We can not eliminate the possibility that slow evolution of environmental conditions (e.g., surface temperature and irradiation) and snow composition (e.g., sea salts levels) induced slight evolution in chemical processes involving GEM in the shallow
firn during recent decades.
Hence, atmospheric GEM concentrations inferred from Greenland
firn air and global anthropogenic Hg emissions have exhibited consistently similar trends
during the most
recent decades (Fig. 2), suggesting that the atmospheric reservoir of mercury at mid - and high - northern latitudes has been driven mainly by anthropogenic emissions
during the last
decades.