Light-absorbing aerosols affect atmospheric radiation, dynamics, and precipitations through
shortwave absorption in the atmosphere and snowpack. Black carbon (BC) is considered …

Black carbon (BC) from anthropogenic and natural sources has a pronounced climatic effect
on the polar environment. The interaction of BC with low-level Arctic clouds, important for …

The atmospheric deposition of soluble (bioaccessible) iron enhances ocean primary
productivity and subsequent atmospheric CO2 sequestration in iron-limited ocean basins …

A key driving factor behind rapid Arctic climate change is black carbon, the atmospheric
aerosol that most efficiently absorbs sunlight. Our knowledge about black carbon in the …

Black carbon (BC) emissions, derived primarily from incomplete fuel combustion,
significantly affect the global and regional climate. Mass absorption efficiency (MAE) is one …

Recent observations show that dust emitted within the Arctic (Arctic dust) has a remarkably
high ice nucleating ability, especially between− 20° C and− 5° C, but its impacts on the …

Black carbon (BC) particles in the Arctic contribute to rapid warming of the Arctic by heating
the atmosphere and snow and ice surfaces. Understanding the source contributions to Arctic …

We investigated long-term changes using a harmonised 22-year data set of aerosol light
absorption measurements, in conjunction with air mass history and aerosol source analysis …

Universal access to clean fuels in household use is one explicit indicator of sustainable
development while currently still billions of people rely on solid fuels for daily cooking …

Mineral dust affects the microphysical and radiative properties of mixed‐phase clouds and
hence the radiative balance of the Earth by acting as ice nucleating particles (INPs) …