Aerosol particles affect the Earth's radiative balance by directly scattering and absorbing solar radiation and, indirectly, through their activation into cloud droplets.
While the study provides clear evidence that
aerosol particles affect the development and intensity of storms, Thornton says it can not be directly generalised to the air above land because there are other factors that need to be taken into account.
Not exact matches
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.
Dust devils might
affect Mars's atmosphere by whipping
particles to high altitudes, where the fine
aerosols help control the planet's dry climate.
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.
Soot
particles, also known as black carbon
aerosols,
affect climate by absorbing sunlight, which warms the surrounding air and limits the amount of solar radiation that reaches the ground.
Studying clouds and
aerosols won't just help scientists study the climate, it's also a chance to investigate air quality and how atmospheric
particles affect daily life.
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?
Reactions in and on sea - salt
aerosol particles may have a strong influence on oxidation processes in the marine boundary layer through the production of halogen radicals, and reactions on mineral
aerosols may significantly
affect the cycles of nitrogen, sulfur, and atmospheric oxidants.
The recently published research results provide further evidence that forests can
affect the climate by producing low - volatility vapours that are able to condense and grow
aerosol particles.
Aerosol pollution also
affects the formation of clouds, which are seeded with dust
particles in the atmosphere.
The study, published Wednesday in the journal Nature, showed that the production of tar sands and other heavy oil — thick, highly viscous crude oil that is difficult to produce — are a major source of
aerosols, a component of fine
particle air pollution, which can
affect regional weather patterns and increase the risk of lung and heart disease.
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.
Why It Matters:
Aerosols, tiny airborne
particles of dust and pollution suspended in the atmosphere,
affect the atmosphere and the surface of Earth by scattering and absorbing light.
Additionally, stimulated bacterial degradation might heavily
affect the organic composition of nascent sea - spray
particles, upon which relies the ability of marine
aerosols to interact with the climate system.
Results: Ubiquitous carbon - rich
aerosol particles created by emissions from cars, trees, and other sources alter our climate and
affect air quality.
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.»
«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.»
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.
And how do
aerosols (fine
particles)
affect the formation of clouds?
Unger's analysis is one of the first of its kind to incorporate the multiple effects that
aerosol particles can have on clouds, which
affect the climate indirectly.
The indirect effect is when
aerosol particles act as a cloud condensation nucleus,
affecting the formation and lifetime of clouds.
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).
The mass of a freshly nucleated
aerosol particle is more than 100,000 times smaller than that of an «aged»
aerosol of a size optimal to
affect climate.
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.