Time-Series Trends of Mercury Deposition Network Data

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Time-Series Trends of Mercury Deposition Network Data Peter Weiss 1, David Gay 2, Mark Brigham 3, Matthew Parsons 4, Arnout Ter Schure 5 1 University of California, Santa Cruz, 2 National Atmospheric Deposition Program, 3 U.S. Geological Survey, 4 Environment Canada, 5 Electric Power Research Institute Acknowledgements to: Leonard Levin, Udaysankar Nair, Greg Weatherbee, Dave Lorentz, and Electric Power Research Institute for funding Presented at the 2014 NADP Fall Meeting, Indianapolis, IN

Objectives Initiate work on analyses of spatial gradients and temporal trends in mercury deposition and atmospheric concentrations using data from the Mercury Deposition Network. The primary question addressed is Do the reductions in mercury emissions from EGUs (and other sources) in the United States, driven by MATS and other regulations, especially since 2007, translate into observed changes in: a) mercury concentrations in precipitation and/or b) total annual mercury wet deposition?

MDN Data QA/QC Dry-week and collector-rinse samples, and laboratory quality control (QC) data, supplied by the Mercury Analytical Laboratory (HAL) and USGS Branch of Quality Systems, were evaluated for Hg recovery trends and compared to environmental trends, 1996-2011. Trends in QC data are null or not of sufficient magnitude to explain precipitation Hg concentration temporal trends.

Approach 127 out of 185 Mercury Deposition Network sites selected with data records > 5 years. Trend analyses performed: 1. Seasonal Mann-Kendall ranking system of monthly sums for Precipitation and Hg Deposition, and monthly medians for Hg Concentration. Non-parameteric, does not require normality of input data (Prestbo and Gay, 2009). Calculations independently derived by D. Gay and M. Parsons and results verified. 2. Linear Regression Model Includes precipitation and season to model the variation in [Hg] and uses a Fourier transform to make the data more normally distributed. log[hg] is a function of log[precip] + sine(2*pi*time) + cosine(2*pi*time) + sine(4*pi*time) + cosine(4*pi*t) 3. Linear Regression on Annual Totals and Means Simple linear fit of annual total deposition and precipitation weighted mean concentration data.

MDN Sites with > 5 Years of Data and Assigned Regions Region Number of Sites PC 10 RM 13 PL 15 MW 15 OH 27 SE 23 NE 19

Duration of Data Set for Each Site > 5 Years

Trends in Hg Deposition with Significance Mann-Kendall Procedure Using Monthly Sums of Weekly Data Sites with Signif. (p<0.1) Neg. Trend PC PL OH SE NE BC06 TX50 OH02 FL04 MA01 WA18 PA47 FL97 ME96 PA60 LA10 NB02 NJ30 LA23 NF09 VA08 NC08 PQ05 MD99 Sites with Signif. (p<0.1) Pos. Trend PC RM PL OH SE CA94 WY08 SK12 IN34 FL34 CA20 CO99 OK04 PA30 MS22 OR01 MT05 ON07 LA28 CO96 SC05 White dot = p > 0.1 Black dot = p < 0.1 Adjoining sites with significant trends of opposite direction

Trends in Hg Concentration with Significance Mann-Kendall Procedure Using Monthly Medians of Weekly Data Sites with Signif. (p<0.1) Neg. Trend (green indicates decreasing trend in Hg Dep) PC RM MW OH SE NE CA94 ID03 WI22 OH02 LA10 NB02 WA18 AB14 MN18 IN20 NC08 PQ04 WI99 IN26 GA40 ME96 MN16 MD99 SC19 PQ05 PA72 GA09 NY20 PA60 FL11 ME98 IN28 TN11 NY68 PA00 FL05 ME02 PA47 FL34 MA01 PA13 LA28 NS01 IN34 NC42 NF09 PA37 ME09 PA90 White dot = p > 0.1 Black dot = p < 0.1 Sites with Signif. (p<0.1) Pos. Trend (red indicates increasing trend in HgDep) PC RM PL SE NE CA20 NV02 OK01 SC05 ME00 CO99 OK06 UT97 OK31 KS03 KS05 NE15 KS99

Mean Regional Trends in PWM-Hg Concentration, Precipitation, and Hg Deposition; 3 Method Comparison Mann-Kendall Linear Trend of Annual Totals and PW-Means 4 4 % per yr trend 2 0-2 PC RM PL MW OH SE NE % per yr trend 2 0-2 PC RM PL MW OH SE NE -4-4 HgConc Precip HgDep Linear Transform Model HgConc Precip HgDep Region HgConc Precip HgDep PC - unclear unclear % per yr trend 4 2 0-2 PC RM PL MW OH SE NE RM + + + Agreement by 3 Methods PL + - unclear MW - + + OH - unclear - -4 SE - unclear unclear HgConc Precip HgDep NE - unclear -

Hg Deposition Trends Since 2005 Compared Against the Trend Since 1998 1998 2013 Trends Difference between 2005-2013 and 1998-2013 Trends Trends becoming more positive since 2005 Trends becoming more negative since 2005 Sites shown are those with the longest (1998 2013) data records

Hg Deposition Trends as a Function of Season Difference between spring/summer trend and the all data trend Difference between the fall/winter trend and the all data trend Spring/Summer trend increases: NE, eastern SE, and PC. Fall/Winter trend increases: RM, PL, and western SE.

Hg Deposition Trends as a Function of Precipitation Amount Precip between 15 and 50 mm Precip < 15 mm Precip > 50 mm All Compared to Trends Using All Data Increasing trends in low precip volume range

Point Source Total Hg Emissions > 10 lbs/yr U.S. NEI Data; Canada NPRI Data 2011 Emissions 2011 Emissions 2005 Emissions Some increasing emissions since 2005 Mostly decreasing emissions since 2005

Increasing [Hg] and Hg Dep Trends at CO99 CO99 Mann-Kendall (sums) (%/yr) Linear Transform Model (%/yr) Linear, Annual (%/yr) Hg Conc 4.1 (signif) 7.5 (signif) 7.2 (signif) Hg Dep 7.0 (signif) 10.8 (signif) 9.6 (signif) Precip-weighted mean monthly Hg concentration with linear fit in green Year 4-Corners Power Plant Hg lbs/yr Data Source 2005 544 NEI 2010 367 EPRI indirect 2011 164 NEI 2012 518 EPRI direct

Conclusions Trends in Concentration and Deposition are statistically significant at many sites across the U.S. and Canada. Mann-Kendall and Linear Regression models produced reasonably similar results. From a regional perspective: Hg Deposition and Hg Concentration are decreasing in NE and OH regions. Hg Deposition and Hg Concentration are increasing in RM region. Hg Concentration is decreasing in SE region, but increasing Precipitation is causing Hg Deposition to be slightly increasing. Hg Concentration is strongly increasing in PL region, but decreasing Precipitation is causing Hg Deposition to be only slightly increasing. Trends since 2005 compared to 1998-2013: generally more negative in NE and more positive in MW. Seasonality: Spr/Sum increases in NE, PC and SE; Fall/Win increases in PL, RM. Trends increasing in PL and decreasing in NE for lowest precip. volume samples. CO99 displays strongly positive trends not explained by emissions at local coal-fired power plant.

Hypotheses to be Tested 1. Domestic Hg emissions reductions has led to a measureable decrease in Precipitation [Hg] in the MW, OH, SE, and NE regions. 2. Downward trend in hemispheric background level of GEM in atmosphere is also contributing to the observed Precipitation [Hg] trends. 3. Increasing trend in oxidant concentration in Western North America is contributing to the increasing Precipitation [Hg] trends in the western regions.