Not exact matches
Indeed, the reduction in the
emission of precursors to polluting particles (sulphur dioxide) would diminish the concealing effects of Chinese
aerosols, and would speed up warming, unless this effect were to be compensated elsewhere, for instance by significantly
reducing long - life greenhouse gas
emissions and «black carbon.»
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.
Beyond
reducing the volume of acidic particles in
aerosols, cutting the sulfur
emissions has also
reduced the deposition of acids in lakes and waterways, noted Armistead «Ted» Russell, a Regent's Professor in Georgia Tech's School of Civil and Environmental Engineering and another of the paper's co-authors.
Li said the study's findings should further spur countries like China and India to cut
aerosol emissions so they
reduce pollution and thereby increase their solar electricity generation more rapidly, in addition to the already known health benefits.
Professor Sybren said: «It can be excluded, however, that this hiatus period was solely caused by changes in atmospheric forcing, either due to volcanic eruptions, more
aerosols emissions in Asia, or
reduced greenhouse gas
emissions.
Or maybe can the chance distribution of the
aerosol forcing (main
emissions moved from US / Europe to Asia f.e.) used to
reduce the uncertainty of the size of the
aerosol forcing or the factor E?
Within the timescales in which the
aerosols will be
reduced, we can / could also see
reduced CH4
emissions and N2O
emissions which will lead to lower GHG forcing in years rather than decades.
Reducing sulfur
emissions also stops the cooling impact of sulfate
aerosols.
However, as I understand it what is currently the mainstream view is that what explains the transition from early 20th century warming to the flat period between is the resumption of industrial production and thus of reflective
aerosols (predominantly sulfates), and that likewise, it was the passage in the early seventies of laws requiring cleaner
emissions that
reduced reflective
aerosols.
It is likely that at least some of this change, particularly over Europe, is due to decreases in pollution; most governments have done more to
reduce aerosols released into the atmosphere that help global dimming instead of
reducing CO2
emissions.
This relationship between cumulative
emissions and warming is not perfect, as it will change based on what happens to non-CO2 greenhouse gases, such as methane and nitrous oxide, as well as how quickly climate - cooling
aerosols are
reduced.
These scenarios presume that there are no major volcanic eruptions and that anthropogenic
aerosol emissions are rapidly
reduced during the near term.
(Sec. 333) Requires the EPA Administrator to promulgate regulations to
reduce emissions of black carbon (light absorbing
aerosols) or propose a finding that existing CAA regulations adequately regulate such
emissions.
Now, the only way that a business recession could cause a temporary rise in average global temperatures is for the
reduced industrial activity to result in a reduction in the amount of SO2
aerosol emissions into the troposphere.
Nations collectively to begin to
reduce sharply global atmospheric
emissions of greenhouse gases and absorbing
aerosols, with the goal of urgently halting their accumulation in the atmosphere and holding atmospheric levels at their lowest practicable value;
«This study has demonstrated for the first time, using in - situ PM measurements, that
reducing aerosol pollution is driving the Insolation Brightening phenomenon and that the trends in
aerosol pollution, particularly for sulphate
aerosol, is directly linked to anthropogenic
emissions.
In addition, the weakening of the RF of sulphate
aerosol in many regions due to
reduced emissions (Section 2.4.4.1) will be partially balanced by increases in the RF of nitrate
aerosol (e.g., Liao and Seinfeld, 2005).
[note] In this context it intrigues me that those who advocate for stratospheric
aerosol injection (SAI) tend to ignore the possibility that the possible termination effect would increase net risk from greenhouse gas
emissions, and the deployment of SAI should therefore (in risk adjustment terms) justify accelerated mitigation rather than
reduced mitigation.
The control knob for climate change is the amount of dimming sulfur dioxide
aerosol emissions in the atmosphere — the fewer there are, the warmer it gets — and we are
reducing them as fast as we can, thanks to the EPA.
«Comparing the amount of warming in the U.S. saved by
reducing our greenhouse gas
emissions by some 80 % to the amount of warming added in the U.S. by increases in Asian black carbon (soot)
aerosol emissions (at least according to Teng et al.) and there is no clear winner.
Sulphur
emissions from fossil fuel combustion lead to the formation of
aerosols that affect regional climate and precipitation patterns and also
reduce radiative forcing.
The sixth possible component, only to be used as a last resort, would be some form of geo - engineering to probably replace the
aerosols that would be lost as carbon
emissions are
reduced and do not replace the short - term
aerosols.
On one hand, the reduction in global SO2
emissions reduces the role of sulfate
aerosols in determining future climate toward the end of the 21st century and therefore
reduces one aspect of uncertainty about future climate change (because the precise forcing effect of sulfate
aerosols is highly uncertain).
Results of this measurement campaign indicate that alcohol fuels (E85, E100) significantly
reduce both primary particulate
emissions as well as subsequent secondary
aerosol formation in the atmosphere when compared
emissions of gasoline fuels.
The failure to actually
reduce global
emissions has meant that all possibilities are now on the table, including some that sound like premises from a science - fiction novel: Humans could sequester carbon dioxide by removing it from the air through technologies that mimic trees, or we could spray water droplets in the lower atmosphere to reflect light and heat back to space, or we could seed sulfur
aerosols in the stratosphere to do the same.