We find that assimilation of OMI and MLS ozone decreases the error in GEOS-Chem ozone forecasts by up to 50% in the upper troposphere and 25% near the surface compared to an assimilation-free control simulation. This result can be attributed to a combination of improved representation of stratosphere-troposphere exchange, lightning NOx emissions, and model background concentrations. The concurrent assimilation of NO2 and CO helps identifying the relative importance of these factors. For instance, model-observation mismatches of NO2 point to local deficiencies in model emissions of NO2as being the cause of some of the observed ozone discrepancies in the free-running model.
This new chemical data assimilation system leverages the expertise of NASA’s Global Modeling and Assimilation Office (GMAO) and the GEOS-Chem modeling community, making it uniquely positioned to benefit from advances in atmospheric chemistry modeling and data assimilation techniques. We discuss ongoing developments as well as challenges with respect to air quality modeling. This includes the increase in horizontal resolution to better capture fine-scale patterns that are critical for human health studies, the transition from 3D-Variational to ensemble-based 4D-Variational systems in the GMAO, and the expansion of the assimilation state vector to include emissions.