Changes to the Multi-Pollutant version in the CMAQ 4.7 William T. Hutzell, Shawn J. Roselle, Annmarie G. Carlton, and O. Russell Bullock Atmospheric Modeling Division US EPA November 28, 2018

Background: Multi-Pollutant Model Developed to simulate criteria and hazardous air pollutants in a single modeling study examine co-benefits of emission reductions over multiple interest O3, Particulate Matter, and Hazardous Air Pollutants (HAPs) Roselle et al. (2007) presented a prototype of the Multi-Pollutant Model mechanism called CB05TXHG_AE4_AQ Based on CB05 mechanisms for mercury and other HAPs in CMAQ version 4.6

Multi-Pollutant Model in version 4.7 Updates prototype in Roselle et al (2007) photochemical production of Secondary Organic Aerosols (SOA) aerosol physics for SOA and interactive coarse mode cloud chemistry of organic compounds and SOA In-calculations for dry deposition and emission processes New mechanism called CB05TXHG_AE5_AQ Specific settings needed to build and run the Multi-Pollutant model. Consult release notes on building and running the model.

Goals of this Presentation Describe major changes to new science options for Multi-Pollutant Model Present differences in predictions from CMAQ using CB05CL_AE5_AQ, the standard version Highlight differences in predictions from the prototype of the Multi-Pollutant Model

Gas Chemistry Adds to CB05CL_AE5_AQ the species and reactions for Hg compounds and other HAPs from CB05HG_AE4_AQ and CB05CLTX_AE4_AQ Two methods compute the chemical transformation of gas phase Hg and other HAPs One participates in ozone and radical photochemistry Other does not affect ozone and radical concentrations and serves as reactive tracers. Changes from CB05TXHG_AE4_AQ adds a new reaction, HG + CL → HGIIGAS This reaction should produce Hg(I) HGIIGAS redefined as reactive gaseous mercury i.e., Hg(I) + Hg(II). Hg(I) assumed to quickly convert into Hg(II) the oxidation process not explicitly represented

Aerosols Adds aerosol species representing mercury and other toxic metals They do not affect aerosol microphysics and deposition rates These aerosols species do coagulate and mode merge Mercury species differ from the other metallic aerosols photochemical source of particulate mercury goes directly into the accumulation mode assumes accumulation mode dominates condensation onto the three aerosol modes unlike version 4.6 where fine modes divided condensation based on their surface area

In-Cloud Chemistry Adds in-scavenging for mercury and other metallic aerosols. Adds cloud chemistry for atmospheric mercury Based on Bullock and Brehme (2002) Indirectly affects other aqueous species modifies the minimum time step used in the numerical solution when the mercury species have the fastest rate of change. mercury chemistry requires using the gas phase HO2, HOCl and Cl2 based on Lin et al. (1998). affects pH and ion balance in cloud droplets

In-Cloud Chemistry (cont.) Possible effects from changes change particulate sulfate wet deposition of HO2, HOCl and Cl2 can produce HOCl from clouds with low or no participation.

Inline Vertical Diffusion Aerosol emissions includes routines for particulate mercury and other metals Emissions includes source of Cl2 over open oceans. Set off by default Set on with the environment variable, CTM_CL2_SEAEMIS Source mimics implied heterogeneous production for sea salt aerosols (Spicer et al. 1998) Knipping and Dadbub (2002 and 2003) proposed a mechanism but not used reaction efficiencies are not well defined CB05CL_AE5_AQ does not include ClNO2 and ClONO2.

Comparison to Standard CMAQ, i.e.,CB05CL_AE5_AQ Using two weekly periods in January and July 2002 Domain covered Continental US grid cell had 36X36 km2 horizontal dimensions 14 vertical layers in s pressure coordinates Comparison used the weekly averages tile plots of differences from CB05CL_AE5_AQ, i.e., standard model scatter plots showing difference versus standard’s prediction

HOCl Higher HOCl production appears higher in January

Ozone Ozone higher in winter and correlate with HOCL but generally within the accuracy of the chemistry solver.

Impact of Ozone Difference: Benzene January’s ozone differences alter OH thereby Benzene

Particulate Sulfate January’s ozone differences also have small effect on sulfate production

Hg Changes between CB05TXHG version 4.6 and 4.7

Areas for further improvement Gas Phase Chemistry for Mercury explicitly representing products Oceanic Cl2 source representing heterogeneous production possible with the proposed SAPRC07 mechanism Bi-Directional Surface Flux for Mercury addressed science model release in version 4.7 see release notes by Jesse Bash Cloud chemistry does not include Cr(III) and Cr(VI) redox reactions Disclaimer: Although this work has been reviewed by EPA and approved for publication, it does not necessarily reflect their policies or views.