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Development and Application of CACM/MPMPO

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<strong>Development</strong> <strong>and</strong> <strong>Application</strong> <strong>of</strong><br />

<strong>CACM</strong>/<strong>MPMPO</strong><br />

R.J. Griffin 1 , J. Chen 1 , C.E. Jordan 1 , H. Mao 1 , R.W.<br />

Talbot 1 , S. Vutukuru 2 , <strong>and</strong> D. Dabdub 2<br />

1<br />

UNH, 2 UCI<br />

December 6, 2006<br />

International Conference on Atmospheric Chemical<br />

Mechanisms


Polycyclic<br />

Low Y<br />

Functionalized Hydrocarbons<br />

Primary<br />

VOC<br />

Aromatic<br />

Non-Arom.<br />

Aromatic<br />

Non-Arom.<br />

Monoaromatic<br />

Alkanes<br />

Alkenes<br />

Biogenics<br />

Phenolic<br />

Aldehydic<br />

Acidic<br />

Carbonyls<br />

Ethers<br />

High Y<br />

C 2 -C 6<br />

C 6 -C 12<br />

C 13 +<br />

Ethene<br />

C 3 -C 6<br />

C 7 +<br />

Terpenes<br />

Isoprene<br />

Aldehydes<br />

Ketones<br />

MeOH<br />

EtOH<br />

α-Pinene<br />

β-Pinene<br />

d-Limonene<br />

Low Y<br />

High Y<br />

HCHO<br />

CH 3 CHO<br />

C 3 +<br />

C 3 -C 6<br />

Alcohols<br />

C 3 +<br />

C 7 +


Surrogate Determination<br />

Example:<br />

AROL – low SOA yield aromatics: two or more methyl<br />

substituents<br />

3 xylene isomers<br />

3 TMB isomers<br />

3 TetMB isomers<br />

More highly substituted}<br />

Average C#: ~9 TMB<br />

1,2,3-TMB<br />

k OH<br />

,<br />

prevalence


The Mechanistic Approach<br />

A + ox<br />

α RP/UR 1<br />

}<br />

if α, β, <strong>and</strong> γ have<br />

β RP/UR 2 been determined<br />

γ RP/UR 3<br />

ox<br />

…<br />

(1−α−β−γ) RO 2 i<br />

NO<br />

ξ ROi + ξ NO2 + (1-ξ) APi<br />

OH<br />

RP/UR<br />

isomerization<br />

decomposition<br />

reaction with O 2<br />

RP/UR


Example Chemistry<br />

Now over 500 reactions to describe the formation <strong>of</strong> SOA precursors,<br />

ozone, <strong>and</strong> other photochemical pollutants (Griffin et al., 2002, 2005;<br />

Chen <strong>and</strong> Griffin, 2005)


Formation <strong>of</strong> SOA<br />

VOC + ox <br />

P 1 , P 2 , …P n<br />

G 1 ,G 2 ,...,G n<br />

A 1 ,A 2 ,...,A n<br />

AQ 1 ,AQ 2 ,...,AQ n<br />

K om,i<br />

Partitioning Theory<br />

A i<br />

/ M o<br />

= ∼<br />

G i<br />

Griffin et al. (2003, 2005)<br />

RT<br />

p o L,i MW om γ i<br />

Henry’s Law <strong>and</strong><br />

Dissociation<br />

H i<br />

= γ i<br />

aq<br />

AQ i<br />

/G i<br />

AQ i AQ i - AQ i<br />

2-<br />

Inorganics using ISORROPIA


Simulation <strong>of</strong> Chamber Experiments<br />

700<br />

70<br />

NO, NO 2 <strong>and</strong> O 3 mixing ratio (ppb)<br />

600<br />

500<br />

400<br />

300<br />

200<br />

100<br />

0<br />

d-limonene<br />

NO<br />

0 30 60 90 120 150 180<br />

Time (min)<br />

O 3<br />

NO 2<br />

60<br />

50<br />

40<br />

30<br />

20<br />

10<br />

0<br />

d-limonene mixing ratio (ppb) -<br />

Experiment: Griffin et al. (1999)<br />

Simulation: Chen <strong>and</strong> Griffin (2005)


Simulation <strong>of</strong> Chamber Experiments<br />

SOA (µg m -3 )<br />

40<br />

30<br />

20<br />

10<br />

Predicted<br />

Observed<br />

0<br />

0 100 200 300<br />

Time (min)<br />

Experiment (α-pinene + O 3 ): Griffin et al. (1999)<br />

Simulation: Chen <strong>and</strong> Griffin (2005)


Simulation <strong>of</strong> Chamber Experiments<br />

Predicted SOA / Observed SOA<br />

3.0<br />

2.0<br />

1.0<br />

0.0<br />

α-pinene<br />

β-pinene<br />

d-limonene<br />

1 10 100 1000<br />

Observed SOA (µg/m 3 )<br />

Experiments: Odum et al. (1996); H<strong>of</strong>fmann et al. (1997); Griffin et al. (1999)<br />

Simulations: Chen <strong>and</strong> Griffin (2005)


