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Observations of Mercury Species and Halogens at Summit, Greenland Steve Brooks 1 , J. Dibb 2 , J. Stutz 3 , R. von Glascow 4 , G. Huey 5 , B. Lefer 6 , G. Chen 7 , and D. Lew 1 NOAA ESRL Global Monitoring Annual Conf. May 15, 2008 1 NOAA ARL 2 Univ.


  1. Observations of Mercury Species and Halogens at Summit, Greenland Steve Brooks 1 , J. Dibb 2 , J. Stutz 3 , R. von Glascow 4 , G. Huey 5 , B. Lefer 6 , G. Chen 7 , and D. Lew 1 NOAA ESRL Global Monitoring Annual Conf. May 15, 2008 1 NOAA ARL 2 Univ. of New Hampshire 3 UCLA 4 Univ. of East Anglia 5 Georgia Tech 6 University of Houston 7 NASA Langley Study Funded by NSF

  2. G-SHO x Summer 2007 Greenland – Summit Halogens and HO x Species Method Research Group Hg (GEM, RGM, FPM) Tekran NOAA - Brooks OH, RO 2 , H 2 SO 4 CIMS Ga. Tech HCl, HO 2 NO 2 , CIMS Ga. Tech BrO,SO 2 , etc BrO, HCHO DOAS UCLA - Stutz Soluble Gases Mist UNH - Dibb Chamber Br - , Cl - , etc. Radiation, J-values Spectrom. UH - Lefer Whole Air Samples GC-MS UCI – Blake NO, O 3 , Dewpoint, etc commercial

  3. Polar Chemistry • Br 2 + h ν => 2Br • Br + O 3 => BrO + O 2 • BrO + h ν => Br + O ‘very fast • Br + Hg => HgBr ‘ Hg(I) radical precursor to RGM Hg(II) • HgBr => Hg + Br ‘ Dominates at Temps. > 0 C or • HgBr + X => HgBrX ‘ X = Br, OH, … • RGM Hg(II) formation mechanism rate doubles for every 6 degree C drop in temperature below 0 ° C (Goodsite et al., 2004; Holmes et al., 2006) • Bromine is recycled in the surface snow

  4. from S. Marcy Mercury Emissions – 1995 (t/y) • Hg is released through coal burning, waste incineration 1475 t and industry • Stationary fossil fuel 325t 29 t combustion accounts 164 t 133 t 109 t for 66% of Hg emitted • In addition, there are fossil fuel non-ferrous natural sources – cement waste Volcanoes, enriched iron-steel other soils

  5. Gaseous Elemental Mercury • Comprises ~95% of Atmospheric Mercury • Atmospheric lifetime ~6 mo. -1 year • Removed by direct deposition or oxidation • Many natural and anthropogenic sources (volcanoes, enriched soils, coal combustion, etc.)

  6. Reactive Gaseous Mercury • Operational defined as mercury collected by a KCl coated denuder tube • Typically believed to be dominated by Hg(II) such as HgCl 2 , HgBrX • Typically rare in the lower troposphere 1-2 pg/m 3 (sub-parts per trillion levels) • Short lifetime (hours) in the near-surface air – dry deposits quickly (similar to nitric acid) • Water soluble – wet deposits

  7. BARROW Brooks et al GRL 2006 800 24 S hore Lead R efreezing S hore Lead R efreezing 700 21 RGM (ng m-3) Ozone (ppb * 600 1 8 500 1 5 BrO (ppt) R G M 10) 400 1 2 O zo n e B rO 300 9 200 6 1 00 3 0 0 84 85 86 87 88 89 90 91 92 93 94 95 96 97 100% 50% 19% 0% 100% 69% 67% 0% 0% 100%100%100%100% Julian day 2003 P ercentage tim e 48-hour back trajectory was over sea ice

