«We've found that cosmic rays significantly enhance
the formation of aerosol particles in the mid-troposphere and above.»
CLOUD has also investigated how the 11 - year solar cycle influences
the formation of aerosol particles in our present - day atmosphere.
Not exact matches
She decided to study the role that organic
particles play in cloud droplet
formation, because a large proportion
of marine
aerosols — which have a significant climate impact — are organics.
Their stickiness makes it hard to get them through an inlet into a measuring device, but these compounds may play a significant role in the
formation and alteration
of aerosols, tiny airborne
particles that can contribute to smog or to the nucleation
of raindrops or ice crystals, affecting the Earth's climate.
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.
The team started by looking at the
formation of the very small
particles — a process called
aerosol nucleation — by mimicking atmospheric conditions inside an ultraclean steel «cloud chamber», which Kirkby says is the cleanest ever created.
The question is: Does the current load
of aerosols in the atmosphere already exceed that limit, in which case adding extra
particles should not greatly affect cloud
formation; or do they continue to be a limiting factor as pollution rises, so that added
aerosols would continue to influence the clouds?
Volatility is a key property
of organic
aerosol because it determines the partitioning between the gas and
particle phases, and thus the
formation of SOA
particles.
Aerosol pollution also affects the
formation of clouds, which are seeded with dust
particles in the atmosphere.
Formation of solid and liquid
aerosol particles is increased.
Formation mechanism
of aerosol particles still a big uncertainty in predicting climate change
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.
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.
The CLOUD experiment consists
of a large instrumented chamber in which the atmosphere can be precisely simulated, and the
formation and growth
of aerosol particles and the clouds they seed can be studied under precisely controled atmospheric conditions.
In the atmosphere, where gaseous vapors and
aerosol particles mix, lies the secret
of cloud
formation that scientists are working to unlock.
Aerosol size distribution measurements at four Nordic field stations: identification, analysis and trajectory analysis
of new
particle formation bursts.
Explaining global surface
aerosol number concentrations in terms
of primary emissions and
particle formation.
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.»
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.»
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.
An umbrella term for any small
particle suspended in the atmosphere,
aerosols can be either light or dark, reflective or absorbent
of sunlight, and can enhance or suppress the
formation of cloud droplets.
And how do
aerosols (fine
particles) affect the
formation of clouds?
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.....
The indirect effect is when
aerosol particles act as a cloud condensation nucleus, affecting the
formation and lifetime
of clouds.
Under strict temperature and humidity conditions, investigations in this laboratory provide new information on the particular
aerosol particles that can lead to the
formation of these clouds.
In addition to the complex physics
of fog
formation and transport, recent research suggests that microscopic
aerosol particles may be critical players in fog dynamics and its effect on coastal human and ecological systems.
Recently it was suggested that the
formation of new atmospheric
aerosol particles is connected with the existence
of thermodynamically stable 1 - to 2 - nm clusters, formed in the atmosphere by some nucleation mechanism.
Emissions
of carbon dioxide, methane, nitrous oxide and
of reactive gases such as sulphur dioxide, nitrogen oxides, carbon monoxide and hydrocarbons, which lead to the
formation of secondary pollutants including
aerosol particles and tropospheric ozone, have increased substantially in response to human activities.
While water may not be significant in the
formation of the
aerosols it can play a big role in the growth and evolution
of particles.
Studying the atmospheric
aerosol particles, which impact cloud
formation and
particles, above a pristine forests, researchers discovered that when left alone the Amazon acts as its own «bioreactor»: clouds and precipitation are produced by the abundance
of plant materials.
Topics that I work on or plan to work in the future include studies
of: + missing
aerosol species and sources, such as the primary oceanic
aerosols and their importance on the remote marine atmosphere, the in - cloud and
aerosol water aqueous
formation of organic
aerosols that can lead to brown carbon
formation, the primary terrestrial biological
particles, and the organic nitrogen + missing
aerosol parameterizations, such as the effect
of aerosol mixing on cloud condensation nuclei and
aerosol absorption, the semi-volatility
of primary organic
aerosols, the importance
of in - canopy processes on natural terrestrial
aerosol and
aerosol precursor sources, and the mineral dust iron solubility and bioavailability + the change
of aerosol burden and its spatiotemporal distribution, especially with regard to its role and importance on gas - phase chemistry via photolysis rates changes and heterogeneous reactions in the atmosphere, as well as their effect on key gas - phase species like ozone + the physical and optical properties
of aerosols, which affect
aerosol transport, lifetime, and light scattering and absorption, with the latter being very sensitive to the vertical distribution
of absorbing
aerosols +
aerosol - cloud interactions, which include cloud activation, the
aerosol indirect effect and the impact
of clouds on
aerosol removal + changes on climate and feedbacks related with all these topics In order to understand the climate system as a whole, improve the
aerosol representation in the GISS ModelE2 and contribute to future IPCC climate change assessments and CMIP activities, I am also interested in understanding the importance
of natural and anthropogenic
aerosol changes in the atmosphere on the terrestrial biosphere, the ocean and climate.