Secondary organic aerosol (SOA) particles can scatter radiation and act as cloud condensation nuclei, and thereby influence the Earth's radiation balance. It is generally assumed that SOA particles are liquid, but these authors show that they can adopt an amorphous solid state under ambient conditions. The findings challenge traditional views of the kinetics and thermodynamics of SOA formation and transformation in the atmosphere.
- Annele Virtanen
- Jorma Joutsensaari
- Ari Laaksonen
