«We developed and implemented new modeling approaches based on laboratory measurements to include shielding of toxics
by organic aerosols in a global atmosphere model that resulted in large improvements of model predictions,» said PNNL scientist Dr. Manish Shrivastava.
Not exact matches
Aerosol nucleation is known to require sulphuric acid, but Kirkby's team found that it is not enough
by itself at low altitudes — the presence of an additional
organic trace vapour is needed (Nature, DOI: 10.1038 / nature10343).
Two important
aerosol species, sulfate and
organic particles, have large natural biogenic sources that depend in a highly complex fashion on environmental and ecological parameters and therefore are prone to influence
by global change.
The results may help to explain discrepancies between observations and theories about how volatile
organic compounds produced
by vegetation are converted into atmospheric
aerosol — especially over forested regions.
By adjusting elements of the test, such as the air exchange rate, which is the number of times per hour indoor air is replaced by outdoor air, as well as the concentrations of terpene and ozone in the chamber, the group was able to ascertain how those variables each affected the formation of secondary organic aerosol
By adjusting elements of the test, such as the air exchange rate, which is the number of times per hour indoor air is replaced
by outdoor air, as well as the concentrations of terpene and ozone in the chamber, the group was able to ascertain how those variables each affected the formation of secondary organic aerosol
by outdoor air, as well as the concentrations of terpene and ozone in the chamber, the group was able to ascertain how those variables each affected the formation of secondary
organic aerosols.
A large portion of secondary
organic aerosols - tiny particles in the air we breathe that contribute to cloud formation and precipitation - arise from a combination of man - made pollution and molecules given off
by plant matter.
CLOUD shows that
organic vapours emitted
by trees produce abundant
aerosol particles in the atmosphere in the absence of sulphuric acid.
Secondary
organic aerosols, or SOAs, are created when hydrocarbon gases, given off
by everything from pine trees to snow blowers, undergo a series of chemical reactions in the atmosphere to produce particles.
Analyses of the ground and aircraft data performed
by Setyan et al. (2012), Shilling et al. (2013), and Kleinman et al. (2016) showed that
organic aerosol production increased when human - caused emissions from Sacramento mixed with air rich in isoprene, an
organic compound wafting from many plants that originate in the area's foothills.
Formation of nitrogen - and sulfur - containing light - absorbing compounds accelerated
by evaporation of water from secondary
organic aerosols
However, because of its acidity, H2SO4 (and potentially MSA) can enhance the formation and growth of secondary
organic aerosol (SOA) from
organic compounds (5, 44, 45), including those produced
by homogeneous nucleation of low - volatility species (46).
Brown clouds contain dark
aerosols such as soot that are released into the atmosphere
by burning
organic matter.
The brownish color of the cloud (which is visible when looking at the horizon) is due to absorption of solar radiation at short wavelengths (green, blue, and UV)
by organic and black carbon
aerosols as well as
by NOx.
New evidence shows that the ocean also acts as a source of
organic matter from biogenic origin -LSB-...] Surface - active
organic matter of biogenic origin -LSB-...] enriched in the oceanic surface layer and transferred to the atmosphere
by bubble - bursting processes, are the most likely candidates to contribute to the observed
organic fraction in marine
aerosol.
It delves into the impacts of
aerosols, which are tiny pollutants of mineral dust, soot and
organic matter emitted
by sources such as power plants, factories and quarries.
...
Aerosol species are grouped
by the parameterization into three basic types: dust and metallic compounds, inorganic black carbon, and insoluble
organic aerosols.
Aerosol «blue haze», as seen here in the Great Smoky Mountains in North Carolina, is formed
by the oxidation of volatile
organic compounds emitted
by trees.
Organic aerosols that are directly injected in the atmosphere in the particulate phase are called primary
organic aerosols (POA), while those that are created
by the oxidation of volatile
organic compounds are known as secondary
organic aerosols (SOA).
International research group shows that the aging of
organic aerosols is caused
by OH radicals
The experiments showed that the mass and composition of
organic aerosols are significantly influenced
by OH radicals.
FIGURE 4 - 1 Annual mean
aerosol optical depth predicted
by an
aerosol chemical transport model due to sulfate, mineral dust, sea salt, and
organic and black carbon
aerosols.
Additional variables also being measured
by Aqua include radiative energy fluxes,
aerosols, vegetation cover on the land, phytoplankton and dissolved
organic matter in the oceans, and air, land, and water temperatures.
This thinning, which can decrease the ozone concentration
by as much as 70 percent, was caused
by the rampant use of human - made chlorofluorocarbons (CFCs),
organic compounds that were once widely used in cooling systems and
aerosols.
Novakov, T., S. Menon, T.W. Kirchstetter, D. Koch, and J.E. Hansen, 2007: Reply to comment
by R.L. Tanner and D.J. Eatough on «
Aerosol organic carbon to black carbon ratios: Analysis of published data and implications for climate forcing».
Theoretically, coatings of essentially non-absorbing components such as
organic carbon or sulphate on strongly absorbing core components such as black carbon can increase the absorption of the composite
aerosol (e.g., Fuller et al., 1999; Jacobson, 2001a; Stier et al., 2006a), with results backed up
by laboratory studies (e.g., Schnaiter et al., 2003).