
gradients. From an observation of the climatology of the various
trace gas gradients important conclu sions on the chemical
lifetimes, the distribution of sources and transport of trace
species can be derived. Thus it is only fitting that the CSIRO
Division of Atmos pheric Research, Aspendale, Australia, hosted the
Conference on the Scientific Application of Baseline Observations
of Atmospheric Composition (SABOAC). It was convened by Dr Graeme
Pearman of the CSIRO and sponsored by the CSIRO and the Australian
Bureau of Meteorology. Graeme Pearman and Ian Galbally of the CSIRO
also agreed to serve as Guest Editors. The Conference was well
attended and because of its location enjoyed an un usually large
number of participants from the Southern Hemisphere. About 40
papers were presented with a large share of original contributions.
At this point we would like to thank the reviewers who helped to
maintain strict standards. The con ference topics ranged from
Nonreactive Gases, Reactive Gases, Transport, Parti culates,
Precipitation Chemistry, to Radiation and Carbondioxide. The
present Proceedings do not quite maintain that sequence but partly
reflect the order of receipt. DIETER EHHALT 3 Journal of
Atmospheric Chemistry 3 (l985), 3-27."
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