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 …

Atmospheric aerosol particles serve as condensation nuclei for the formation of both, cloud
droplets and atmospheric ice particles. As a result, they exert a substantial influence on the …

We describe here the development and evaluation of an Earth system model suitable for
centennial-scale climate prediction. The principal new components added to the physical …

The scientific understanding of the Earth's climate system, including the central question of
how the climate system is likely to respond to human-induced perturbations, is …

We describe the HadGEM2 family of climate configurations of the Met Office Unified Model,
MetUM. The concept of a model" family" comprises a range of specific model configurations …

The potentially significant role of the biogenic trace gas dimethylsulfide (DMS) in
determining the Earth's radiation budget makes it necessary to accurately reproduce …

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 …

Seawater concentrations of the climate-cooling, volatile sulphur compound dimethylsulphide
(DMS) are the result of numerous production and consumption processes within the marine …

The oceans contribute significantly to the global emissions of a number of atmospherically
important volatile gases, notably those containing sulfur, nitrogen and halogens. Such gases …

Aerosol processes and, in particular, aerosol‐cloud interactions cut across the traditional
physical‐Earth system boundary of coupled Earth system models and remain one of the key …