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dc.contributor.authorIm, Ulas
dc.contributor.authorBianconi, Roberto
dc.contributor.authorSolazzo, Efisio
dc.contributor.authorKioutsioukis, Ioannis
dc.contributor.authorBadia, Alba
dc.contributor.authorBalzarini, Alessandra
dc.contributor.authorBaró, Rocío
dc.contributor.authorBellasio, Roberto
dc.contributor.authorBrunner, Dominik
dc.contributor.authorChemel, C.
dc.contributor.authorCurci, Gabriele
dc.contributor.authorFlemming, Johannes
dc.contributor.authorForkel, Renate
dc.contributor.authorGiordano, Lea
dc.contributor.authorJiménez-Guerrero, Pedro
dc.contributor.authorHirtl, Marcus
dc.contributor.authorHodzic, Alma
dc.contributor.authorHonzak, Luka
dc.contributor.authorJorba, Oriol
dc.contributor.authorKnote, Christoph
dc.contributor.authorKuenen, Jeroen J.P.
dc.contributor.authorMakar, Paul A.
dc.contributor.authorManders-Groot, Astrid
dc.contributor.authorNeal, Lucy
dc.contributor.authorPérez, Juan L.
dc.contributor.authorPirovano, Guido
dc.contributor.authorPouliot, George
dc.contributor.authorSan Jose, Roberto
dc.contributor.authorSavage, Nicholas
dc.contributor.authorSchroder, Wolfram
dc.contributor.authorSokhi, Ranjeet S.
dc.contributor.authorSyrakov, Dimiter
dc.contributor.authorTorian, Alfreida
dc.contributor.authorTuccella, Paolo
dc.contributor.authorWerhahn, Johannes
dc.contributor.authorWolke, Ralf
dc.contributor.authorYahya, Khairunnisa
dc.contributor.authorZabkar, Rahela
dc.contributor.authorZhang, Yang
dc.contributor.authorZhang, Junhua
dc.contributor.authorHogrefe, Christian
dc.contributor.authorGalmarini, Stefano
dc.date.accessioned2015-08-18T10:28:36Z
dc.date.available2015-08-18T10:28:36Z
dc.date.issued2015-08
dc.identifier.citationIm , U , Bianconi , R , Solazzo , E , Kioutsioukis , I , Badia , A , Balzarini , A , Baró , R , Bellasio , R , Brunner , D , Chemel , C , Curci , G , Flemming , J , Forkel , R , Giordano , L , Jiménez-Guerrero , P , Hirtl , M , Hodzic , A , Honzak , L , Jorba , O , Knote , C , Kuenen , J J P , Makar , P A , Manders-Groot , A , Neal , L , Pérez , J L , Pirovano , G , Pouliot , G , San Jose , R , Savage , N , Schroder , W , Sokhi , R S , Syrakov , D , Torian , A , Tuccella , P , Werhahn , J , Wolke , R , Yahya , K , Zabkar , R , Zhang , Y , Zhang , J , Hogrefe , C & Galmarini , S 2015 , ' Evaluation of operational on-line-coupled regional air quality models over Europe and North America in the context of AQMEII phase 2 : Part I: Ozone ' , Atmospheric Environment , vol. 115 , pp. 404-420 . https://doi.org/10.1016/j.atmosenv.2014.09.042
dc.identifier.issn1352-2310
dc.identifier.otherRIS: urn:6B4A7A632A062D30D6BB1722CD792862
dc.identifier.otherORCID: /0000-0001-9785-1781/work/104213777
dc.identifier.urihttp://hdl.handle.net/2299/16281
dc.description.abstractThe second phase of the Air Quality Model Evaluation International Initiative (AQMEII) brought together sixteen modeling groups from Europe and North America, running eight operational online-coupled air quality models over Europe and North America on common emissions and boundary conditions. With the advent of online-coupled models providing new capability to quantify the effects of feedback processes, the main aim of this study is to compare the response of coupled air quality models to simulate levels of O3 over the two continental regions. The simulated annual, seasonal, continental and sub-regional ozone surface concentrations and vertical profiles for the year 2010 have been evaluated against a large observational database from different measurement networks operating in Europe and North America. Results show a general model underestimation of the annual surface ozone levels over both continents reaching up to 18% over Europe and 22% over North America. The observed temporal variations are successfully reproduced with correlation coefficients larger than 0.8. Results clearly show that the simulated levels highly depend on the meteorological and chemical configurations used in the models, even within the same modeling system. The seasonal and sub-regional analyses show the models' tendency to overestimate surface ozone in all regions during autumn and underestimate in winter. Boundary conditions strongly influence ozone predictions especially during winter and autumn, whereas during summer local production dominates over regional transport. Daily maximum 8-h averaged surface ozone levels below 50–60 μg m−3 are overestimated by all models over both continents while levels over 120–140 μg m−3 are underestimated, suggesting that models have a tendency to severely under-predict high O3 values that are of concern for air quality forecast and control policy applications.en
dc.format.extent4902029
dc.language.isoeng
dc.relation.ispartofAtmospheric Environment
dc.titleEvaluation of operational on-line-coupled regional air quality models over Europe and North America in the context of AQMEII phase 2 : Part I: Ozoneen
dc.contributor.institutionSchool of Physics, Astronomy and Mathematics
dc.contributor.institutionScience & Technology Research Institute
dc.contributor.institutionCentre for Atmospheric and Climate Physics Research
dc.contributor.institutionAtmospheric Dynamics & Air Quality
dc.description.statusPeer reviewed
rioxxterms.versionofrecord10.1016/j.atmosenv.2014.09.042
rioxxterms.typeJournal Article/Review
herts.preservation.rarelyaccessedtrue


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