Answer 2:
Good question, and not an easy one to answer. As
I'm sure you know, the main effect of fires on the
climate system is the release of dust particles
and aerosols into the atmosphere. (The release of
carbon dioxide and other greenhouse gases is also
significant but has a less severe immediate
effect.) As a rule of thumb, aerosols tend to
cool the climate system, because they scatter some
fraction of incoming sunlight back out to
space. For example, large volcanic eruptions such
as Mt. Pinatubo in 1991 (1992?)result in reduced
temperatures for the next 1-2 years, until the
aerosols act as nucleation points for water
vapor
and are rained out of the atmosphere.
But
this is only a rough rule and in general the
aggregate effect of aerosols on the climate system
are not well known. In fact, aerosols and
aerosol-cloud feedbacks are probably the major
sources of uncertainty in our modelling of the
present and future climate system. For more
information about the effects of aerosols on
future climate predictions, see the
Intergovernmental Panel on Climate Change's.
Sorry to not be able to
give a more definitive answer but this is a real
scientific frontier right now and a lot of
organizations are spending a lot of money studying
this issue. Click Here to return to the search form.
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