The Marginal Ice Zone as a dominant source region of atmospheric mercury during central Arctic summertime
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Arctic mercury flux increased through the Last Glacial Termination with a warming climate
Sources and melt flux of methylmercury in sea ice on the Chukchi Plateau, Arctic Ocean - ScienceDirect
The Marginal Ice Zone as a dominant source region of atmospheric mercury during central Arctic summertime
Mercury isotope evidence for Arctic summertime re-emission of mercury from the cryosphere
Physical map of the Arctic region showing International Arctic Systems
What are the likely changes in mercury concentration in the Arctic atmosphere and ocean under future emissions scenarios? - ScienceDirect
Climate change and mercury in the Arctic: Abiotic interactions - ScienceDirect
Modeling the Mercury Cycle in the Sea Ice Environment: A Buffer between the Polar Atmosphere and Ocean
Arctic mercury flux increased through the Last Glacial Termination with a warming climate
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