@misc{liu_attributing_differences_2018, 
author={Liu, P., Hogrefe, C., Im, U., Christensen, J., Bieser, J., Nopmongcol, U., Yarwood, G., Mathur, R., Roselle, S., Spero, T.},
title={Attributing differences in the fate of lateral boundary ozone in AQMEII3 models to physical process representations},
year={2018},
howpublished = {journal article},
doi = {https://doi.org/10.5194/acp-18-17157-2018},
abstract = {COSMO-CLM∕CMAQ and WRF∕CMAQ show similar performance in inert tracers both at the surface and aloft through most seasons, which suggests similarity between the two models at process level. The largest difference is found in summer. Sub-grid cloud mixing plays a primary role in their differences in inert tracers over the southeastern US and the oceans in summer. Our analysis of the vertical profiles of inert tracers also suggests that the model differences in dry deposition over certain regions are offset by the model differences in vertical turbulent mixing, leading to small differences in inert tracers at the surface in these regions.},
note = {Online available at: \url{https://doi.org/10.5194/acp-18-17157-2018} (DOI). Liu, P.; Hogrefe, C.; Im, U.; Christensen, J.; Bieser, J.; Nopmongcol, U.; Yarwood, G.; Mathur, R.; Roselle, S.; Spero, T.: Attributing differences in the fate of lateral boundary ozone in AQMEII3 models to physical process representations. Atmospheric Chemistry and Physics. 2018. vol. 18, no. 23, 17157-17175. DOI: 10.5194/acp-18-17157-2018}}