aerosol particle

Aerosol particle scattering and absorption can also play a significant role.

However, they emphasize that these aerosol particles can only travel short distances.

Worldwide each year, aerosol particles result in about 800,000 premature deaths.

The aerosol particles form a whitish haze in the sky.

On balance, aerosol particles tend to scatter energy back to space and cool the planet.

Computer models can be used to understand the behaviour of aerosol particles, and are particularly useful in modelling their effect on global climate.

Aerosol particles are eventually deposited from the stratosphere onto land and ocean.

The size of aerosol particles is also crucial, and efforts must be made to ensure optimal delivery.

Yellow areas show plumes in which large and small aerosol particles are intermingling.

A common controlled environment aerosol particle counters are used is a cleanroom.

This is the process by which aerosol particles move randomly due to collisions with gas molecules.

A high proportion of aerosol particles originate from the reactor control rod materials.

Where aerosol particles deposit in the in the respiratory system has a strong influence on their health impact.

The gaseous compounds may be adsorbed on the surface of the aerosol particles.

Deposition of aerosol particles from moving gas streams.

The previous discussion focussed on single aerosol particles.

Clouds are created when water vapor condenses on tiny aerosol particles to form droplets.

The hygroscopicity of the aerosol particles is related to the aerosol composition.

A mass attack using anthrax would require the creation of aerosol particles of 1.5 to 5 micrometres.

By 1985, a three-dimensional configuration was introduced specifically to measure the scattering properties of single aerosol particles.

Fig. 2 Schematic depicting the effect of relative humidity on the size of aerosol particles.

Aerosol particles appear to suppress precipitation, although multiple feedbacks make it difficult to detect this effect.

The particulates may be very finely divided solids or aerosol particles composed of liquid materials.

Aerosols particles and gases mixing with the gaseous components of the flame isolate the fire's fuel.

Following eruptions, these aerosol particles can linger as long as three to four years in the stratosphere.