The severity and spatial extent of the health impact of anthropogenic mercu
ry (Hg) emission to the atmosphere depend on the emission rate and chemical
form of the emitted species. The few measurements of combustion flue gas g
ive highly variable results about how the emission is divided between the e
lemental (Hg degrees) and reactive forms and are difficult to extrapolate t
o a regional scale. Here we combine measurement of total gaseous mercury (T
GM) and carbon dioxide (CO2) concentrations at a background site in the win
ter with carbon (C) emission inventory to show that at a regional (500 km)
scale, the effective anthropogenic Hg-degrees flux is 41(+/-2) g km(-2) yr(
-1) in the north-east United States. This regional-scale flux was higher un
der clear skies than under cloudy skies, suggesting some removal of Hg degr
ees by cloud water, but the physical mechanisms of the removal are yet to b
e identified.