Temporal Trends in Mercury Wet Deposition Across the U.S. and Canada
Previously Published Material: some of these early results were reported at the National Atmospheric Deposition Meeting 2014 October, but we have moved well beyond these reported results.
Abstract ID#: 36861
Annual rates of change in Hg concentration and Hg deposition rates were calculated using two different methods; (1) the Seasonal Kendall-Mann non-parametric method, and (2) a Fourier transform linear regression parametric method using precipitation depth as an input variable. For this presentation, we will also show results from both methods, where they agree, where they disagree, and potential reasons for this disagreement.
The results from both methods agreed in showing widespread decreasing Hg concentration trends (p<0.05) across most regions in the eastern half of the continent (-0.5 to < -3 %/yr) and significant increasing Hg concentration trends (+1.5 to > +3 %/yr), primarily located in the U.S. Great Plains and Rocky Mountain/Desert regions. Some trends are consistent region-wide, while other regions show significant between–site and –season variation. The downward trend in precipitation Hg concentrations observed at many sites with data beginning before 1998 is becoming significantly less steep in recent years. Finally, best estimates of trends over North America will be provided for use by others.
