improved (i.e., lower emission) technologies for
transport, industry and domestic heating/cooking
will determine local atmospheric composition
over the coming decade. Dramatic improvements
have been shown to be possible in cities when
suitably stringent emission controls are implemented, for example, during the Beijing Olympics
in 2008 [14, 36]. A key issue for future urban
atmospheric composition processes is the potentially changing climate within which the air chemistry takes place, and the global perspective of
cities as sources of a range of pollutants into the
wider atmosphere. A number of the processes
outlined above are strongly temperaturedependent, in particular the stability of PAN and
other organic nitrates which sequester NO x , and
the equilibria between the condensed and vapor
phases for many of the secondary components of
PM, in particular nitrate. Changed temperatures
will also affect emission sources, including evaporative losses of fuels, and emissions of biogenic
VOCs, many of which are strongly (and nonlinearly) temperature-dependent, and has been
suggested to affect the prevalence of the meteorological patterns which favor ozone pollution episodes, such as the western European heatwave of
2003 [37]. These latter effects may particularly
influence the background atmospheric composition (ozone levels) upon which localized urban
influences build. Urban heat island effects already
drive some of these changes on a local scale.
A potentially larger climate-related impact may
however arise from the widespread adoption of
non-fossil-fuel-based transportation systems,
driven by carbon emission considerations. Should
this occur, our currently low understanding of the
non-exhaust contributions to urban air pollution
will assume much greater importance.
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