Acidity is one central
parameter in atmospheric multiphase reactions,
influencing aerosol formation and its effects on climate, health,
and ecosystems. Weak acids and bases, mainly CO
2
, NH
3
, and organic acids, are long considered to play a role in
regulating atmospheric acidity. However, unlike strong acids and bases,
their importance and influencing mechanisms in a given aerosol or
cloud droplet system remain to be clarified. Here, we investigate
this issue with new insights provided by recent advances in the field,
in particular, the multiphase buffer theory. We show that, in general,
aerosol acidity is primarily buffered by NH
3
, with a negligible
contribution from CO
2
and a potential contribution from
organic acids under certain conditions. For fogs, clouds, and rains,
CO
2
, organic acids, and NH
3
may all provide
certain buffering under higher pH levels (pH > ∼4). Despite
the 10
4
to 10
7
lower abundance of NH
3
and organic weak acids, their buffering effect can still be comparable
to that of CO
2
. This is because the cloud pH is at the
very far end of the CO
2
multiphase buffering range. This
Perspective highlights the need for more comprehensive field observations
under different conditions and further studies in the interactions
among organic acids, acidity, and cloud chemistry.