Leon, M. Sorokin, and I. Slutsker, 2006: Application of spheroid models to account
for aerosol particle nonsphericity in remote sensing of desert dust.
The specialized instruments onboard the aircraft sampled the plume
for aerosol particle size distribution and composition as well as concentrations of pollutant gases such as sulfur dioxide, nitric oxide, nitrogen dioxide, ozone, and volatile organic compounds (VOCs).
What's more, according to Tim Bates of the National Oceanic and Atmospheric Administration (NOAA), «there's a very wide range of sizes [
for aerosol particles], and the effect that the particle is going to have on climate is going to be very dependent on its size, which makes it trickier.»
I haven't seen any estimates from him as to the expected residence times
for the aerosol particles, except in a presentation where it seemed he was thinking they would last two seasons.
Not exact matches
For the study, Dr. Toohey and his colleagues from GEOMAR and the Max Planck Institute for Meteorology in Hamburg have used an aerosol - climate model to track 70 different eruption scenarios while analyzing the distribution of the sulfur particl
For the study, Dr. Toohey and his colleagues from GEOMAR and the Max Planck Institute
for Meteorology in Hamburg have used an aerosol - climate model to track 70 different eruption scenarios while analyzing the distribution of the sulfur particl
for Meteorology in Hamburg have used an
aerosol - climate model to track 70 different eruption scenarios while analyzing the distribution of the sulfur
particles.
After allowing
for humidity and rainfall, they found that «
aerosol optical thickness» — a measure of the concentration of atmospheric
particles — decreased by only 10 to 15 per cent compared with the same periods in 2002 to 2007 (Geophysical Research Letters, in press).
For example, the tiny
particles known as
aerosols are far better understood, says atmospheric scientist Piers Forster of the University of Leeds in England andalso a lead author.
Ozone, methane and
aerosols (tiny pollutant
particles) remain in the atmosphere
for a shorter time than CO2, but can affect both the climate and air quality.
It has been known
for several years that sulfuric acid contributes to the formation of tiny
aerosol particles, which play an important role in the formation of clouds.
Aerosol particles influence Earth's climate through cloud formation: Clouds can only form if so - called cloud condensation nuclei (CCN) are present, which act as seeds
for condensing water molecules.
Where the atmosphere has few
aerosol particles — over the ocean,
for instance — water molecules have fewer
particles to condense around, so cloud droplets are large.
Such sulfuric acid
aerosols are already responsible
for the bulk of nacreous clouds that form in the polar stratosphere; added
particles would just amp up the natural process (although it might also amp up damage the ozone layer).
And the way those droplets form - with scarce or plentiful
aerosol particles - could have serious implications
for weather and climate change.
Black carbon
aerosols —
particles of carbon that rise into the atmosphere when biomass, agricultural waste, and fossil fuels are burned in an incomplete way — are important
for understanding climate change, as they absorb sunlight, leading to higher atmospheric temperatures, and can also coat Arctic snow with a darker layer, reducing its reflectivity and leading to increased melting.
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.»
Thus, when the characteristics of a water mass were favourable
for reproduction of microalgae, researchers noticed that after a certain amount of time, the
aerosols detected above this same water mass contained more biological
particles.
Plants release gases that, after atmospheric oxidation, tend to stick to
aerosol particles, growing them into the larger - sized
particles that reflect sunlight and also serve as the basis
for cloud droplets.
Atmospheric
aerosols (solid or liquid
particles suspended in the atmosphere) are difficult to examine
for various reasons.
A newly developed
aerosol deposition chamber also allowed
for the
particles to be realistically deposited on cell cultures from healthy and diseased airways.
Sophisticated microscopic instruments were used to look
for iron - containing nanoscale
particles — specifically locating them from thousands of
aerosol particles.
The results show
for the first time
for a number of natural compounds, which together account
for around 70 per cent of the biological hydrocarbon emissions, how much each compound produces low - volatility products and how they can possibly affect the climate via producing
aerosol particles.
IPCC scientists have suspected
for a decade that
aerosols of smoke and other
particles from burning rainforest, crop waste and fossil fuels are blocking sunlight and counteracting the warming effect of carbon dioxide emissions.
Mikhailov, E., Vlasenko, S., Martin, S.T., Koop, T., and Pöschl, U.: Amorphous and crystalline
aerosol particles interacting with water vapour: conceptual framework and experimental evidence
for restructuring, phase transitions and kinetic limitations, Atmospheric Chemistry and Physics, 9, 9491 - 9522, 2009.
, Kilcoyne, A.L.D., Moffet, R.C., Weigand, M., Martin, S.T., Pöschl, U., and Andreae, M.O.: Biogenic potassium salt
particles as seeds
for secondary organic
aerosol in the Amazon, Science, 337, 1075 - 1078, 2012.
