Sulphate pollution from power stations and factory chimneys
produces aerosol particles in the atmosphere which encourage clouds to form.
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.
Not exact matches
Whether these reactions
produce condensing vapours that can condense onto the smallest
particles or even molecules can have strong impacts on
aerosol formation.
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.
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, said co-author and PNNL laboratory fellow Ruby Leung, «strongly suggest that increasing
aerosol concentrations (
particles, mainly soot and sulfur, that pollute the air) in the past has
produced a fog - like haze that has reduced solar radiation (surface heat from sunshine), despite more frequent clear days that should lead to increased solar radiation.»
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.
Airborne
particles in the form of naturally occurring dusts and human -
produced aerosols can serve as ice nuclei, sites around which water vapor condenses into clouds.
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.
We must remember that are a number of
aerosol sources that
produce particles of this size (about 100 nm or 0.1 micron), including anthropogenic ones.
Hansen's group estimates that
aerosols probably counteract about half of the warming
produced by man - made greenhouse gases, but he cautions that better measurements of these elusive
particles are needed.
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.
As the
aerosol particles rise on the warm, convecting air, they
produce more rain over northern India and the Himalayan foothill, which further warms the atmosphere and fuels a «heat pump» that draws yet more warm air to the region.
These fires
produced huge amounts of fine
aerosol particles and trace gases, which can potentially impact the climate and degrade air quality drastically at ground level.
Before a cloud can
produce rain or snow, rain drops or ice
particles must form and
aerosols often serve as the nuclei for condensation.
As this happens, we would probably want a global fleet of aircraft that spray sulfate
particles into the lower atmosphere to make up for the loss of
aerosols once
produced by coal plants.
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.