Aerosol-cloud interaction
contributes to the largest uncertainties
in the estimation and interpretation of the Earth’s changing
energy budget. The present study explores experimentally the impacts
of water condensation-evaporation events, mimicking processes occurring
in atmospheric clouds, on the molecular composition of secondary organic
aerosol (SOA) from the photooxidation of methacrolein. A range of
on- and off-line mass spectrometry techniques were used to obtain
a detailed chemical characterization of SOA formed in control experiments
in dry conditions, in triphasic experiments simulating gas-particle-cloud
droplet interactions (starting from dry conditions and from 60% relative
humidity (RH)), and in bulk aqueous-phase experiments. We observed
that cloud events trigger fast SOA formation accompanied by evaporative
losses. These evaporative losses decreased SOA concentration in the
simulation chamber by 25–32% upon RH increase, while aqueous
SOA was found to be metastable and slowly evaporated after cloud dissipation.
In the simulation chamber, SOA composition measured with a high-resolution
time-of-flight aerosol mass spectrometer, did not change during cloud
events compared with high RH conditions (RH > 80%). In all experiments,
off-line mass spectrometry techniques emphasize the critical role
of 2-methylglyceric acid as a major product of isoprene chemistry,
as an important contributor to the total SOA mass (15–20%)
and as a key building block of oligomers found in the particulate
phase. Interestingly, the comparison between the series of oligomers
obtained from experiments performed under different conditions show
a markedly different reactivity. In particular, long reaction times
at high RH seem to create the conditions for aqueous-phase processing
to occur in a more efficient manner than during two relatively short
cloud events.