Interest in stratospheric aerosol and its role in climate have increased over the last decade
due to the observed increase in stratospheric aerosol since 2000 and the potential for …

Volatile organic compounds (VOCs) play a vital role in the global carbon budget and in the
regional formation of ozone in the troposphere, and are emitted from both natural and …

Dimethylsulfide (DMS), a gas produced by marine microbial food webs, promotes aerosol
formation in pristine atmospheres, altering cloud radiative forcing and precipitation. Recent …

Dimethylsulfoniopropionate (DMSP) is a ubiquitous phytoplankton metabolite and the main
precursor of the climate-active gas dimethylsulfide (DMS) in the oceans' surface. Here we …

Earth system models (ESMs) are key tools for providing climate projections under different
scenarios of human-induced forcing. ESMs include a large number of additional processes …

Conspectus The ocean surface serves as a source and sink for a diverse set of reactive
trace gases in the atmosphere, including volatile organic compounds (VOCs), reactive …

Anthropogenic inputs are increasing the CO2 content of the atmosphere, and the CO2 and
total inorganic C in the surface ocean and, to a lesser degree, the deep ocean. The …

Phytoplankton blooms in the Arctic marginal ice zone (MIZ) can be prolific dimethylsulfide
(DMS) producers, thereby influencing regional aerosol formation and cloud radiative forcing …

Marine dimethyl sulfide (DMS) is important to climate due to the ability of DMS to alter Earth's
radiation budget. Knowledge of the global-scale distribution, seasonal variability, and sea-to …

The impacts of natural dimethyl sulfide (DMS) and ship emissions on marine environments
and particulate matter (PM) over the western and southern sea areas around South Korea …