Sulfuric acid represents a fundamental precursor for new nanometre-sized atmospheric
aerosol particles. These particles, after subsequent growth, may influence Earth´ s radiative …

Aerosol indirect radiative forcing (IRF), which characterizes how aerosols alter cloud
formation and properties, is very sensitive to the preindustrial (PI) aerosol burden. Dimethyl …

Organic hydrotrioxides (ROOOH) are known to be strong oxidants used in organic synthesis.
Previously, it has been speculated that they are formed in the atmosphere through the gas …

The oxidation of carbonyl sulfide (OCS) is the primary, continuous source of stratospheric
sulfate aerosol particles, which can scatter shortwave radiation and catalyze heterogeneous …

The atmospheric oxidation of dimethyl sulfide (DMS) represents a major natural source of
atmospheric sulfate aerosols. However, there remain large uncertainties in our …

Autoxidation has been acknowledged as a major oxidation pathway in a broad range of
atmospherically important compounds including isoprene and monoterpenes. More recently …

Dimethyl sulfide (DMS) influences climate via cloud condensation nuclei (CCN) formation
resulting from its oxidation products (mainly methanesulfonic acid, MSA, and sulfuric acid …

The intramolecular hydrogen-shift rate coefficient of the CH3SCH2O2 (
methylthiomethylperoxy, MSP) radical, a product formed in the oxidation of dimethyl sulfide …

Dimethyl sulfide (DMS) is an important trace gas emitted from the ocean. The oxidation of
DMS has long been recognised as being important for global climate through the role DMS …

Despite its impact on the climate, the mechanism of methanesulfonic acid (MSA) formation in
the oxidation of dimethyl sulfide (DMS) remains unclear. The DMS+ OH reaction is known to …