Light-absorbing carbonaceous aerosols (LACs), including black carbon and light-absorbing
organic carbon (brown carbon, BrC), have an important role in the Earth system via heating …

Atmospheric ice‐nucleating particles (INPs) play a critical role in cloud freezing processes,
with important implications for precipitation formation and cloud radiative properties, and …

Short‑lived climate forcers (SLCFs) affect climate and are, in most cases, also air pollutants.
They include aerosols (sulphate, nitrate, ammonium, carbonaceous aerosols, mineral dust …

Poor air quality is currently responsible for large impacts on human health across the world.
In addition, the air pollutants ozone (O3) and particulate matter less than 2.5 µm in diameter …

We describe Global Atmosphere 7.0 and Global Land 7.0 (GA7. 0/GL7. 0), the latest science
configurations of the Met Office Unified Model (UM) and the Joint UK Land Environment …

Aerosol forcing uncertainty represents the largest climate forcing uncertainty overall. Its
magnitude has remained virtually undiminished over the past 20 years despite considerable …

We document and evaluate the aerosol schemes as implemented in the physical and Earth
system models, the Global Coupled 3.1 configuration of the Hadley Centre Global …

The Arctic region is a harbinger of global change and is warming at a rate higher than the
global average. While Arctic warming is driven by increases in anthropogenic greenhouse …

Particles formed in the atmosphere via nucleation provide about half the number of
atmospheric cloud condensation nuclei, but in many locations, this process is limited by the …

Abstract Biomass burning emits~ 34–41 Tg yr− 1 of smoke aerosol to the atmosphere.
Biomass burning aerosol directly influences the Earth's climate by attenuation of solar and …