Simulations of Atmospheric Mercury with the NOAA HYSPLIT Model Mark Cohen, Roland Draxler, Winston Luke, Paul Kelley, and Richard Artz NOAA Air Resources.

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Presentation transcript:

Simulations of Atmospheric Mercury with the NOAA HYSPLIT Model Mark Cohen, Roland Draxler, Winston Luke, Paul Kelley, and Richard Artz NOAA Air Resources Laboratory, Silver Spring, MD, Symposium on Atmospheric Modeling and Application of GIS and Scientific Visualization Technologies for Risk Assessment July 30-31, 2009, Jackson State University In collaboration with Anjaneyulu Yerramilli, Jerzy Leszczynski, Hari Dasari, Rao V.B. Dodla, Chuck Patrick, Robert Hughes, Julius Baham, Shelton Swanier, and other colleagues at Jackson State University

Public Health Context  Methyl-mercury is a developmental neurotoxin -- risks to fetuses/infants  Uncertainties, but mercury toxicity relatively well understood well-documented tragedies: (a) Minimata (Japan) ~1930 to ~1970; (b) Basra (Iraq), 1971 epidemiological studies, e.g., (a) Seychelles; (b) Faroe Islands; (c) New Zealand methylmercury vs. Omega-III Fatty Acids selenium – protective role?  Cardiovascular toxicity might be even more significant (CRS, 2005)  At current exposures, risk to large numbers of fetuses/infants + Wildlife Health Issues e.g., fish-eating birds  Critical exposure pathway: methylmercury from fish consumption  Widespread fish consumption advisories

Elemental Mercury -- Hg(0) most of total Hg in atmosphere not very water soluble doesn’t easily dry or wet deposit upward evasion vs. deposition atmos. lifetime approx ~ yr globally distributed Particulate Mercury -- Hg(p) a few percent of total atmos Hg not pure particles of mercury Hg compounds in/on atmos particles species largely unknown (HgO?) atmos. lifetime approx 1~ 2 weeks local and regional effects bioavailability? Reactive Gaseous Mercury -- RGM a few percent of total atmos Hg oxidized Hg (HgCl2, others) operationally defined very water soluble and “sticky” atmos. lifetime <= 1 week local and regional effects bioavailable Atmospheric methyl-mercury? Different “forms” of mercury in the atmosphere

emissions of Hg(0), Hg(II), Hg(p) Hg from other sources: local, regional & more distant wet and dry deposition to the watershed wet and dry deposition to the water surface  Enhanced oxidation of Hg(0) to RGM  Enhanced deposition Reactive halogens in marine boundary layer Source Attribution for Deposition?

color of symbol denotes type of mercury source coal-fired power plants other fuel combustion waste incineration metallurgical manufacturing & other size/shape of symbol denotes amount of mercury emitted (kg/yr) – U.S. data from USEPA National Emissions Inventory (NEI); 2002 Canadian data from Environment Canada; 1999 Mexican data from inventory prepared by Acosta y Asociados for the Commission for Environmental Cooperation Elemental Mercury -- Hg(0) -- Emissions to the Air

color of symbol denotes type of mercury source coal-fired power plants other fuel combustion waste incineration metallurgical manufacturing & other size/shape of symbol denotes amount of mercury emitted (kg/yr) – U.S. data from USEPA National Emissions Inventory (NEI); 2002 Canadian data from Environment Canada; 1999 Mexican data from inventory prepared by Acosta y Asociados for the Commission for Environmental Cooperation Reactive Gaseous Mercury – RGM -- Emissions to the Air

color of symbol denotes type of mercury source coal-fired power plants other fuel combustion waste incineration metallurgical manufacturing & other size/shape of symbol denotes amount of mercury emitted (kg/yr) – U.S. data from USEPA National Emissions Inventory (NEI); 2002 Canadian data from Environment Canada; 1999 Mexican data from inventory prepared by Acosta y Asociados for the Commission for Environmental Cooperation Particulate Mercury -- Hg(p) -- Emissions to the Air

color of symbol denotes type of mercury source coal-fired power plants other fuel combustion waste incineration metallurgical manufacturing & other size/shape of symbol denotes amount of mercury emitted (kg/yr) – U.S. data from USEPA National Emissions Inventory (NEI); 2002 Canadian data from Environment Canada; 1999 Mexican data from inventory prepared by Acosta y Asociados for the Commission for Environmental Cooperation Total Mercury Emissions to the Air [ Hg(0) + RGM + Hg(p) ]

