In the mid-20th century, coal - burning power plants and other sources released huge amounts of sulfur dioxide, which then formed toxic
sulfate aerosols in the atmosphere.
I'll let John Philips dig up the studies but just to add a little more explanation: It is not only that the sulfate aerosol pollution from First World countries started to decrease, it also has to do with the different residence time of CO2 and of
sulfate aerosols in the atmosphere.
Not exact matches
The results imply that the interaction between organic and sulfuric acids promotes efficient formation of organic and
sulfate aerosols in the polluted
atmosphere because of emissions from burning of fossil fuels, which strongly affect human health and global climate.
Ironically, if the world burns significantly less coal, that would lessen CO2 emissions but also reduce
aerosols in the
atmosphere that block the sun (such as
sulfate particulates), so we would have to limit CO2 to below roughly 405 ppm.
Aerosols are solid or liquid particles suspended
in the
atmosphere, consisting of (
in rough order of abundance): sea salt, mineral dust, inorganic salts such as ammonium
sulfate (which has natural as well as anthropogenic sources from e.g. coal burning), and carbonaceous
aerosol such as soot, plant emissions, and incompletely combusted fossil fuel.
That's far from the worst flaw
in his calculation, since his two biggest blunders are the neglect of the radiative cooling due to
sulfate aerosols (known to be a critical factor
in the period
in question) and his neglect of the many links
in the chain of physical effects needed to translate a top of
atmosphere radiative imbalance to a change
in net surface energy flux imbalance.
I'd like to learn whether or not spraying
sulfate aerosols high
in the
atmosphere to mitigate global warming will significantly enhance the probability of acid rain.
Do you mean simulations isolating
sulfate and nitrate
aerosols or do you mean simulations isolating CFCs (Chlorofluorocarbons), a relatively unimportant greenhouse gas - due to its relatively extremely low concentrations
in the
atmosphere?).
In my mind, the most serious peril of sulfate geoengineering is one that stems from a problem that is not at all in dispute: the fact that the lifetime of CO2 in the atmosphere is centuries to millennia, whereas the lifetime of aerosols in the stratosphere is at best a few year
In my mind, the most serious peril of
sulfate geoengineering is one that stems from a problem that is not at all
in dispute: the fact that the lifetime of CO2 in the atmosphere is centuries to millennia, whereas the lifetime of aerosols in the stratosphere is at best a few year
in dispute: the fact that the lifetime of CO2
in the atmosphere is centuries to millennia, whereas the lifetime of aerosols in the stratosphere is at best a few year
in the
atmosphere is centuries to millennia, whereas the lifetime of
aerosols in the stratosphere is at best a few year
in the stratosphere is at best a few years.
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.
This cooling was from the same root cause as volcanic cooling, namely
aerosols (mostly
sulfate aerosols)
in the
atmosphere.
Real Climate defines «
aerosols» as ``... solid or liquid particles suspended
in the
atmosphere, consisting of (
in rough order of abundance): sea salt, mineral dust, inorganic salts such as ammonium
sulfate (which has natural as well as anthropogenic sources from e.g. coal burning), and carbonaceous
aerosol such as soot, plant emissions, and incompletely combusted fossil fuel.»
Meanwhile, production of greenhouse gases — which linger
in the
atmosphere much longer than
sulfate aerosols — has continued, causing average global temperatures to rise.
The
Sulfate cooling mechanism is also evidenced whenever there is a high ejecta mass volcanic eruption, which causes a measurable cooling effect, for about 3 years after an eruption; until the sulfate particulate aerosols diminish in the atmosphere to the point that they become negl
Sulfate cooling mechanism is also evidenced whenever there is a high ejecta mass volcanic eruption, which causes a measurable cooling effect, for about 3 years after an eruption; until the
sulfate particulate aerosols diminish in the atmosphere to the point that they become negl
sulfate particulate
aerosols diminish
in the
atmosphere to the point that they become negligible.
They can either be directly emitted into the
atmosphere (primary
aerosols like dust), or they can be formed
in the
atmosphere by condensation (secondary
aerosol like
sulfates).
Volcanic eruptions emit
sulfate aerosols via volcanic plumes, which may stay
in the stratosphere for months to years, reflecting sunlight back into space, cooling the Earth's lower
atmosphere or troposphere over a long time...