ACC would also include any «special»
regional effects of aerosols; aside from that, though, I think either term works.
It seems that at least
the regional effect of aerosols in S.E. - Asia is warming, not cooling... Thus any reduction there would have a cooling effect.
Not exact matches
The study also showed that the
effect was much larger on a
regional scale, counteracting possibly up to 30 %
of warming in more rural, forested areas where anthropogenic emissions
of aerosols were much lower in comparison to the natural
aerosols.
The top priorities should be reducing uncertainties in climate sensitivity, getting a better understanding
of the
effect of climate change on atmospheric circulation (critical for understanding
of regional climate change, changes in extremes) and reducing uncertainties in radiative forcing — particularly those associated with
aerosols.
The potential risks around sulfate
aerosol solar geoengineering include alteration
of regional precipitation patterns, its
effects on human health, and the potential damage to Earth's ozone layer by increased stratospheric sulfate particles.
Greenhouse gases are well mixed and have an
effect globally, other forcings may be more
regional (
aerosols, land use) but they can still have far field affects due to the nature
of the atmospheric circulation.
But more generally, something I've wondered is: while in the global annual average,
aerosols could be said to partly cancel (net
effect) the warming from anthropogenic greenhouse forcing, the circulatory, latitudinal,
regional, seasonal, diurnal, and internal variability changes would be some combination
of reduced changes from reduced AGW + some other changes related to
aerosol forcing.
Not it is not similar because one event injected sulfate
aerosols into the stratosphere where they stayed for years and affected the globe while the other («human particulates and
aerosol pollution») were produced in the troposphere and have a residency time in the atmosphere
of about 4 days and had only a
regional effect.
Changes in atmospheric composition from human activities are the main cause
of anthropogenic climate change by enhancing the greenhouse
effect, although with important
regional effects from
aerosol particulates (IPCC 2007).
«We found that
aerosol indirect
effect on deep convective cloud systems could lead to enhanced
regional convergence and a strong top -
of - atmosphere warming.»
Regional effects of aerosol forcing are large;
regional mean values
of anthropogenic
aerosol radiative forcing can be factors
of 5 to 10 higher than the global mean values
of 0.5 to 1.5 W m − 2 (IPCC, 2001).
Vegetation cover changes caused by land use can alter
regional and global climate through both biogeochemical (emissions
of greenhouse gases and
aerosols) and biogeophysical (albedo, evapotranspiration, and surface roughness) feedbacks with the atmosphere, with reverse
effects following land abandonment, reforestation, and other vegetation recoveries (107).
However, human activity may have already caused some some changes that are not yet detectable due to the small magnitude
of the changes or observation limitations, or are not yet confidently modeled (e.g.,
aerosol effects on
regional climate).
The study also showed that the
effect was much larger on a
regional scale, counteracting possibly up to 30 %
of warming in more rural, forested areas where anthropogenic emissions
of aerosols were much lower in comparison to the natural
aerosols.
The direct and indirect radiative
effects of aerosols suspended in the atmosphere above clouds (ACA) are a highly uncertain component
of both
regional and global climate.
Emissions scenarios were converted to projections
of atmospheric GHG and
aerosol concentrations, radiative forcing
of the climate,
effects on
regional climate, and climatic
effects on global sea level (IPCC, 2001a).