The Marginal Ice Zone as a dominant source region of atmospheric mercury during central Arctic summertime

Arctic mercury flux increased through the Last Glacial Termination with a warming climate

Arctic Ocean's wintertime mercury concentrations limited by seasonal loss on the shelf

Schematic of the cycling of mercury in Polar Regions (modified from

The Marginal Ice Zone as a dominant source region of atmospheric mercury during central Arctic summertime

Map of the Arctic Ocean, highlighting sea-ice circulation and export

PDF) Mercury isotope evidence for Arctic summertime re-emission of mercury from the cryosphere

Impact of Changing Arctic Sea Ice Extent, Sea Ice Age, and Snow Depth on Sea Salt Aerosol From Blowing Snow and the Open Ocean for 1980–2017 - Confer - 2023 - Journal

The Marginal Ice Zone as a dominant source region of atmospheric mercury during central Arctic summertime

Model comparison of surface concentrations of elemental mercury, Hg(0)

A review of global environmental mercury processes in response to human and natural perturbations: Changes of emissions, climate, and land use

Riverine source of Arctic Ocean mercury inferred from atmospheric observations

a) Time‐series of measured gaseous oxidized mercury (GOM) levels

Climate change and mercury in the Arctic: Abiotic interactions - ScienceDirect