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

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Last updated 01 abril 2025
The Marginal Ice Zone as a dominant source region of atmospheric mercury during central Arctic summertime
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
The Marginal Ice Zone as a dominant source region of atmospheric mercury during central Arctic summertime
Arctic Ocean's wintertime mercury concentrations limited by seasonal loss on the shelf
The Marginal Ice Zone as a dominant source region of atmospheric mercury during central Arctic summertime
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
The Marginal Ice Zone as a dominant source region of atmospheric mercury during central Arctic summertime
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
The Marginal Ice Zone as a dominant source region of atmospheric mercury during central Arctic summertime
PDF) Mercury isotope evidence for Arctic summertime re-emission of mercury from the cryosphere
The Marginal Ice Zone as a dominant source region of atmospheric mercury during central Arctic summertime
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
The Marginal Ice Zone as a dominant source region of atmospheric mercury during central Arctic summertime
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)
The Marginal Ice Zone as a dominant source region of atmospheric mercury during central Arctic summertime
A review of global environmental mercury processes in response to human and natural perturbations: Changes of emissions, climate, and land use
The Marginal Ice Zone as a dominant source region of atmospheric mercury during central Arctic summertime
Riverine source of Arctic Ocean mercury inferred from atmospheric observations
The Marginal Ice Zone as a dominant source region of atmospheric mercury during central Arctic summertime
a) Time‐series of measured gaseous oxidized mercury (GOM) levels
The Marginal Ice Zone as a dominant source region of atmospheric mercury during central Arctic summertime
Climate change and mercury in the Arctic: Abiotic interactions - ScienceDirect
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