The Marginal Ice Zone as a dominant source region of atmospheric mercury during central Arctic summertime
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Arctic Ocean: Is It a Sink or a Source of Atmospheric Mercury?
The Marginal Ice Zone as a dominant source region of atmospheric mercury during central Arctic summertime
ACP - Late summer transition from a free-tropospheric to boundary layer source of Aitken mode aerosol in the high Arctic
Climate change and mercury in the Arctic: Abiotic interactions - ScienceDirect
ACP - A full year of aerosol size distribution data from the central Arctic under an extreme positive Arctic Oscillation: insights from the Multidisciplinary drifting Observatory for the Study of Arctic Climate (
What are the likely changes in mercury concentration in the Arctic atmosphere and ocean under future emissions scenarios? - ScienceDirect
Arctic Ocean: Is It a Sink or a Source of Atmospheric Mercury?
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
Stable isotope signatures of Hg in the global atmosphere and the Arctic
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
Shallow methylmercury production in the marginal sea ice zone of the central Arctic Ocean
Overview schematic of Arctic mercury chemical processes represented in
Modeling the Mercury Cycle in the Sea Ice Environment: A Buffer between the Polar Atmosphere and Ocean
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