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dc.contributor.authorChen, Dan
dc.contributor.authorYuxuan, Wang
dc.contributor.authorMcElroy, Michael Brendon
dc.contributor.authorHe, Kebin
dc.contributor.authorYantosca, Robert M.
dc.contributor.authorLe Sager, Philippe
dc.date.accessioned2011-07-22T19:30:13Z
dc.date.issued2009
dc.identifier.citationChen, Dan, Yuxuan Wang, Michael B. McElroy, Kebin He, Robert M. Yantosca, and Philippe Le Sager. 2009. Regional CO pollution in China simulated by the high-resolution nested-grid GEOS-Chem model. Atmospheric Chemistry and Physics Discussions 9: 5853-5887.en_US
dc.identifier.issn1680-7367en_US
dc.identifier.urihttp://nrs.harvard.edu/urn-3:HUL.InstRepos:5029363
dc.description.abstractAn updated version of the nested-grid GEOS-Chem model is developed allowing for higher horizontal (0.5°×0.667°) and vertical resolution as compared to global models. CO transport over a heavily polluted region, the Beijing-Tianjin-Hebei (BTH) city cluster in China, and the pattern of outflow from East China in summertime are investigated. Comparison of the nested-grid with global models indicates that the fine-resolution nested-grid model is capable of resolving individual cities with high associated emission intensities. The nested-grid model indicates the presence of a high CO column density over the Sichuan Basin in summer, attributable to the low-level stationary vortex associated with the Basin's topographical features. The nested-grid model provides good agreement also with measurements from a suburban monitoring site in Beijing during summer 2005. Tagged CO simulation results suggest that regional emissions make significant contributions to elevated CO levels over Beijing on polluted days and that the southeastward moving cyclones bringing northwest winds to Beijing are the key meteorological mechanisms responsible for dispersion of pollution over Beijing in summer. Overall CO fluxes to the NW Pacific from Asia are found to decrease by a factor of 3–4 from spring to summer. Much of the seasonal change is driven by decreasing fluxes from India and Southeast Asia in summer, while fluxes from East China are only 30% lower in summer than in spring. Compared to spring, summertime outflow from Chinese source regions is strongest at higher latitudes (north of 35° N). The deeper convection in summer transporting CO to higher altitudes where export is more efficient is largely responsible for enhanced export in summer.en_US
dc.description.sponsorshipEngineering and Applied Sciencesen_US
dc.language.isoen_USen_US
dc.publisherCopernicus Publicationsen_US
dc.relation.isversionofhttp://www.atmos-chem-phys-discuss.net/9/5853/2009/en_US
dc.relation.hasversionhttp://acmg.seas.harvard.edu/publications/danchen2009a.pdfen_US
dash.licenseOAP
dc.titleRegional CO Pollution in China Simulated by the High-Resolution Nested-Grid GEOS-Chem Modelen_US
dc.typeJournal Articleen_US
dc.description.versionAccepted Manuscripten_US
dc.relation.journalAtmospheric Chemistry and Physics Discussionsen_US
dash.depositing.authorMcElroy, Michael Brendon
dc.date.available2011-07-22T19:30:13Z
dc.identifier.doi10.5194/acp-9-3825-2009
dash.contributor.affiliatedYantosca, Robert
dash.contributor.affiliatedMcElroy, Michael
dash.contributor.affiliatedLe Sager, P


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