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DOI10.5194/acp-19-14211-2019
Analysis of summer O3 in the Madrid air basin with the LOTOS-EUROS chemical transport model
Escudero M.; Segers A.; Kranenburg R.; Querol X.; Alastuey A.; Borge R.; De La Paz D.; Gangoiti G.; Schaap M.
发表日期2019
ISSN16807316
起始页码14211
结束页码14232
卷号19期号:22
英文摘要Tropospheric O3 remains a major air-quality issue in the Mediterranean region. The combination of large anthropogenic emissions of precursors, transboundary contributions, a warm and dry aestival climate, and topographical features results in severe cases of photochemical pollution. Chemical transport models (CTMs) are essential tools for studying O3 dynamics and for assessing mitigation measures, but they need to be evaluated specifically for each air basin. In this study, we present an optimisation of the LOTOS-EUROS CTM for the Madrid air basin. Five configurations using different meteorological datasets (from the European Centre for Medium-Range Weather Forecast, ECMWF; and the Weather Research and Forecasting Model, WRF), horizontal resolution and number of vertical levels were compared for July 2016. LOTOS-EUROS responded satisfactorily in the five configurations reproducing observations of surface O3 with notable correlation and reduced bias and errors. However, the best-fit simulations for surface O3 were obtained by increasing spatial resolution and using a large number of vertical levels to reproduce vertical transport phenomena and the formation of reservoir layers. Using the optimal configuration obtained in the evaluation, three characteristic events have been described: recirculation (REC) episodes and northern and southern advection (NAD and SAD, respectively) events. REC events were found to produce the highest O3 due to the reduced ventilation associated with low wind speeds and the contribution of reservoir layers formed by vertical transport of O3 formed near the surface in the previous days of the event. NAD events, usually associated with higher wind speeds, present the lowest ground-level O3 concentrations in the region. During SAD episodes, external contributions along with low wind speeds allow O3 to increase considerably but not as much as in REC events because steady southerly winds disperse local emissions and hinder the formation of reservoir layers. © Author(s) 2019. This work is distributed under the Creative Commons Attribution 4.0 License.
语种英语
scopus关键词air quality; atmospheric chemistry; atmospheric transport; concentration (composition); data set; oxygen; seasonal variation; troposphere; Madrid Basin; Spain
来源期刊Atmospheric Chemistry and Physics
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/144021
作者单位Centro Universitario de la Defensa (CUD) de Zaragoza, Academia General Militar, Ctra. de Huesca s/n, Zaragoza, 50090, Spain; TNO, P.O. Box 80015, Utrecht, 3584 TA, Netherlands; Institute of Environmental Assessment and Water Research (IDAEA-CSIC), Jordi Girona 18-26, Barcelona, 08034, Spain; Department of Chemical and Environmental Engineering, Technical University of Madrid (UPM), c/José Gutiérrez Abascal 2, Madrid, 28006, Spain; Escuela Técnica Superior de Ingeniería de Bilbao, Departamento de Ingeniería Química y Del Medio Ambiente, Universidad Del País Vasco (UPV/EHU), Urkixo Zumarkalea, s/n, Bilbao, 48013, Spain
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Escudero M.,Segers A.,Kranenburg R.,et al. Analysis of summer O3 in the Madrid air basin with the LOTOS-EUROS chemical transport model[J],2019,19(22).
APA Escudero M..,Segers A..,Kranenburg R..,Querol X..,Alastuey A..,...&Schaap M..(2019).Analysis of summer O3 in the Madrid air basin with the LOTOS-EUROS chemical transport model.Atmospheric Chemistry and Physics,19(22).
MLA Escudero M.,et al."Analysis of summer O3 in the Madrid air basin with the LOTOS-EUROS chemical transport model".Atmospheric Chemistry and Physics 19.22(2019).
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