Ozone assimilation in the ERA‐40 reanalysis project

By A. Dethof, Elias V. Holm. 2004

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Data assimilation: making sense of Earth Observation (2014, unknown): “…include: Levelt et al. (1998), Hólm et al. (1999), Khattatov et al. (2000), El Serafy et al. (2002), Struthers et al. (2002), Eskes et al. (2003), Dethof and Hólm (2004), Štajner and Wargan (2004), Massart et al. (2005, 2009), Segers et al. (2005), Wargan et al. (2005, 2010), Geer et al. (2006,…”
Introduction to the SPARC Reanalysis Intercomparison Project (S-RIP) and overview of the reanalysis systems (2016, background): “However, some of the reanalysis systems that assimilate ozone and produce ozone analyses (notably ERA40, ERA-Interim, and ERA-20C) nevertheless use climatological ozone fields for radiation calculations in the forecast model, rather than their respective ozone analyses, because interactions between ”
A revised linear ozone photochemistry parameterization for use in transport and general circulation models: multi-annual simulations (2007, unknown): “At ECMWF, the CD86 ozone scheme has been used for assimilation of ozone observations and some of the coefficients derived by the 2D model had to be replaced by the FL dataset in order to remove biases in the lower stratosphere (Dethof and Holm, 2004).”