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

Ocean biogeochemistry involves the production and consumption of an array of organic
compounds and halogenated trace gases that influence the composition and reactivity of the …

The climate active trace-gas carbonyl sulfide (OCS) is the most abundant sulfur gas in the
atmosphere. A missing source in its atmospheric budget is currently suggested, resulting …

Reactive atmospheric halogens destroy tropospheric ozone (O3), an air pollutant and
greenhouse gas. The primary source of natural halogens is emissions from marine …

An accurate quantification of surface emissions and of their evolution over time is essential
to understand and simulate the composition of the atmosphere and its trends. This chapter …

This study investigates the impact of reactive halogen species (RHS, containing chlorine
(Cl), bromine (Br) or iodine (I)) on atmospheric chemistry in the tropical troposphere and …

The first concerted multi-model intercomparison of halogenated very short-lived substances
(VSLS) has been performed, within the framework of the ongoing Atmospheric Tracer …

We quantify the stratospheric injection of brominated very short‐lived substances (VSLS)
based on aircraft observations acquired in winter 2014 above the Tropical Western Pacific …

Ozone depletion events (ODEs) in the polar boundary layer have been observed frequently
during springtime. They are related to events of boundary layer enhancement of bromine …

Halogenated very short-lived substances (VSLSs) are naturally produced in the ocean and
emitted to the atmosphere. When transported to the stratosphere, these compounds can …