Title: Prakash Bhave, Ann Marie Carlton, Sergey Napelenok, Tad Kleindienst, John Offenberg, Michael Lewandowski, Mohammed Jaoui
1Evaluation of CMAQ for Precursor-Specific
Contributions to SOA in the Southeastern U.S.
- Prakash Bhave, Ann Marie Carlton, Sergey
Napelenok, Tad Kleindienst, John Offenberg,
Michael Lewandowski, Mohammed Jaoui - CMAS Conference
- Chapel Hill, NC
- October 19 21, 2009
2Overview
- Background
- Previous evaluations of CMAQ organic aerosol
- Revised SOA treatment in CMAQ v4.7
- Evaluation of current CMAQ results
3CMAQ v4.5 Evaluation OC EC
Median Bias (µgC m-3)
Summary of performance at all eastern U.S sites
in 2001.Ref K.W. Appel, et al. (2008), Atmos.
Environ. 6057-6066.
4Carbon Source Matrix
5Model Eval. POA tracers (Jul99)
Modeled Observed Concentration
Bhave, Pouliot, Zheng, Environ. Sci. Technol.
(2007)
6Radiocarbon Measurements (14C)
- Technique takes advantage of fact that 14C
isotope is absent in fossil fuels - PM2.5 samples collected at Nashville on June 21
July 13, 1999 were analyzed for 14C
C.W. Lewis et al., Atmos. Environ. (2004)
7Model Eval. Fossil-Fuel Carbon
8Model Eval. Contemporary Carbon
9Model Evaluation OC/EC Ratio
- Legend
- CMAQ results solid line empirical estimates
dashed line - OCsec is underestimated in the Southeast during
summer - OCsec is overestimated in the west-coast states
Yu, Bhave, Dennis, Mathur, Environ. Sci.
Technol. (2007)
10Missing Source(s) in CMAQ?(Summer OC in
Southeast)
11Tracer-Based Estimates of SOC
- Tracer-based method for estimating source
contributions to ambient SOC - Lab Experiments
- Smog chamber irradiations of numerous VOC/NOx
mixtures - Identified and quantified unique tracer compounds
(e.g., methyl tetrols) using advanced GC/MS
methods. - Computed tracer/SOC ratios for each SOA precursor
( tracers 3 isop, 9 mono., 1 sesq., 1 arom.) - Field Measurements
- Collected 33 PM2.5 samples in RTP throughout 2003
(2 5 day duration) - Quantified the same tracer compounds that were
found in the chamber studies. - Estimated ambient SOC contribution from each VOC
precursor, using the tracer/SOC ratios. - See Kleindienst et al. (Atmos. Environ., 41
8288-8300, 2007) for details.
Greatest source of uncertainty - Are the
tracer/SOC ratios measured in the chamber equal
to those in the atmosphere? Approach - Accept
the tracer estimates at face value until better
information becomes available.
12Tracer-Based Estimates
CMAQ v4.6 Results
Secondary Organic Carbon (µgC m-3)
- CMAQ v4.6 had
- the wrong seasonal cycle for total SOC
- too much monoterpene SOC (especially in Spring
Fall) - not enough aromatic SOC
- no isoprene or sesquiterpene SOC (also noted by
Morris et al., 2006)
Kleindienst, Jaoui, Lewandowksi, Offenberg,
Lewis, Bhave, Edney, Atmos. Environ. (2007)
13CMAQ v4.7
14Did It Make a Difference?
CMAQ v4.6
new SOA treatment
Secondary Organic Carbon (µgC m-3)
- Model results from lowest layer are averaged by
month - 36km grid cell containing Research Triangle Park
measurement site
15Did It Make a Difference?
CMAQ v4.6
new SOA treatment
Secondary Organic Carbon (µgC m-3)
- Model results from lowest layer are averaged by
month - 36km grid cell containing Research Triangle Park
measurement site
16Model Evaluation for 4 SOC Classes
Tracer-Based Estimates
CMAQ new SOA
- Model results are consistently low (29 out of 33
samples), especially during high-pollution
episodes in Summer
17Model Evaluation for 4 SOC Classes
CMAQ Model Results µgC m-3
Tracer-Based Estimates µgC m-3
18Summary
- References
- Appel, K.W. Bhave, P.V. Gilliland, A.B.
Sarwar, G. Roselle, S.J. Evaluation of the
Community Multiscale Air Quality (CMAQ) Model
Version 4.5 Sensitivities Impacting Model
Performance Part II Particulate Matter,
Atmospheric Environment, 2008, 426057-6066. - Bhave, P.V. Pouliot, G.A. Zheng, M. Diagnostic
Model Evaluation for Carbonaceous PM2.5 Using
Organic Markers Measured in the Southeastern
U.S., Environmental Science and Technology, 2007,
411577-1583 - Bhave, P. Yu, S. Lewis, C. Evaluation of a Model
for Predicting the Fossil-Fuel and Biogenic
Contributions to Fine Particulate Carbon,
American Association of Aerosol Research, 11B1,
Austin, October 2005 - Kleindienst, T.E. Jaoui, M., Lewandowski, M.
Offenberg, J.H. Lewis, C.W. Bhave, P.V. Edney,
E.O. Estimates of the Contributions of Biogenic
and Anthropogenic Hydrocarbons to Secondary
Organic Aerosol at a Southeastern US Location,
Atmospheric Environment, 2007, 418288-8300 - Yu, S. Bhave, P.V. Dennis, R.L. Mathur, R.
Seasonal and Regional Variations of Primary and
Secondary Organic Aerosols over the Continental
United States Semi-empirical estimates and model
evaluation, Environmental Science and Technology,
2007, 41 4690-4697
- Despite significant updates, CMAQ results still
fall short of observed SOC in Southeast during
Summer - Missing isoprene SOC
- May be due to insufficient in-cloud formation
- Missing aromatic SOC
- May require a VBS approach
- Monoterpene sesquiterpene SOC are in the right
ballpark - Preliminary results from Midwest
- All 4 SOC types underestimated from May Sept.
- See poster by Napelenok et al.
19Extra Figures
20Site Location Aerial Photo
RTP sampling site located at 35.894ºN and 78.877ºW
21Site Location Gridded Map w. Counties
MM5 Land Use Categories
Site is in NE corner of grid cell (121,50) 4km
from nearest neighboring cell.
LEGEND Mixed ForestCropland/Woodland
MosaicEvergreen Needleleaf ForestDryland
Cropland and PastureDeciduous Broadleaf Forest