Why atmospheric nanoparticles grow at similar rates everywhere | HappeningNow.news

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Why atmospheric nanoparticles grow at similar rates everywhere

Large fractions of airborne fine particulate matter consist of secondary organic aerosols (SOA) formed by gas-to-particle conversion of organic precursor molecules in the atmosphere.

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Aerosols significantly affect air quality, human health, clouds and climate, yet the mechanisms of new particle formation in the atmosphere remain unresolved. A substantial portion of fine particulate matter consists of secondary organic aerosols, which arise from the gas‑to‑particle conversion of organic precursor molecules.

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