Articles | Volume 18, issue 23
https://doi.org/10.5194/acp-18-17157-2018
https://doi.org/10.5194/acp-18-17157-2018
Research article
 | 
05 Dec 2018
Research article |  | 05 Dec 2018

Attributing differences in the fate of lateral boundary ozone in AQMEII3 models to physical process representations

Peng Liu, Christian Hogrefe, Ulas Im, Jesper H. Christensen, Johannes Bieser, Uarporn Nopmongcol, Greg Yarwood, Rohit Mathur, Shawn Roselle, and Tanya Spero

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Cited articles

Baker, K. R., Emery, C., Dolwick, P., and Yarwood, G.: Photochemical grid model estimates of lateral boundary contributions to ozone and particulate matter across the continental United States, Atmos. Environ., 123, 49–62, 2015. 
Christensen, J. H.: The Danish Eulerian Hemispheric Model – a three-dimensional air pollution model used for the Arctic, Atmos. Environ., 31, 4169–4191, 1997. 
Cooper, O. R., Gao, R. S., Tarasick, D., Leblanc, T., and Sweeney, C.: Long-term ozone trends at rural ozone monitoring sites across the United States, 1990–2010, J. Geophys. Res.-Atmos., 117, 1984–2012, 2012. 
Dolwick, P., Akhtar, F., Baker, K. R., Possiel, N., Simon, H., and Tonnesen, G.: Comparison of background ozone estimates over the western United States based on two separate model methodologies, Atmos. Environ., 109, 282–296, 2015. 
Doms, G., Föerstner, J., Heise, E., Herzog, H.-J., Mironov, D., Raschendorfer, M., Reinhardt, T., Ritter, B., Schrodin, R., Schulz, J.-P., and Vogel, G.: A Description of the Nonhydrostatic Regional COSMO Model Part II: Physical Parameterization, German weather service, Offenbach, Germany, available at: http://www.cosmo-model.org/content/model/documentation/core/cosmoPhysParamtr.pdf (last access: 3 October 2018), 2011. 
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Short summary
This study represents an intercomparison of four regional-scale air quality simulations in order to understand the model similarities and differences in estimating the impact of ozone imported from outside of the US on the surface ozone within the US at process level. Vertical turbulent mixing stands out as a primary contributor to the model differences in inert tracers.
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