Tubex has launched its first aluminium
aerosol can produced neither with lacquer nor ink, the Purity can.
Not exact matches
Then, in 1949, Robert Abplanalp, a 27 - year - old machine - shop operator from the Bronx, gladdened the hearts of whipped - cream lovers everywhere by inventing a cheap, reliable
aerosol -
can valve that could be mass -
produced.
Ball Corporation has won a 2017
Aerosol Dispensing Forum (ADF) Innovation Award for its L'Oreal Men Expert antiperspirant
can,
produced using Ball's ReAl technology.
Experiments Prather and her team conducted in California's Sierra Nevada
produced the first conclusive evidence that dust
aerosols can change the amount of precipitation
produced by clouds.
«This paper is indeed universal, and the conclusions
can apply to the sea spray
produced in oceans or the
aerosols produced above a glass of sparkling wine.»
Current research methods such as ice - core drilling
can produce high - quality records of
aerosols and soot going back centuries and even millennia, he says, and «these written accounts provide a good complement» to the data.
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 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.
If
aerosol quantities are known, they
can of course be compared with how much lightning is later
produced by the cloud in question.
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.
Our proposed mechanism could
produce quite a lot of
aerosol but only future studies
can show the precise impact.
I'm pretty sure you
can get the grey version of that into a strat - cooling / trop - warming situation if you pick the strat absorbers right, but Andy is certainly right that non-grey effects play a crucial role in explaining quantitatively what is going on in the real atmosphere (that's connected with the non-grey explanation for the anomalously cold tropopause which I have in Chapter 4, and also with the reason that
aerosols do not
produce stratospheric cooling, and everything depends a lot on what level you are looking at).
Industrial -
produced cooling
aerosols, without which most climate models can't be made to fit history, are another example.
The hole in the ozone layer over Antarctica was created by human -
produced chlorofluorocarbons (CFCs) that came from things like
aerosol cans and air - conditioners and refrigerators.
Meanwhile, other types of
aerosols, often
produced by burning fossil fuels,
can change surface temperatures by either reflecting or absorbing incoming sunlight.
However, because of its acidity, H2SO4 (and potentially MSA)
can enhance the formation and growth of secondary organic
aerosol (SOA) from organic compounds (5, 44, 45), including those
produced by homogeneous nucleation of low - volatility species (46).
Measurements from ground - based sun photometer networks
can be used both to provide a ground - truth validation of satellite
aerosol retrieval sand to
produce a land - based
aerosol climatology which is complementary to satellite retrievals that currently are being performed mostly over ocean.
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.
Moreover, the semi-direct effect is not exclusive to absorbing
aerosol, as potentially any radiative heating of the mid-troposphere
can produce a similar response in a GCM (Hansen et al., 2005; see also Section 2.8).
Backing that up, NASA says that 1) sea surface temperature fluctuations (El Niño - La Niña)
can cause global temperature deviation of about 0.2 °C; 2) solar maximums and minimums
produce variations of only 0.1 °C, warmer or cooler; 3)
aerosols from natural sources such as volcanic eruptions (Mount Pinatubo for example) have caused average cooling of 0.3 °C, but recent eruptions have had not had significant effect.