Logarithmic Why is emissions speciation information critical? NOTE: distance results averaged over all directions – Some directions will have higher fluxes, some will have lower

’s ’s: many mercury-cell chlor-alkali plants converted to alternate processes or closed due to regulatory and other pressures 2002 – Clear Skies Initiative for power plants introduced (ultimately withdrawn) Clean Air Act Amendments of 1990 – calls for Maximum Achievable Control Technology (MACT) to regulate hazardous air pollutants; intent is to prohibit emissions trading for these air toxics 1990’s – Hg emissions from municipal and medical waste incinerators fall dramatically due to:  closure of some municipal waste incinerators and many medical waste incinerators  MACT-related pollution control requirements  reduction in mercury content of waste (e.g., battery legislation) 2005 – CAIR (Clean Air Interstate Rule) for power plants (Hg reduced as co-benefit of SO 2 & NO x controls) 2005 – EPA meets court-ordered deadline and promulgates CAMR (Clean Air Mercury Rule) for power plants – based on Hg emissions trading 2008 – CAMR and CAIR overturned... What is next? Some events in the U.S. regulation and prevention of mercury emissions “Hot Spot” Controversy -- Many States sue EPA & propose / promulgate more strict regulations

Direct, Anthropogenic Mercury Emissions in the United States (data from USEPA)

Largest sources of total mercury emissions to the air in the U.S. and Canada, based on the U.S. EPA 1999 National Emissions Inventory and data from Environment Canada Canaan Valley Institute-NOAA Beltsville EPA-NOAA Three NOAA sites committed to emerging inter-agency speciated mercury ambient concentration measurement network (comparable to Mercury Deposition Network (MDN) for wet deposition, but for air concentrations) Grand Bay NOAA 13

Barry Holcim Cement NOAA Grand Bay NERR Hg site Weeks Bay OLF Molino Pace Ellyson Jack Watson AL24 AL02 Crist Pascagoula MSW incin haz waste incin paper manuf Victor J. Daniel Mobile Bay Mobile Pascagoula MississippiAlabama NOAA SEARCH USGS UWF/FSU MDN Monitoring Site coal-fired power plant waste incinerator manufacturing metallurgical other fuel combustion type of mercury emissions source total atmospheric mercury emissions (kg/yr, 1999 EPA NEI) – 50 MS 22

Atmospheric Mercury Measurement Site at the Grand Bay NERR, MS mercury and trace gas monitoring tower (10 meters) view from top of the tower

Elemental mercury * 2 Fine particulate mercury * 2 Reactive gaseous mercury * 2 Sulfur dioxide Ozone Carbon Monoxide Nitrogen Oxides (NO, NOy) Wind speed, Wind Direction Temperature, Relative Humidity Precipitation Amount Total Mercury & Methyl Mercury in Precipitation Trace Metals in Precipitation Major Ions in Precipitation WET DEPOSITION: Currently being added, in collaboration with MS DEQ and U.S. EPA “Speciated” Atmospheric Mercury Concentrations Trace gases to help understand and interpret mercury data Meteorological Data Atmospheric Measurements at the Grand Bay NERR

Instrumentation inside the trailer at the Grand Bay NERR site

18

Can we learn what is needed about atmospheric mercury deposition by making atmospheric measurements alone? NO…

Why do we need atmospheric mercury models?  to get comprehensive source attribution information...we don’t just want to know how much is depositing at any given location, we also want to know where it came from:  different source regions (local, regional, national, global)  different jurisdictions (different states and provinces)  anthropogenic vs. natural emissions  different source types (power plants, waste incin., smelters…)

Why do we need atmospheric mercury models?  to get comprehensive source attribution information...we don’t just want to know how much is depositing at any given location, we also want to know where it came from:  different source regions (local, regional, national, global)  different jurisdictions (different states and provinces)  anthropogenic vs. natural emissions  different source types (power plants, waste incin., smelters…)  to estimate deposition over large regions …because deposition fields are highly spatially variable, and one can’t measure everywhere all the time…

