Less understood — and more difficult to measure — is the influence
of aerosol particles from human sources, particularly the use of coal and other fossil fuels.
Not exact matches
This year, Summit's list
of long - term visitors includes Brandon Strellis, an environmental engineering graduate student
from the Georgia Institute
of Technology studying how
aerosols influence how much energy is reflected and absorbed by Greenland's ice — and where those
particles are coming
from.
Another source
of uncertainty comes
from the direct effect
of aerosols from human origins: How much do they reflect and absorb sunlight directly as
particles?
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
particles.
It then combines with pollutants
from combustion — mainly nitrogen oxides and sulfates
from vehicles, power plants and industrial processes — to create tiny solid
particles, or
aerosols, no more than 2.5 micrometers across, about 1/30 the width
of a human hair.
The research focuses on the power
of minute airborne
particles known as
aerosols, which can come
from urban and industrial air pollution, wildfires and other sources.
These
particles pose health risks to populations, especially to the medically vulnerable, By infusing CATS data directly into
aerosol models, data
from CATS can make a difference in tracking and responding to impacts
of similar events in the future.
By engineering breaking waves
of natural ocean water under purified air in the lab, they were able to isolate and analyze
aerosols from the spray and determine how life within the water altered the chemistry
of the
particles.
The step
from moisture to clouds involves cooling, seed
particles (including pollutant
aerosols) and global wind patterns that blow the moisture
from its place
of origin to its place
of condensation.
That's because scientists have presumed that most
of the
aerosols from minor eruptions do not rise beyond the troposphere, the layer
of Earth's atmosphere where weather occurs and where natural processes quickly clear
particles from the atmosphere.
Now an international team
of researchers led by the lung researcher Marianne Geiser
from the Institute
of Anatomy at the University
of Bern and the
aerosol researcher Josef Dommen
from the Paul Scherrer Institute PSI has shown that secondary
particles from gasoline combustion in Euro 5 engines directly damage lung tissue as well as weaken its defense functions.
Sophisticated microscopic instruments were used to look for iron - containing nanoscale
particles — specifically locating them
from thousands
of 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.
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.
«
From agglomerates of spheres to irregularly shaped particles: Determination of dynamic shape factors from measurements of mobility and vacuum aerodynamic diameters,» Aerosol Science and Technology 40 (3): 197 -
From agglomerates
of spheres to irregularly shaped
particles: Determination
of dynamic shape factors
from measurements of mobility and vacuum aerodynamic diameters,» Aerosol Science and Technology 40 (3): 197 -
from measurements
of mobility and vacuum aerodynamic diameters,»
Aerosol Science and Technology 40 (3): 197 - 217.
Additional
aerosol mass composed
of organosulfate and organonitrate chemicals can then form via nitrogen oxide - initiated oxidation
of VOCs
from natural vegetation (e.g., isoprene) in the presence
of highly acidic ultrafine
particles.
Unfortunately, the exact mechanisms
of interactions between clouds and tiny
aerosol particles from pollution, dust, and soot remained largely a mystery.
Incoming energy, which comes primarily
from the sun, is turned into various forms
of absorbed energy, depending on terrain and atmospheric conditions such as clouds and
aerosol particles.
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.
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.
The organic
aerosol particles that coat the toxic hitchhikers are wafted into the atmosphere through emissions
from trees (like those that produce the smell
of pine trees), and burning biomass and fossil fuel to form a semi-solid sap - like casing surrounding and protecting the
particle's payload
from breaking down 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.
A paper discussing the difficulty
of getting
from nm sized nucleation mode to a size that can generate cloud
particles is: Erupe, M. E., et al. (2010), Correlation
of aerosol nucleation rate with sulfuric acid and ammonia in Kent, Ohio: An atmospheric observation, J. Geophys.
Scientists found that emissions
of tiny air
particles from human - made sources — known as anthropogenic
aerosols — were the cause.
The parameterization
of the interactions are at all levels;
from estimation
of the geometric characterization
of the
aerosols, to the numbers
of particles, to connections with several important aspects
of clouds, and finally to the interactions with radiative energy transport.
