Larger aerosol particles greater than 100 nanometers, such as soot or black carbon, are known to help seed clouds.
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.
Where the atmosphere has few
aerosol particles — over the ocean, for instance — water molecules have fewer
particles to condense around, so cloud droplets are
large.
Plants release gases that, after atmospheric oxidation, tend to stick to
aerosol particles, growing them into the
larger - sized
particles that reflect sunlight and also serve as the basis for cloud droplets.
Two important
aerosol species, sulfate and organic
particles, have
large natural biogenic sources that depend in a highly complex fashion on environmental and ecological parameters and therefore are prone to influence by global change.
«
Particles of any kind, even much smaller than the wavelength of visible light, will, as a rule, make the sky brighter but at the expense of its purity of color,» Bohren says, noting that the effect is more pronounced when there is a high concentration of
large aerosols.
* Yellow areas show where
large and small
aerosol particles are mixing.
Therefore, considering the
large contribution of these
particles to the
aerosol mass concentration in the atmosphere and the importance of the INPs, we study the ability of these
particles as INPs by immersion freezing mode.
Because small - scale climate features, such as clouds and atmospheric
aerosol particles, have a
large impact on global climate, it's important to improve the methods used to represent those climate features in the models.
Because much of Earth's land mass is covered by plants, there is a
large source of these biogenic
aerosol particles that need to be accounted for in climate change prediction.
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 this case,
large amounts of sulphate
aerosols (small
particles) are injected into the stratosphere by
large explosive eruptions (the most recent one being Mt. Pinatubo in 1991).
According to «Atmospheric
particles and nuclei» by Götz et al. (1991), Junge (1963) proposed on the basis of
aerosol measurements that «
large» and «giant»
particles (radius greater than 0.1 micro-meter) constitute the majority of CCN, independently of their chemical composition.
My question is: does the retroreflectivity of the
larger droplets, i.e. back towards the light source, play into the sulfur
aerosol issue or is it simply averaged out by the bulk effect of all the
aerosol particles present in the apparently white haze?
The Muchachas project looked at organic
aerosols, which constitute the
largest proportion of chemical airborne
particles.
While the standard suit of instruments deployed at the ground site (Eastern North Atlantic, ENA) can measure
particle sizes between 2.5 nm and 1 um (using the Scanning Mobility Particle Sizer, SMPS and the Ultra-High Sensitivity Aerosol Spectrometer, UHSAS), there is still a need to measure larger pa
particle sizes between 2.5 nm and 1 um (using the Scanning Mobility
Particle Sizer, SMPS and the Ultra-High Sensitivity Aerosol Spectrometer, UHSAS), there is still a need to measure larger pa
Particle Sizer, SMPS and the Ultra-High Sensitivity
Aerosol Spectrometer, UHSAS), there is still a need to measure
larger particles.
Large volcanic eruptions eject sulfur dioxide, which rapidly forms tiny
particles in the air known as «
aerosols» that block sunlight.
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.