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Ozone Source Apportionment to Quantify Local-to-Continental Source Contributions to Episodic Events in Northern Iberia

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Air Pollution Modeling and its Application XXV (ITM 2016)

Abstract

We present here a study of a number of ozone episodes in Northern Iberia (NIB) during the warm season of 2010 (April 1–September 30) using WRF and CAMx models. The episodes were selected after a detailed analysis of the ozone concentrations registered by the Air Quality Monitoring Network of the Basque Country (AQNBC), and rural background stations of the European Air Quality Database AirBase located in Northern Iberia. Preliminary results of the analysis of an early summer episode (24–26 June) are shown. For the first time during this type of episodes, it is shown that in the stations where the EU information threshold is exceeded frequently, there is an important contribution from local and regional sources, but the causative factor of high levels of ozone is the transport from medium-long range sources (France and Central Europe). Ozone production is mainly NOx limited.

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Acknowledgements

This work was supported by Ministry of Economy and Competitiveness through the project CTM2013-45223-P (PRORAT), UPV/EHU UFI (11/47) and Ministry of Education, Culture and Sport under the JC2015-00414 José Castillejo mobility grant to Sáez de Cámara. The authors wish to thank the Basque Government for providing the meteorological and air quality data, the European Environmental Agency for its AirBase data, ECMWF for materorological data and Denier van der Goon from TNO for anthropogenic emissions.

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Correspondence to Estíbaliz Sáez de Cámara .

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de Cámara, E.S., Gangoiti, G., Alonso, L., Valdenebro, V., Aksoyoglu, S., Oikonomakis, E. (2018). Ozone Source Apportionment to Quantify Local-to-Continental Source Contributions to Episodic Events in Northern Iberia. In: Mensink, C., Kallos, G. (eds) Air Pollution Modeling and its Application XXV. ITM 2016. Springer Proceedings in Complexity. Springer, Cham. https://doi.org/10.1007/978-3-319-57645-9_57

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