Ambient submicron
particle measurements were made with a high - resolution time -
of - flight
aerosol mass spectrometer (AMS) at the north campus
of the University
of California Irvine, which is located in the SoCAB approximately 5 miles inland
from the Pacific Ocean.
It then combines with pollutants
from combustion — mainly nitrogen oxides and sulfates
from vehicles, power plants and industrial processes — to create tiny solid
particles, or
aerosols, no more than 2.5 micrometers across, about 1/30 the width
of a human hair.
In response, the IPCC added a cooling factor to its models
of the atmosphere, consisting
of tiny
aerosol particles produced by the emission
of sulfur dioxide
from electric power plants.
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.
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.»
One positive effect
of burning coal is the formation
of sulfate
aerosol particles which help in reflecting incoming sunlight away
from the earth.
Later, the enhancement
of atmospheric
aerosol particle formation by ions generated
from cosmic rays was proposed as a physical mechanism explaining this correlation.
In principle, at least, the recent results
from the CLOUD project at CERN provide information about the role
of ionizing
particles in «sensitizing» atmospheric
aerosols which might, later, give rise to cloud droplets.
That's because the tiny ash
particles and
aerosols that were blown into the stratosphere spread around the planet, blocking some
of the Sun's rays
from ever reaching Earth.
Fan's most recent paper appeared in Science and investigated the influence
of ultrafine
aerosol particles from urban areas on severe storms.
In the article «Global atmospheric
particle formation
from CERN CLOUD measurements,» sciencemag.org, 49 authors concluded «Atmospheric
aerosol nucleation has been studied for over 20 years, but the difficulty
of performing laboratory nucleation - rate measurements close to atmospheric conditions means that global model simulations have not been directly based on experimental data.....
In the United States, new research
from the City College
of New York on the effects
of particle pollution on weather patterns around Manhattan has shown that
aerosols can either increase or decrease local rainfall, sometimes creating situations where one area will be deluged while a neighboring town will remain dry.
The study, which appeared in a recent issue
of Geophysical Research Letters, used 16 years
of monthly mean observations
from satellites, ground stations, and computer models to look at the relationship between dust
particles in the air, called mineral
aerosols, and cloud properties.
Mishchenko, M.I., I.V. Geogdzhayev, L. Liu, J.A. Ogren, A.A. Lacis, W.B. Rossow, J.W. Hovenier, H. Volten, and O. Muñoz, 2003:
Aerosol retrievals from AVHRR radiances: Effects of particle nonsphericity and absorption and an updated long - term global climatology of aerosol prop
Aerosol retrievals
from AVHRR radiances: Effects
of particle nonsphericity and absorption and an updated long - term global climatology
of aerosol prop
aerosol properties.
Dlugach, Z.M., and M.I. Mishchenko, 2005: The effect
of aerosol shape in retrieving optical properties
of cloud
particles in the planetary atmospheres
from the photopolarimetric data Jupiter.
Warming
from decade to decade can also be affected by human factors such as variations in the emissions,
from coal - fired power plants and other pollution sources,
of greenhouse gases and
of aerosols (airborne
particles that can have both warming and cooling effects).
In addition to the data
from the radiometers, the Berkeley Lab scientists will get supplemental data by taking advantage
of a separate, in - depth DOE climate study at the same location, which is using additional instruments and a balloon - borne sounding system to get information on temperature, cloud cover, the density and types
of aerosols or pollution
particles, heat fluxes and other climate variables like precipitation.
A shortcoming,
from the modern point
of view, is that Broecker did not include other anthropogenic greenhouse gases or
aerosol particles in his calculations.
For atmospheric
aerosol, this shape factor is usually not strongly different
from one; its effect is usually assumed negligible compared to the effect
of particle size, which covers several orders
of magnitude.
Poking around with Scholar, I found mention
of «hydrophobic soot
particles from residential coal and industrial oil burning» and also mention
of radar being used that distinguishes
aerosols from water vapor and clouds.
This work eventually led to investigation
of how planetary cooling might be caused by the
aerosol particles arising
from large - scale fires generated by a nuclear war.
Organic
aerosols are emitted as primary
aerosol particles or formed as secondary
aerosol particles from condensation
of organic gases considered semi-volatile or having low volatility.