Fan went to China in 2008 for an ARM Mobile Facility field campaign studying
the climatic effects of aerosols in that country's fast - changing atmosphere.
1993 Thomas P. Charlock, et al., «Review of Recent Research on
the Climatic Effect of Aerosols.»
Not exact matches
A major
climatic downturn observed within the Greenland ice cores has been attributed to the cooling
effects of the ash and
aerosols ejected during the eruption
of the Youngest Toba Tuff (YTT).
While this is indeed very interesting and does suggest that
aerosol indirect
effects can have important
climatic consequences, it is merely the first step to attributing any particular
climatic effect (failure
of Sahel monsoon) to a particular cause (
aerosol indirect
effects).
SCIENTIFIC UNDERSTANDING
of these OTHER FACTORS â MOST NOTABLY NATURAL
climatic variations, changes in the sun's energy, and the cooling
effects of pollutant
aerosols â REMAINS INCOMPLETE.»
This proves that the
climatic effect of the removal
of stratospheric and tropospheric SO2
aerosol emissions is identical.
They concluded that with a bit
of help from changes in solar output and natural
climatic cycles such as the El Nino Southern Oscillation (ENSO), the growth in the volume
of aerosols being pumped up power station chimneys was probably enough to block the warming
effect of rising greenhouse gas emissions over the period 1998 - 2008.
However — a group
of scientists
of the US Department
of Energy Pacific Northwest National Laboratory, the University
of Maryland and the Hebrew University
of Jerusalem now say that
aerosol pollution does not necessarily lead to (low - lying) stratus clouds one would appreciate for
climatic cooling, but that it can also be a factor in the creation
of thunderstorm clouds, clouds that have a complicated climate
effect, but that are suspected
of being net warmers.
In any event, all
of these calcs are B S because we don't really understand the sum total
of past / present and future
aerosol effects nor
of CO2 feedbacks nor
of the combo
of CO2 feedbacks with changing
aerosols nor
of natural low frequency
climatic variation.
Theoretical and Applied Climatology covers climate modeling,
climatic changes and climate forecasting, micro - to mesoclimate, applied meteorology as in agro - and forestmeteorology, biometeorology, building meteorology and atmospheric radiation problems as they relate to the biosphere;
effects of anthropogenic and natural
aerosols or gaseous trace constituents; hardware and software elements
of meteorological measurements, including techniques
of remote sensing, among other topics
of current interest.
In fact, thee exists an attempt to reconstruct climate variations by stressing the
climatic effect of the volcano
aerosol, but the lack
of strong volcano spikes in the temperature record suggest that the volcano
effect is already overestimated.
This section assesses (1) the impact
of meteorological (
climatic) factors like wind, temperature and precipitation on the natural
aerosol burden and (2) possible
effects of aerosols on climate parameters and biogeochemistry.
But one thing all
aerosols have in common is that if you are going to balance the greenhouse
effect due to increasing levels
of carbon dioxide, you must keep increasing the amount
of aerosols — which will then increase the negative
effects associated with them — including diminished agricultural output and
climatic side -
effects — as they will not evenly counteract the
effects of increased carbon dioxide and its water vapor feedback due to evaporation.
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).
The relative importance
of the various
aerosol components is critical for the
aerosol climatic effect, since atmospheric
aerosols behave differently when their chemical composition changes.