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Small
airborne particles (aerosols) are responsible for a variety of well known
optical phenomena in the atmosphere, e.g. rainbows, halos and deep red-coloured
sunrises and sunsets. The latter is a direct consequence of selective extinction
of sunlight by Rayleigh- and Mie-scattering. Light scattering and absorption
by anthropogenic aerosol emissions from biomass-burning and fuel-combustion
may affect the atmospheric heat budged, i.e. the earth's climate, the visibility,
and even photochemical reaction rates. Due to their high spatial and temporal
variability the influences of aerosols on climate are much more complex
than those for greenhouse gases. Different sources and production mechanisms
provide a wide variety of different compositions and morphologies. Moreover,
during the atmospheric residence times, from less than a day to more than
a month, the microphysical aerosol properties are aged. A detailed knowledge
of aerosol optical properties is required to assess the direct shortwave
radiative forcing of anthropogenic aerosols.
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