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11/23/2009 1 Reducing Uncertainties in Modeling Atmospheric Mercury Reducing Uncertainties in Modeling Atmospheric Mercury Tracey Holloway Tracey Holloway Caitlin Littlefield, Jami Morton, Jamie Schauer, Andrew Rutter University of Wisconsin-Madison Nelson Institute Center for Sustainability and the Global Environment (SAGE) R833375 Three different atmospheric mercury species Elemental Gaseous Mercury (Hg 0 ) - stays in Mercury Basics Mercury Basics Elemental Gaseous Mercury (Hg ) - stays in atmosphere for 1-1.5 years, global pollutant from global sources Reactive Gaseous Mercury (RGHg) - stays in atmosphere for a few days, highly reactive Particulate Mercury (PHg) - stays in atmosphere for about a week, removed by precipitation

Reducing Uncertainties in Modeling Atmospheric Mercury · • Great Lakes region with 12 km x 12 km resolution • 30 vertical layers in WRF, 15 vertical layers in CMAQ 20 10 •

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Page 1: Reducing Uncertainties in Modeling Atmospheric Mercury · • Great Lakes region with 12 km x 12 km resolution • 30 vertical layers in WRF, 15 vertical layers in CMAQ 20 10 •

11/23/2009

1

Reducing Uncertainties in Modeling Atmospheric Mercury

Reducing Uncertainties in Modeling Atmospheric Mercury

Tracey HollowayTracey Holloway

Caitlin Littlefield, Jami Morton, Jamie Schauer, Andrew Rutter

University of Wisconsin-Madison

Nelson Institute Center for Sustainability and the Global Environment (SAGE)

R833375

Three different atmospheric mercury species

• Elemental Gaseous Mercury (Hg0) - stays in

Mercury BasicsMercury Basics

• Elemental Gaseous Mercury (Hg ) - stays in atmosphere for 1-1.5 years, global pollutant from global sources

• Reactive Gaseous Mercury (RGHg) - stays in atmosphere for a few days, highly reactive

• Particulate Mercury (PHg) - stays in atmosphere for about a week, removed by precipitation

Page 2: Reducing Uncertainties in Modeling Atmospheric Mercury · • Great Lakes region with 12 km x 12 km resolution • 30 vertical layers in WRF, 15 vertical layers in CMAQ 20 10 •

11/23/2009

2

Mercury BasicsMercury Basics

Mercury BasicsMercury Basics

Hg0 is transported across the globe, while RGHg and PHg are removed

more quickly.

Page 3: Reducing Uncertainties in Modeling Atmospheric Mercury · • Great Lakes region with 12 km x 12 km resolution • 30 vertical layers in WRF, 15 vertical layers in CMAQ 20 10 •

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3

Mercury BasicsMercury Basics

Total wet deposition isTotal wet deposition is known, but species

contribution is unclear.

Mercury BasicsMercury Basics

Total wet deposition isTotal wet deposition is known, but species

contribution is unclear.

Page 4: Reducing Uncertainties in Modeling Atmospheric Mercury · • Great Lakes region with 12 km x 12 km resolution • 30 vertical layers in WRF, 15 vertical layers in CMAQ 20 10 •

11/23/2009

4

Mercury BasicsMercury Basics

Dry deposition is highlyDry deposition is highly uncertain.

Mercury BasicsMercury Basics

Chemical cycling in the atmosphere is uncertain.

Page 5: Reducing Uncertainties in Modeling Atmospheric Mercury · • Great Lakes region with 12 km x 12 km resolution • 30 vertical layers in WRF, 15 vertical layers in CMAQ 20 10 •

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Species ContributionSpecies Contribution

•Most mercury emissions as Hg0, followed by RGHg and then PHg

100

75

•Spatial artifacts from data collection methods - by state and country

25

50

Percent Hg0 of Total Annual Emissions

(%)0

Percent RGHg of Total Annual Emissions Percent PHg of Total Annual Emissions

Emissions Meteorology

Modeling SystemsModeling Systems

AssimilatedMeteorology

D t

North AmericanSpeciated Mercuryd C it i E i i

Chemical Transport

Model(CMAQ)

Chemical Transport

Model(CMAQ)

Emissions Processing Model

Regional ClimateModel(WRF)

Dataand Criteria Emissions

ConcentrationsAmbient

ConcentrationsDry

DepositionWet

Deposition

Page 6: Reducing Uncertainties in Modeling Atmospheric Mercury · • Great Lakes region with 12 km x 12 km resolution • 30 vertical layers in WRF, 15 vertical layers in CMAQ 20 10 •

11/23/2009

6

Model Grid & ResolutionModel Grid & Resolution

• Full-year run from January 2003 to January 2004

40

30• U.S. domain with 36 km x 36 km resolution

• Great Lakes region with 12 km x 12 km resolution

• 30 vertical layers in WRF, 15 vertical layers in CMAQ

30

20

10CMAQ• CB05 chemistry and

aerosol module 4, with mercury

Average Temperature for July 2003(°C)

0

Wet DepositionWet Deposition

Mercury Deposition Network (MDN)• Weekly unspeciated total mercury wet deposition• CMAQ generally under-predicts wet deposition

(B ll k d B h 2002 Gb t l 2007 B ll k(Bullock and Brehme, 2002; Gbor et al., 2007; Bullock et al., 2009; Lin et al., 2007)

General agreement across

models, mechanisms andmechanisms and

inputs.