Why do we need atmospheric mercury models?  to get comprehensive source attribution information...we don’t just want to know how much is depositing at any given location, we also want to know where it came from:  different source regions (local, regional, national, global)  different jurisdictions (different states and provinces)  anthropogenic vs. natural emissions  different source types (power plants, waste incin., smelters…)  to estimate deposition over large regions …because deposition fields are highly spatially variable, and one can’t measure everywhere all the time…  to estimate dry deposition... presently, dry deposition can only be estimated via models

Why do we need atmospheric mercury models?  to get comprehensive source attribution information...we don’t just want to know how much is depositing at any given location, we also want to know where it came from:  different source regions (local, regional, national, global)  different jurisdictions (different states and provinces)  anthropogenic vs. natural emissions  different source types (power plants, waste incin., smelters…)  to estimate deposition over large regions …because deposition fields are highly spatially variable, and one can’t measure everywhere all the time…  to estimate dry deposition... presently, dry deposition can only be estimated via models  to evaluate potential consequences of future emissions scenarios

Models are not perfect “…Everyone believes monitoring results except for the person making the measurements… and nobody believes modeling results except for the person doing the modeling…” How not perfect are they? Results are encouraging, but difficult to evaluate models due to lack of contemporaneous monitoring and emissions inventory data More certain info at a few locations (monitoring) vs. less certain info region-wide (modeling) Models are a test of our knowledge… If they don’t work, fundamental things about our understanding of atmospheric mercury that are wrong or incomplete…

Dry and wet deposition of the pollutants in the puff are estimated at each time step. The puff’s mass, size, and location are continuously tracked… Phase partitioning and chemical transformations of pollutants within the puff are estimated at each time step = mass of pollutant (changes due to chemical transformations and deposition that occur at each time step) Centerline of puff motion determined by wind direction and velocity Initial puff location is at source, with mass depending on emissions rate TIME (hours) 012 deposition 1 deposition 2deposition to receptor lake Lagrangian Puff Atmospheric Fate and Transport Model NOAA HYSPLIT MODEL 25

26

ReactionRateUnitsReference GAS PHASE REACTIONS Hg 0 + O 3  Hg(p) 3.0E-20cm 3 /molec-secHall (1995) Hg 0 + HCl  HgCl 2 1.0E-19cm 3 /molec-secHall and Bloom (1993) Hg 0 + H 2 O 2  Hg(p) 8.5E-19cm 3 /molec-secTokos et al. (1998) (upper limit based on experiments) Hg 0 + Cl 2  HgCl 2 4.0E-18cm 3 /molec-secCalhoun and Prestbo (2001) Hg 0 +OH  Hg(p) 8.7E-14cm 3 /molec-secSommar et al. (2001) Hg 0 + Br  HgBr 2 AQUEOUS PHASE REACTIONS Hg 0 + O 3  Hg E+7(molar-sec) -1 Munthe (1992) Hg 0 + OH  Hg E+9(molar-sec) -1 Lin and Pehkonen(1997) HgSO 3  Hg 0 T*e ((31.971*T) )/T) sec -1 [T = temperature (K)] Van Loon et al. (2002) Hg(II) + HO 2  Hg 0 ~ 0(molar-sec) -1 Gardfeldt & Jonnson (2003) Hg 0 + HOCl  Hg E+6(molar-sec) -1 Lin and Pehkonen(1998) Hg 0 + OCl -1  Hg E+6 (molar-sec) -1 Lin and Pehkonen(1998) Hg(II)  Hg(II) (soot) 9.0E+2liters/gram; t = 1/hour eqlbrm: Seigneur et al. (1998) rate: Bullock & Brehme (2002). Hg +2 + hv  Hg 0 6.0E-7(sec) -1 (maximum)Xiao et al. (1994); Bullock and Brehme (2002) (Evolving) Atmospheric Chemical Reaction Scheme for Mercury ? ? ? new

When puffs grow to sizes large relative to the meteorological data grid, they split, horizontally and/or vertically Ok for regional simulations, but for global modeling, puff splitting overwhelms computational resources

In this example, the maximum number of puffs was set to 100,000, so when it got close to that number, the splitting was turned off Exponential puff growth Due to puff splitting, the number of puffs quickly overwhelms numerical resources

In each test, the number of puffs rises to the maximum allowable within ~ one week This line is the example from the last slide