  8. South Pole Averages of High Volume Filters, Brooks et al. Atmos. Environ. 2008 25 1800 1600 Filterable Hg (pg m-3) Solar Elevation (deg) 20 1400 1200 15 1000 800 10 600 400 5 200 0 0 1-Jan 20-Feb 11-A pr 31-M ay 20-Jul 8-S ep 28-O ct 17-D ec

  9. Mercury speciation at Summit 2007 GEM – Gaseous Elem Hg, RGM – Reactive Gaseous Hg, FPM – Fine Particulate Hg 350 4 Peak Solar 3.5 300 3 RGM or FPM pg m-3 250 RGM 2.5 GEM ng m-3 200 GEM 2 150 1.5 100 1 50 0.5 FPM 0 0 5/14/07 0:00 5/15/07 0:00 5/16/07 0:00 5/17/07 0:00 5/18/07 0:00 5/19/07 0:00

  10. Mercury speciation at Summit 2007 GEM – Gaseous Elem Hg, RGM – Reactive Gaseous Hg, FPM – Fine Particulate Hg 350 4 Peak Solar 3.5 300 3 RGM or FPM pg m-3 250 RGM 2.5 GEM ng m-3 200 GEM 2 150 1.5 100 1 50 0.5 FPM 0 0 5/14/07 0:00 5/15/07 0:00 5/16/07 0:00 5/17/07 0:00 5/18/07 0:00 5/19/07 0:00

  11. 67 300 Daily peak solar 66 250 65 200 R G M p g m - 3 64 O z o n e p p b 63 150 62 100 61 RGM 50 60 Ozone 59 0 5/16/07 0:00 5/16/07 5/17/07 0:00 5/17/07 5/18/07 0:00 5/18/07 5/19/07 0:00 12:00 12:00 12:00

  12. Fluxes Hg o + Br => HgBr => Reactive Gaseous Mercury, HgBrX Photoreduction Gaseous Elemental Mercury, Hg o Snow Surface

  13. Hour averages 5/13 - 5/19 250 1.8 1.7 Peak Solar 200 1.6 RG M or FPM pg m -3 1.5 G EM ng m -3 RGM 150 1.4 GEM 1.3 100 1.2 1.1 50 1 FPM 0.9 0 0.8 0 2 4 6 8 10 12 14 16 18 20 22 24 Hour of Day

  14. Hour averages all data 5/9 - 6/17 80 1.8 Peak Solar 70 1.6 RG M or FPM pgm -3 60 RGM G EM ng m -3 50 1.4 GEM 40 1.2 30 FPM 20 1 10 0 0.8 0 2 4 6 8 10 12 14 16 18 20 22 24 Hour of day

  15. Summit, Greenland Jack Dibb UNH

  16. 4.5 180 Daily Peak Solar 4 160 BrO 3.5 140 3 120 2.5 100 2 80 1.5 60 RGM 1 40 0.5 20 0 0 6/7/2007 0:00 6/8/2007 0:00 6/9/2007 0:00 6/10/2007 0:00 6/11/2007 0:00 6/12/2007 0:00

  17. Summit Vs. Barrow • Barrow • Summit • BrO 0-40 ppt • BrO 0-5 ppt • Hg o Depletions • Hg o Drops 10% • Surface O 3 Depletions • O 3 Drops by 5ppb • Hg in snow released • Hg in snow to melt water sequestered at depth • Bromine primarily • Bromine primarily from local sea ice from snow pack formation recycling

  18. Global Implications • Barrow and the coastal Polar Regions – Mercury is preferentially deposited (net 100-200 tons/year) and is added to the mercury burden in biota • Antarctic Polar Plateau – deposited mercury buried by snow sequesters 60 metric tons per year at depth (Brooks et al. Atmos Envir. 2008) • Greenland Ice Sheet – due to more rapid burial sequesters ~38 metric tons per year Anthropogenic Emissions are 1500 metric tons/year Sequestration is total Hg buried below 1m All US coal combustion emissions are 48 tons/year

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