The new findings help to explain a significant part of the organic
mass of aerosol particles in the air, which had remained mysterious to the scientists so far.
Not exact matches
The findings provide evidence that a 3 - kilometer - deep blanket
of pollution — a
mass of ash, acids,
aerosols, and other
particles — is disrupting weather systems in western Asia.
Thus, when the characteristics
of a water
mass were favourable for reproduction
of microalgae, researchers noticed that after a certain amount
of time, the
aerosols detected above this same water
mass contained more biological
particles.
Additional
aerosol mass composed
of organosulfate and organonitrate chemicals can then form via nitrogen oxide - initiated oxidation
of VOCs from natural vegetation (e.g., isoprene) in the presence
of highly acidic ultrafine
particles.
Mike Alexander, Alex Laskin, Yuri Desyaterik, and John Ortega, who work at DOE's Environmental Molecular Sciences Laboratory (EMSL) at PNNL and Xiao - ying Yu
of PNNL's Atmospheric Science and Global Change Division, collected an extensive set
of measurements
of aerosol mass, size distribution, composition, and
particle morphology using an array
of in - situ techniques and
aerosol sampling approaches.
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 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.
This research is the first to connect a commercial CCN, with a CVI and
mass spectrometers to study the chemistry
of aerosol particles that activate to cloud droplets.
The Single
Particle Soot Photometer (SP2) measures the soot (black carbon)
mass of individual
aerosol particles by laser - induced incandescence down to concentrations as low as ng / m ^ 3.
Ambient submicron
particle measurements were made with a high - resolution time -
of - flight
aerosol mass spectrometer (AMS) at the north campus
of the University
of California Irvine, which is located in the SoCAB approximately 5 miles inland from the Pacific Ocean.
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.
The
Aerosol Chemical Speciation Monitor is a thermal vaporization, electron impact, ionization mass spectrometer that measures bulk chemical composition of the rapidly evaporating component of sub-micron aerosol particles in rea
Aerosol Chemical Speciation Monitor is a thermal vaporization, electron impact, ionization
mass spectrometer that measures bulk chemical composition
of the rapidly evaporating component
of sub-micron
aerosol particles in rea
aerosol particles in real time.
The detailed chemical composition
of exhaust
particles was determined by using a soot
particle aerosol mass spectrometer (SP - AMS).