Articles | Volume 7, issue 1
Geosci. Model Dev., 7, 283–302, 2014

Special issue: Monitoring atmospheric composition and climate, research in...

Geosci. Model Dev., 7, 283–302, 2014

Model evaluation paper 13 Feb 2014

Model evaluation paper | 13 Feb 2014

Regional scale ozone data assimilation using an ensemble Kalman filter and the CHIMERE chemical transport model

B. Gaubert1, A. Coman1, G. Foret1, F. Meleux2, A. Ung2, L. Rouil2, A. Ionescu3, Y. Candau3, and M. Beekmann1 B. Gaubert et al.
  • 1LISA, CNRS/INSU UMR7583, Université Paris-Est Créteil et Université Paris Diderot, Institut Pierre Simon Laplace, 94010 Créteil, France
  • 2Institut National de l'Environnement Industriel et des Risques, INERIS, Parc Technologique ALATA-B.P. No. 2, 60550 Verneuil en Halatte, France
  • 3Centre d'Études et de Recherche en Thermique, Environnement et Systèmes EA 3481, Université Paris-Est Créteil, 94010 Créteil, France

Abstract. An ensemble Kalman filter (EnKF) has been coupled to the CHIMERE chemical transport model in order to assimilate ozone ground-based measurements on a regional scale. The number of ensembles is reduced to 20, which allows for future operational use of the system for air quality analysis and forecast. Observation sites of the European ozone monitoring network have been classified using criteria on ozone temporal variability, based on previous work by Flemming et al. (2005). This leads to the choice of specific subsets of suburban, rural and remote sites for data assimilation and for evaluation of the reference run and the assimilation system. For a 10-day experiment during an ozone pollution event over Western Europe, data assimilation allows for a significant improvement in ozone fields: the RMSE is reduced by about a third with respect to the reference run, and the hourly correlation coefficient is increased from 0.75 to 0.87. Several sensitivity tests focus on an a posteriori diagnostic estimation of errors associated with the background estimate and with the spatial representativeness of observations. A strong diurnal cycle of both these errors with an amplitude up to a factor of 2 is made evident. Therefore, the hourly ozone background error and the observation error variances are corrected online in separate assimilation experiments. These adjusted background and observational error variances provide a better uncertainty estimate, as verified by using statistics based on the reduced centered random variable. Over the studied 10-day period the overall EnKF performance over evaluation stations is found relatively unaffected by different formulations of observation and simulation errors, probably due to the large density of observation sites. From these sensitivity tests, an optimal configuration was chosen for an assimilation experiment extended over a three-month summer period. It shows a similarly good performance as the 10-day experiment.