R. Ahmadov 1,2, S. McKeen 1,2, R. Bahreini 1,2, A. Middlebrook 2, J.A. deGouw 1,2, J.L. Jimenez 1,3, P.L. Hayes 1,3, A.L. Robinson 4, M. Trainer 2 1 Cooperative.

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R. Ahmadov 1,2, S. McKeen 1,2, R. Bahreini 1,2, A. Middlebrook 2, J.A. deGouw 1,2, J.L. Jimenez 1,3, P.L. Hayes 1,3, A.L. Robinson 4, M. Trainer 2 1 Cooperative Institute for Research in Environmental Sciences, University of Colorado at Boulder, Boulder, CO, USA 2 Earth System Research Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO, USA 3 Department of Chemistry and Biochemistry, University of Colorado, Boulder, CO, USA 4 Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, PA, USA Acknowledgements: E. Edgerton, J. Meagher, T. Ryerson, C. Warneke, R. Weber, L. Russell, A. Goldstein, R. Cohen, J. Stutz, J. Holloway, NOAA USWRP program 1 Application of a volatility basis set model to secondary organic aerosol simulations across the U.S.

Outline VBS mechanism WRF-CHEM evaluation for the eastern U.S., August- September, 2006 DWH oil spill CalNex-2010 simulations – preliminary results 2

3 Farina et al., 2010 Volatility Basis Set (VBS) Faster aging takes place in the gas phase, deposition of these vapors can be significant removal mechanism Organic condensable vapors (OCVs)

SOA yields – RACM mechanism Updates to Murphy and Pandis (2010)

WRF-CHEM sensitivity runs Anthropogenic OCV reaction rate with OH Biogenic OCV reaction rate with OH Deposition Velocity of OCVs Model Horizontal Resolution Planetary Boundary Layer Scheme Optimum Values – Based on Evaluation Statistics Both Anthropogenic and Biogenic OCV age OCV - OH rx rate = /cm 3 -s Deposition velocity of OCV = 0.25*(HNO3 deposition velocity) No additional SVOC or IVOC Ahmadov et al., submitted

6 Near surface organic aerosol concentrations, daily averaged during 08/04– 09/28, 2006 Ahmadov et al., submitted

Observation data 7

Comparison with the SEARCH data 8

9

10 Comparison with the SEARCH data

Mexican Gulf oil spill from DWH  NOAA P3 aircraft’s 2 flights on 8th and 10th of June  High concentrations (10-20 ppb) of aromatics C9-11 were detected  μg/m3 organic particles were observed too! deGouw J. et al., Science (2011) 11

Middlebrook et al., in press Comparison against the surface data: search network Model shows good overall correlation with observations during June, When model shows an impact from the DWH spill, there is a corresponding peak in the observations. The magnitude and timing of the peaks are not always coincident. Gulfport, MS

CalNex-2010 domain, 20km resolution domain, topography 13 4km domain Caltech Bakersfield

14

15 UTC Vertical profile of OA over Caltech, May-16 th (weekend)

16 Evaluation of the organic aerosol simulation, Caltech site, 14/05-15/06, 2010

Concluding remarks The new SOA scheme based on the VBS approach, the updated SOA yields and the aging mechanism substantially improves OA simulations by WRF-CHEM The new SOA scheme within the MADE module of WRF-CHEM is a computationally efficient and suitable tool for a wide range of air quality modeling applications More OA measurements across the U.S. with high spatiotemporal resolution is needed to better constrain the SOA models (e.g. drawback of daily concentrations) Additional measurements/variables for better evaluation are necessary: e.g. O:C ratios, PMF analysis, C14… 17