Evaluating the Impact of Chemical Complexity and Horizontal Resolution on Tropospheric Ozone Over the Conterminous US With a Global Variable Resolution Chemistry Model

dc.contributor.authorSchwantes, Rebecca H.
dc.contributor.authorLacey, Forrest G.
dc.contributor.authorTilmes, Simone
dc.contributor.authorEmmons, Louisa K.
dc.contributor.authorWolfe, Glenn
dc.contributor.authoret al.
dc.date.accessioned2023-07-19T20:20:17Z
dc.date.available2023-07-19T20:20:17Z
dc.date.issued2022-05-20
dc.descriptionAuthors: - Rebecca H. Schwantes, Forrest G. Lacey, Simone Tilmes, Louisa K. Emmons, Peter H. Lauritzen, Stacy Walters, Patrick Callaghan, Colin M. Zarzycki, Mary C. Barth, Duseong S. Jo, Julio T. Bacmeister, Richard B. Neale, Francis Vitt, Erik Kluzek, Behrooz Roozitalab, Samuel R. Hall, Kirk Ullmann, Carsten Warneke, Jeff Peischl, Ilana B. Pollack, Frank Flocke, Glenn Wolfe, Thomas F. Hanisco, Frank N. Keutsch, Jennifer Kaiser, Thao Paul V. Bui, Jose L. Jimenez, Pedro Campuzano-Jost, Eric C. Apel, Rebecca S. Hornbrook, Alan J. Hills, Bin Yuan, Armin Wisthaleren_US
dc.description.abstractA new configuration of the Community Earth System Model (CESM)/Community Atmosphere Model with full chemistry (CAM-chem) supporting the capability of horizontal mesh refinement through the use of the spectral element (SE) dynamical core is developed and called CESM/CAM-chem-SE. Horizontal mesh refinement in CESM/CAM-chem-SE is unique and novel in that pollutants such as ozone are accurately represented at human exposure relevant scales while also directly including global feedbacks. CESM/CAM-chem-SE with mesh refinement down to ∼14 km over the conterminous US (CONUS) is the beginning of the Multi-Scale Infrastructure for Chemistry and Aerosols (MUSICAv0). Here, MUSICAv0 is evaluated and used to better understand how horizontal resolution and chemical complexity impact ozone and ozone precursors over CONUS as compared to measurements from five aircraft campaigns, which occurred in 2013. This field campaign analysis demonstrates the importance of using finer horizontal resolution to accurately simulate ozone precursors such as nitrogen oxides and carbon monoxide. In general, the impact of using more complex chemistry on ozone and other oxidation products is more pronounced when using finer horizontal resolution where a larger number of chemical regimes are resolved. Large model biases for ozone near the surface remain in the Southeast US as compared to the aircraft observations even with updated chemistry and finer horizontal resolution. This suggests a need for adding the capability of replacing sections of global emission inventories with regional inventories, increasing the vertical resolution in the planetary boundary layer, and reducing model biases in meteorological variables such as temperature and clouds.en_US
dc.description.sponsorshipThe authors thank the following researchers who helped collect the field campaign data used in this work as further summarized in Tables S3 and S4 in Supporting Information S1: Ronald Cohen for organic nitrates and peroxy acyl nitrates during SEAC4RS; Richard Ferrare, John Hair, and Amy Jo Scarino for PBLH during SEAC4RS; Thomas B. Ryerson for ozone and NOx during SEAC4RS and SENEX; Paul Wennberg, John Crounse, and Jason St. Clair for isoprene oxidation products during SEAC4RS; Glenn S. Diskin for CO and H2O from SEAC4RS and CO from DISCOVER-AQ; John S. Holloway for CO during SENEX, Gerd Huebler for photolysis rates during SENEX; Martin Graus for acetonitrile, isoprene, and monoterpenes during SENEX; Ann Middlebrook, Jin Liao, and Andre Welti for organic aerosol measurements during SENEX; Andrew J. Weinheimer, David