Implementation into CMAQ<br />

Caltech Atmospheric<br />

Chemistry Mechanism<br />

Updated with α-Pinene,<br />

β-Pinene & d-Limonene<br />

Chemistry<br />

H 2<br />

SO 4<br />

,HNO 3<br />

NH 3<br />

ISORROPIA Inorganic<br />

Aerosol Module<br />

H 2<br />

O, H +<br />

SOA<br />

Precursors<br />

POA<br />

Model to Predict the<br />

Multi-phase<br />

Partitioning <strong>of</strong> Organics<br />

SOA Output


Model<br />

Domain<br />

62 x 66 cells<br />

36km resolution<br />

21 vertical layers<br />

Dates: August 3-4, 2004<br />

August 1-2 spin-up<br />

(ICARTT)<br />

Meteorological fields:<br />

MM-5<br />

Emissions: 1999 NEI/BEIS3<br />

Circles: IMPROVE<br />

Star: AIRMAP<br />

Triangles: SEARCH


Example Gas-Phase Results: AI*<br />

160<br />

Observation<br />

120<br />

<strong>CACM</strong><br />

CB4_1<br />

O 3 Mixing Ratio (ppb)<br />

80<br />

40<br />

0<br />

2004-8-3 0:00 2004-8-3 12:00 2004-8-4 0:00 2004-8-4 12:00 2004-8-5 0:00<br />

Time (UTC)<br />

*Appledore Isl<strong>and</strong>, ME Chen et al., 2006


Aerosol-Phase Results: Domain<br />

18<br />

Concentration (µg/m 3 )<br />

16<br />

14<br />

12<br />

10<br />

8<br />

6<br />

Measured<br />

<strong>CACM</strong>/<strong>MPMPO</strong><br />

CB4/SORGAM<br />

4<br />

2<br />

0<br />

PM2.5 Sulfate Nitrate Ammonium EC OC<br />

24-hour filter measurements; ions by IC, EC <strong>and</strong> OC by thermo-optical method<br />

Chen et al., 2006


Aerosol-Phase Results: TF*<br />

12.0<br />

AMS measured<br />

6.0<br />

Measured OC (µg/m 3 )<br />

10.0<br />

8.0<br />

6.0<br />

4.0<br />

2.0<br />

<strong>CACM</strong>/<strong>MPMPO</strong><br />

CB4/SORGAM<br />

4.0<br />

2.0<br />

Modeled OC (µg/m 3 )<br />

0.0<br />

8-3 0:00 8-3 12:00 8-4 0:00 8-4 12:00 8-5 0:00<br />

Time (UTC)<br />

0.0<br />

Data from an Aerodyne Q-AMS (Cottrell et al., 2006, in prep.)<br />

*Thompson Farm, NH<br />

Chen et al., 2006


Domain-Wide Results: SOA<br />

<strong>CACM</strong>/<strong>MPMPO</strong><br />

CB4/SORGAM<br />

Chen et al.,<br />

2006


Chen et al., 2006<br />

Aqueous-Phase SOA


Other Recent <strong>Application</strong>s<br />

•Study <strong>of</strong> dynamics <strong>of</strong> SOA in the SoCAB (Vutukuru et al.,<br />

2006)<br />

• SOA source apportionment in the SoCAB (Ying et al.,<br />

2006; Kleeman et al., 2006)<br />

• SOA study in southern France (high contribution <strong>of</strong><br />

diesel!; Tulet et al., 2006)<br />

• Photochemical formation <strong>of</strong> CO in the eastern US <strong>and</strong> the<br />

SoCAB (Griffin et al., 2006)<br />

• Photochemical modeling <strong>of</strong> peroxy radicals for φ<br />

calculations in New Engl<strong>and</strong> (Griffin et al., 2006)


Hot Off the Press (1) – In-cloud<br />

Chen et al.<br />

poster here!


Hot Off the Press (2) - Alkanes<br />

Jordan et al.<br />

poster here!


Hot Off the Press (3) - Dynamics<br />

Vutukuru et al.<br />

AAAR poster


Example Strengths <strong>and</strong><br />

Weaknesses<br />

Strengths<br />

• Not specific to one set <strong>of</strong> chamber conditions<br />

• Chemical <strong>and</strong> phase specificity<br />

• Appropriate NO x<br />

dependence (though not strong enough)<br />

• A dynamic duo<br />

Weaknesses<br />

• Missing SOA sources (i.e., isoprene, sesquiterpenes,<br />

organic-sulfate interactions including aldehydes, ?, etc.)<br />

• Computationally expensive<br />

• Specificity <strong>of</strong> emissions is somewhat burdensome<br />

• POA <strong>and</strong> vapor pressure characterization<br />

• Biased to SoCAB?


What’s Next?<br />

• Missing chemistry<br />

– Isoprene <strong>and</strong> sesquiterpenes<br />

– Particle-phase/heterogeneous reactions (organicsulfate,<br />

peroxides)<br />

–Low-NO x chemistry<br />

– Ammonia-acid interactions<br />

– Cl-VOC chemistry for application to the MBL


Thanks to…<br />

• My co-authors<br />

• Laura Cottrell, Luke Ziemba, Pieter Beckman<br />

(AMS data)<br />

• Additional collaborators (Meteo France, UCD,<br />

UCR)<br />

• NOAA, EPA, NSF, & EPRI for funding<br />

• The organizers

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