The marine trace gas dimethylsulfide (DMS) supplies sulfur to the atmosphere at a rate of 15–
40 Tg S per year, contributing to the production of atmospheric sulfate aerosols that …

Motivated by the need to predict how the Arctic atmosphere will change in a warming world,
this article summarizes recent advances made by the research consortium NETCARE …

This paper presents an updated estimation of the bottom-up global surface seawater
dimethyl sulfide (DMS) climatology. This update, called DMS-Rev3, is the third of its kind and …

The CHIMERE chemistry-transport model v2020r1 replaces the v2017r5 version and
provides numerous novelties. The most important of these is the online coupling with the …

Polar environments are among the fastest changing regions on the planet. It is a crucial time
to make significant improvements in our understanding of how ocean and ice …

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

While carbon dioxide is the main cause for global warming, modeling short-lived climate
forcers (SLCFs) such as methane, ozone, and particles in the Arctic allows us to simulate …

A number of studies have examined the size of the allowable global cumulative carbon
budget compatible with limiting twenty-first century global average temperature rise to below …

Hydroperoxymethyl thioformate (HPMTF) is a newly identified major oxidation product of
dimethyl sulfide (DMS). It is speculated that it could act as a major reservoir of marine sulfur …

Dimethylsulfide (DMS), outgassed from ocean waters, plays an important role in the climate
system, as it oxidizes to methane sulfonic acid (MSA) and sulfur dioxide (SO 2), which can …