The fates of organic
hydroperoxides (ROOHs) in atmospheric condensed
phases are key to understanding the oxidative and toxicological potentials
of particulate matter. Recently, mass spectrometric detection of ROOHs
as chloride anion adducts has revealed that liquid-phase α-hydroxyalkyl
hydroperoxides, derived from hydration of carbonyl oxides (Criegee
intermediates), decompose to geminal diols and H2O2 over a time frame that is sensitively dependent on the water
content, pH, and temperature of the reaction solution. Based on these
findings, it has been proposed that H+-catalyzed conversion
of ROOHs to ROHs + H2O2 is a key process for
the decomposition of ROOHs that bypasses radical formation. In this
perspective, we discuss our current understanding of the aqueous-phase
decomposition of atmospherically relevant ROOHs, including ROOHs derived
from reaction between Criegee intermediates and alcohols or carboxylic
acids, and of highly oxygenated molecules (HOMs). Implications and
future challenges are also discussed.