J. Knapp, Deedee Montzka, and Geoffrey S. Tyndall for ozone and NOx during NOMADSS and DISCOVER-AQ; Lisa Kaser for monoterpenes and isoprene during NOMADSS; Daniel Riemer and Nicola Blake for their assistance with the Trace Organic Gas Analyzer measurements during NOMADSS; Teresa Campos, Michael Reeves, Daniel Stechman, and Meghan Stell for CO during NOMADSS; Alan Fried and James Walega for CH2O during DISCOVER-AQ; and John Barrick and Ali Aknan for photolysis measurements during DISCOVER-AQ. The PTR-MS instrument team (T. Mikoviny, M. Müller, and P. Eichler) is acknowledged for their support with field work and data processing and Ionicon Analytik is acknowledged for instrumental support. This material is based upon work supported by the National Center for Atmospheric Research (NCAR), which is a major facility sponsored by the National Science Foundation (NSF) under Cooperative Agreement No. 1852977. The Community Earth System Model (CESM) project is supported primarily by the NSF. Computing and data storage resources, including the Cheyenne supercomputer (https://doi.org/10.5065/D6RX99HX), were provided by the Computational and Information Systems Laboratory (CISL) at the NCAR (CISL, 2017). We thank all the scientists, software engineers, and administrators who contributed to the development of CESM2. Computational resources for this work were provided by a NCAR Strategic Capability (NSC) award (NACM0003). This work was supported in part by the NOAA Cooperative Agreement with CIRES, NA17OAR4320101. PTR-MS measurements aboard the NASA DC-8 during SEAC4RS and DISCOVER-AQ were supported by the Austrian Federal Ministry for Transport, Innovation and Technology (bmvit, FFG, ASAP). Formaldehyde measurements during SENEX were supported by US EPA Science to Achieve Results (STAR) program Grant 83540601. J. L. Jimenez and P. Campuzano-Jost were supported by the NASA grants #80NSSC18K0630 and #80NSSC21K1451. B. Roozitalab was supported in part by the NCAR as the Ralph Cicerone fellow of the Atmospheric Chemistry Observations and Modeling Laboratory.en_US
dc.description.urihttps://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2021MS002889en_US
dc.format.extent32 pagesen_US
dc.genrejournal articlesen_US
dc.identifierdoi:10.13016/m28f4j-8ojg
dc.identifier.citationSchwantes, R. H., Lacey, F. G., Tilmes, S., Emmons, L. K., Lauritzen, P. H., Walters, S., et al. (2022). Evaluating the impact of chemical complexity and horizontal resolution on tropospheric ozone over the conterminous US with a global variable resolution chemistry model. Journal of Advances in Modeling Earth Systems, 14, e2021MS002889. https://doi.org/10.1029/2021MS002889en_US
dc.identifier.urihttps://doi.org/10.1029/2021MS002889
dc.identifier.urihttp://hdl.handle.net/11603/28783
dc.language.isoen_USen_US
dc.publisherAGUen_US
dc.relation.isAvailableAtThe University of Maryland, Baltimore County (UMBC)
dc.relation.ispartofUMBC Joint Center for Earth Systems Technology
dc.relation.ispartofUMBC Faculty Collection
dc.rightsThis work was written as part of one of the author's official duties as an Employee of the United States Government and is therefore a work of the United States Government. In accordance with 17 U.S.C. 105, no copyright protection is available for such works under U.S. Law.*
dc.rightsPublic Domain Mark 1.0*
dc.rights.urihttp://creativecommons.org/publicdomain/mark/1.0/*
dc.titleEvaluating the Impact of Chemical Complexity and Horizontal Resolution on Tropospheric Ozone Over the Conterminous US With a Global Variable Resolution Chemistry Modelen_US
dc.typeTexten_US
dcterms.creatorhttps://orcid.org/0000-0001-6586-4043en_US

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