Accuracy or imitation?

Page 7: Reducing Uncertainties in Modeling Atmospheric Mercury · • Great Lakes region with 12 km x 12 km resolution • 30 vertical layers in WRF, 15 vertical layers in CMAQ 20 10 •

11/23/2009

7

Ambient ConcentrationsAmbient Concentrations

• Episodic and/or unspeciated (Sillman et al., 2007; Burke et al., 1995)

Devil’s Lake

, )

• CMAQ captures total mercury concentrations (e.g. Lin and Tao, 2007)

• Comparison with speciated surface concentrations every ..Madison

Milwaukee

surface concentrations every two hours at Devil’s Lake (rural) and Milwaukee (urban) for 2003 and 2004 collected by Jamie Schauer and Andy Rutter

Wet Deposition in the Great LakesWet Deposition in the Great LakesJuly Wet Deposition

y = 0.3859x + 103.18

2500

R2 = 0.2815

500

1000

1500

2000

Mod

eled

(ng/

m2 )

0

500

0 500 1000 1500 2000 2500

MDN (ng/m 2)Observed (ng/m2)

Page 8: Reducing Uncertainties in Modeling Atmospheric Mercury · • Great Lakes region with 12 km x 12 km resolution • 30 vertical layers in WRF, 15 vertical layers in CMAQ 20 10 •

11/23/2009

8

Wet Deposition in the Great LakesWet Deposition in the Great LakesJuly Wet Deposition

y = 0.3859x + 103.18

2500 Reproduces range for total wet deposition as well as previous studies

R2 = 0.2815

500

1000

1500

2000

Mod

eled

(ng/

m2 )

as well as previous studies

Under-predicts Great Lakes weekly wet deposition by a factor of 1.5

Precipitation can explain roughly 50% of wet deposition error

0

500

0 500 1000 1500 2000 2500

MDN (ng/m 2)Observed (ng/m2)

Model reproduces observed values best in summer

Ambient Surface Concentration - RuralAmbient Surface Concentration - RuralHg0

ng/m3

2.5

2

1.5

1

RGHgpg/m3

40

30

20

10

50

Observed Modeled

PHgpg/m340

30

20

10

50

Apr May Jun Jul Aug Sep Oct Nov Dec Jan Feb Mar Apr May

Page 9: Reducing Uncertainties in Modeling Atmospheric Mercury · • Great Lakes region with 12 km x 12 km resolution • 30 vertical layers in WRF, 15 vertical layers in CMAQ 20 10 •

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Ambient Surface Concentration - RuralAmbient Surface Concentration - RuralImported or Emitted?Imported or Emitted?

April RHgpg/m3

July RHgpg/m3pg

Observed Emissions OnlyBase Case Imported Only

Ambient Surface Concentration - UrbanAmbient Surface Concentration - UrbanHg0

ng/m3

5

4

3

2

1

RGHgpg/m3

70

50

30

10

Observed Modeled

PHgpg/m3

20

40

60

80

Jul Aug Sep Oct Nov Dec Jan Feb Mar Apr May Jun

Page 10: Reducing Uncertainties in Modeling Atmospheric Mercury · • Great Lakes region with 12 km x 12 km resolution • 30 vertical layers in WRF, 15 vertical layers in CMAQ 20 10 •

11/23/2009

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Ambient Surface Concentration - UrbanAmbient Surface Concentration - UrbanImported or Emitted?Imported or Emitted?

July RHgpg/m3

Observed Emissions OnlyBase Case Imported Only

Wet DepositionWet DepositionImported or Emitted?Imported or Emitted?

July Wet Deposition

2000

500

1000

1500

Mod

eled

(ng/

m2 )

0

500

0 500 1000 1500 2000

MDN (ng/m 2)

MDN: 2456, 2043Base Case: 807, 973Case IMPT: 766, 916

Case EMIS: 42, 57

Emissions OnlyBase Case Imported Only

Observed (ng/m2)

Page 11: Reducing Uncertainties in Modeling Atmospheric Mercury · • Great Lakes region with 12 km x 12 km resolution • 30 vertical layers in WRF, 15 vertical layers in CMAQ 20 10 •

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Dry DepositionDry DepositionImported or Emitted?Imported or Emitted?

100

50

Imported RHg Percent Contribution to Total July Dry Deposition

(%)0

Major Uncertainties…Major Uncertainties…

O di ti t f f ti• Over-prediction at surface for reactive mercury concentrations driven by local chemical production from Hg0

RHg production is too high

• RGHg plumes do not reach rural sitesDry deposition removal likely too fastDry deposition removal likely too fast

• Wet deposition values agree, but are based on erroneous chemistry

“Tuned” wet deposition, not model accuracy

Page 12: Reducing Uncertainties in Modeling Atmospheric Mercury · • Great Lakes region with 12 km x 12 km resolution • 30 vertical layers in WRF, 15 vertical layers in CMAQ 20 10 •

11/23/2009

12

Research Needs

Speciated concentration monitorsSpeciated concentration monitors

Further laboratory study for mercury chemistry and dry deposition

Speciated reporting for wet depositionp p g p

Laboratory and field measurements for dry deposition data

Thank you!Thank you!

Tracey Holloway

[email protected]

Center for Sustainability and the Global Environment (SAGE)

R833375