Krish Vijayaraghavan, Prakash Karamchandani Christian Seigneur AER San Ramon, CA 3rd Annual CMAS...

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Krish Vijayaraghavan, Prakash Karamchandani Christian Seigneur AER San Ramon, CA 3rd Annual CMAS Models-3 Conference October 18-20, 2004 Chapel Hill, NC Application of CMAQ-APT to the Central California Ozone Study

Transcript of Krish Vijayaraghavan, Prakash Karamchandani Christian Seigneur AER San Ramon, CA 3rd Annual CMAS...

Krish Vijayaraghavan, Prakash KaramchandaniChristian Seigneur

AERSan Ramon, CA

3rd Annual CMAS Models-3 ConferenceOctober 18-20, 2004

Chapel Hill, NC

Application of CMAQ-APT tothe Central California Ozone Study

Overview

• Limitations of 3-D grid modeling• CMAQ-APT: Plume-in-grid (PiG) air quality model

• State-of-the science treatment of stack plumes at the sub-grid scale

• 3-D grid host model - CMAQ• Reactive plume model – SCICHEM

• Impact of PiG treatment on ozone and HNO3 concentrations

Interface between CMAQ and SCICHEM

Domain, grid informationgeophysical datameteorological datadeposition velocities

CMAQ SCICHEM

Emissions,IC/BC

OutputOutput

puffinformation

Pointsource

emissions

Dumppuffs

chemicalconcentrations

chemicalconcentrations

I/OAPI

I/OAPI

I/OAPI

I/OAPI

StandardSCICHEM

output

Puff diagnostics (process analysis)

ControlFile

Improvements to CMAQ-APT

• Optional treatment for the effects of building downwash on plume rise and dispersion (PRIME)

• Incorporation of CMAQ code updates released in September 2003 (version 4.3)

• Incorporation of modifications in SCICHEM version 1601 (January 2004 release)

• Young & Boris chemistry solver

Application to Central California

• Central California Ozone Study (CCOS)

• Ozone episode: July 30 to August 1, 2000

• Study domain– 185 x 185 grid cells– Horizontal grid resolution of 4 km– 20 layers from surface to tropopause

(surface layer ~ 30 m)

Features of July/August 2000 CCOS episode

• Observed peak ozone during the modeling period was 134 ppb at San Andreas station on August 1, 2000

• Prevailing winds from the coast to the Central Valley

• Wildfires in the southeast (Tulare County near the Sierra Nevada)

Model Inputs

• Meteorology driven by MM5

• CMAQ emissions, initial and boundary conditions from CAMx files (ARB)

• 3-D gridded emissions using SMOKE plume rise processor

• Ten largest NOx emitting plants (with 56 stacks) selected for plume-in-grid (PiG) treatment

PiG Sources

Top 10 NOx emissions

1. Pittsburg power plant (16 Mg/day NOx)

2. Riverside Cement3. California Cement4. Moss Landing power plant5. Martinez refinery6. Hanson Cement7. Unknown8. Portland Cement9. IMC Chemicals10.Contra Costa power plant

Total = 101 Mg/day(4% of domain-wideNOx emissions)

Simulations

• CMAQ base simulation

– All emissions in domain in 3-D gridded format

• CMAQ background simulation– 3-D gridded emissions without PiG sources

• CMAQ-APT simulation– 3-D gridded emissions other than PiG sources– PiG sources treated separately with SCICHEM

ExtendedSan Francisco Bay Area

CMAQ Base: Surface Ozone 3 p.m. PDT on July 30, 2000

(Base – Background) Surface Ozone 3 p.m. PDT on July 30, 2000

(APT – Base) Surface Ozone 3 p.m. PDT on July 30, 2000

Evolution of Plume Chemistry

Early Plume Dispersion

NO/NO2/O3 chemistry

1

2

Mid-range Plume Dispersion

Reduced VOC/NOx/O3 chemistry — acid formation from OH and NO3/N2O5 chemistry

Long-range Plume Dispersion

3

Full VOC/NOx/O3 chemistry — acid and O3 formation

CMAQ Base: Surface HNO3

3 p.m. PDT on July 31, 2000

(Base – Background) Surface HNO3 3 p.m. PDT on July 31, 2000

(APT – Base) Surface HNO3 3 p.m. PDT on July 31, 2000

Comparison of CMAQ-APT results in CCOS and NARSTO

• CCOS– APT produces up to 10 ppb lower ozone than Base

and up to 1.5 ppb lower HNO3

• NARSTO– APT produces up to 40 ppb lower ozone than Base

and up to 24 ppb lower HNO3

(Karamchandani et al., J. Geophys. Res.,107, 4403, 2002)

• NOx emissions from PiG sources are about 50 times higher in NARSTO than in CCOS

Conclusions

• CMAQ-APT applied to July/August 2000 CCOS episode

• O3 concentrations using APT show both decrements (up to 10 ppb) and increments (up to 6 ppb) with respect to the base

• The VOC vs. NOx limited nature of the background environment explains the differences in O3 production and destruction between the APT and base results

Conclusions

• Surface HNO3 concentrations are up to 1.5 ppb (about 10%) lower in the CCOS APT simulation and 24 ppb lower in the NARSTO APT simulation, compared to the base cases

• Effect of PiG treatment on HNO3 is important for PM nitrate and regional haze modeling.

• PiG treatment for PM (CMAQ-MADRID-APT) is currently being tested (Karamchandani et al., AWMA, October 2004)

Acknowledgements

• California Energy Commission

• California Air Resources Board

• EPRI

• Titan/ARAP