During ISDAC, they collected an unprecedented level of data and detailed observations on Arctic clouds and
aerosols, those tiny
particles in the atmosphere that act as seeds
for cloud droplets and ice crystals.
Possible reasons revolve around tiny natural and manmade
particles called
aerosols that serve as seeds
for cloud droplets to form around.
Global climate models are essential tools
for understanding climate change and
for developing policy regarding future emissions of greenhouse gases, primary
aerosol particles, and
aerosol precursor gases.
One of those complex interactions is
aerosols, the microscopic
particles of dust, soot, and chemicals dispersed in the atmosphere that scatter or absorb sunlight and act as seeds
for cloud formation.
Because much of Earth's land mass is covered by plants, there is a large source of these biogenic
aerosol particles that need to be accounted
for in climate change prediction.
ERICA, a worldwide unique
aerosol particle mass spectrometer was designed and constructed in Mainz specifically
for these research flights aboard the M - 55 Geophysika.
These have garnered more than 600 citations advancing our understanding of what the research field calls secondary organic
aerosols — or SOA
for short — and how the carbon - containing
aerosol particles mix in the atmosphere.
In the middle of the last century,
for example, soot and other
particles spewing from factory smokestacks, collectively known as
aerosols — cooled the planet
for a couple of decades.
The paper describes and evaluates CAM5, the advanced
aerosol module
for the Community Earth System Model, which provides a clearer picture of these atmospheric
particles.
Press release (emphases added):... scientists have succeeded
for the first time in directly observing that the electrically charged
particles coming from space and hitting the atmosphere at high speed contribute to creating the
aerosols that are the prerequisites
for cloud formation.
As
for Pinatubo
aerosols, the residence time
for such
particles is around 3 to 4 years before they are advected / settle out the stratosphere — there are effectively none left.
After each of these eruptions we have noted the presence of (generally) submicrometer - sized ash
particles and
aerosol droplets on collectors, although we can not always be certain of the identity of the volcano responsible
for the material.
We also know quite accurately the spectral absorption characteristics
for the absorbing gases, and how cloud and
aerosol particles interact with thermal radiation.
«We're trying to understand what the connection is between a cosmic ray going through the atmosphere and the creation of so - called
aerosol seeds — the seed
for a cloud droplet or an ice
particle,» Kirkby explains.
I write it off as a very real effect that is not well characterized by the models, probably because these models don't model with enough accuracy the effect of the additional
aerosol particles on cloud production to properly account
for it's full effect on temperature.
The remainder is made up with the other minor greenhouse gases, ozone and methane
for instance, and a small amount from
particles in the air (dust and other «
aerosols»).
But the team found that the smoke and cloud layers are closer together than expected so that
aerosol particles from the smoke act as nuclei
for cloud droplets to form around.
nevertheless, both states can coexist
for a wide range of environmental conditions.5, 7
Aerosols, liquid or solid
particles suspended in the atmosphere, serve as Cloud Condensation Nuclei (CCN) and therefore affect the concentration of activated cloud droplets.8 Changes in droplet concentration affect key cloud properties such as the time it takes
for the onset of significant collision and coalescence between droplets, a process critical
for rain formation.»
For the first time, researchers have developed a comprehensive approach to look at
aerosols — those fine
particles found in pollution — and their effect on clouds and climate.
Aerosols, liquid or solid
particles suspended in the atmosphere, serve as Cloud Condensation Nuclei (CCN) and therefore affect the concentration of activated cloud droplets.8 Changes in droplet concentration affect key cloud properties such as the time it takes
for the onset of significant collision and coalescence between droplets, a process critical
for rain formation.»
It is found that with a number concentration of
aerosol particles of ∼ 102 — 103 cm − 3 (which corresponds to the
aerosol density in the deposited layer of about 1 — 10 mg / m2 with the layer thickness along the ray path of about 100 m) the solar radiation attenuation with artificial
aerosol layers accounts
for 1 to 10 %.
Several proposals call
for injecting microscopic
particles, called
aerosols, into the stratosphere, the quiet region of the atmosphere above the troposphere about 18 kilometers up from the equator.
«The results also show that ionisation of the atmosphere by cosmic rays accounts
for nearly one - third of all
particles formed, although small changes in cosmic rays over the solar cycle do not affect
aerosols enough to influence today's polluted climate significantly.»
This method uses consistency between direct normal and diffuse horizontal measurements together with a special regression technique
for retrieval of daily time series of column mean
aerosol particle size,
aerosol optical depth, NO2, ozone and water vapor column amounts together with the instrument's calibration constants.
Airborne Open Polar / Imaging Nephelometer
for Ice
Particles in Cirrus Clouds and
Aerosols Field Campaign Report.
These NCA emissions directly affect
particle concentrations and human exposure to nanosized
aerosol in urban areas, and potentially may act as nanosized condensation nuclei
for the condensation of atmospheric low - volatile organic compounds.