In the new version of HYSPLIT (4.9), puffs are “dumped” into an Eulerian grid after a specified time (e.g., 96 hrs), and the mercury is simulated on that grid from then on…

atmospheric chemistry phase partitioning Atmospheric Mercury Model wet and dry deposition Wet and dry deposition of different Hg forms to sensitive ecosystems Source attribution information for deposition Model Outputs Speciated ambient concentration data Wet deposition data Model Evaluation Model Inter-comparison Model Visualization meteorology Inputs to Model emissions land use For model evaluation, model inputs must be for the same time period as measurement data

atmospheric chemistry phase partitioning Atmospheric Mercury Model wet and dry deposition Wet and dry deposition of different Hg forms to sensitive ecosystems Source attribution information for deposition Model Outputs Speciated ambient concentration data Wet deposition data Model Evaluation Model Inter-comparison Model Visualization meteorology Inputs to Model emissions land use Collaboration with JSU is providing a unique and unprecedented opportunity to evaluate and improve atmospheric mercury models JSU collaboration For model evaluation, model inputs must be for the same time period as measurement data

36 We are organizing the initial collaborative work around specific episodes of high concentration of one or more mercury forms

Thanks!

Extra Slides

39 Hg from other sources: local, regional & more distant atmospheric deposition to the water surface atmospheric deposition to the watershed Measurement of ambient air concentrations Measurement of wet deposition

OctNovDecJanFebMarAprMayJunJulAugSep …. Recent RGM concentrations measured at the Grand Bay NERR Then down for ~2 months due to hurricanes

CLOUD DROPLET cloud Primary Anthropogenic Emissions Hg(II), ionic mercury, RGM Elemental Mercury [Hg(0)] Particulate Mercury [Hg(p)] Re-emission of previously deposited anthropogenic and natural mercury Hg(II) reduced to Hg(0) by SO 2 and sunlight Hg(0) oxidized to dissolved Hg(II) species by O 3, OH, HOCl, OCl - Adsorption/ desorption of Hg(II) to /from soot Natural emissions Upper atmospheric halogen-mediated heterogeneous oxidation? Polar sunrise “mercury depletion events” Br Dry deposition Wet deposition Hg(p) Vapor phase: Hg(0) oxidized to RGM and Hg(p) by O 3, H 2 0 2, Cl 2, OH, HCl Multi-media interface Atmospheric Mercury Fate Processes

Environmental Mercury Cycling -- Natural vs. Anthropogenic  Most anthropogenic Hg is “released” as atmospheric emissions:  Hg in coal is released to the air when coal is burned  Hg in other fuels is released to the air when they are processed and burned  Hg in ores is released to the air during metallurgical processes  Hg in products is released to the air when burned or landfilled after being discarded (e.g., batteries, switches)  This has always been going on, and there has always been Hg in fish  Mercury (Hg) is an element... there is the same amount of mercury on Earth today as there always has been  “natural” Hg cycle – Hg is transported throughout the environment, and chemical transformations interconvert different mercury species  But, we make some Hg unexpectedly “bioavailable”  Average, current atmospheric Hg deposition is ~3x pre-industrial levels  Evidence suggests that newly deposited Hg is more bioavailable

Freemont Glacier, Wyoming source: USGS, Shuster et al., 2002 Natural vs. anthropogenic mercury? Studies show that anthropogenic activities have typically increased bioavailable Hg concentrations in ecosystems by a factor of 2 – 10

Mercury transformed by bacteria into methylmercury in sediments, soils & water, then bioaccumulates in fish Humans and wildlife affected primarily by eating fish containing mercury Best documented impacts are on the developing fetus: impaired motor and cognitive skills atmospheric deposition to the watershed atmospheric deposition to the water surface adapted from slides prepared by USEPA and NOAA

What Do We Need to Know Regarding Atmospheric Mercury? Type of InformationMonitoringModeling Atmospheric deposition* Can give us “exact” answers at a few locations Can give us approximate answers throughout the domain* Source-attribution for deposition For monitoring site only -- using receptor-based techniques & enhanced monitoring Can give us approx. information with suitably designed methodology Deposition for historical periods -- Possible if historical emissions inventories can be estimated Deposition for alternative future scenarios -- “Easy” as long as emissions scenarios are specified * consistent with the needs of subsequent analyses (e.g., ecosystem modeling) with respect to spatial, temporal, and “species” resolution (e.g., Hg(0) vs. RGM vs. Hg(p))