Elongated open-water areas in sea ice (leads) release sea spray particles to the
atmosphere. However, there is limited knowledge on the amount, properties and drivers of …

Tropospheric reactive bromine (Bry) influences the oxidation capacity of the atmosphere by
acting as a sink for ozone and nitrogen oxides. Aerosol acidity plays a crucial role in Bry …

Polar oceans and sea ice cover 15% of the Earth's ocean surface, and the environment is
changing rapidly at both poles. Improving knowledge on the interactions between the …

Natural aerosols are an important, yet understudied, part of the Arctic climate system.
Natural marine biogenic aerosol components (eg, methanesulfonic acid, MSA) are …

Observed trends in tropospheric ozone, an important air pollutant and short‐lived climate
forcer (SLCF), are estimated using available surface and ozonesonde profile data for 1993 …

The state and fate of snow on sea ice are crucial in the mass and energy balance of sea ice.
The function of atmospheric rivers (ARs) on snow depth over sea ice has not been …

The simulations of upward and downward irradiances by the Integrated Forecasting System
(IFS) of the European Centre for Medium-Range Weather Forecasts are compared with …

Ozone depletion events (ODEs) occur every spring in the Arctic and have implications for the
region's atmospheric oxidizing capacity, radiative balance, and mercury oxidation. Here, we …

Sea ice is an active component of the Earth's climate system, interacting with both the
atmosphere and the ocean. Arctic sea ice is commonly covered by melt ponds during late …

In the polar regions, there is significant model bias in the number concentrations and
seasonality of sea salt aerosol (SSA) due to the lack of understanding of aerosol sources …