A stratospheric prognostic ozone for seamless Earth system models: performance, impacts and future

• Published in: Atmospheric Chemistry and Physics
• Main Authors: Monge-Sanz, Beatriz M., Bozzo, Alessio, Byrne, Nicholas, Chipperfield, Martyn P., Diamantakis, Michail, Flemming, Johannes, Gray, Lesley J., Hogan, Robin J., Jones, Luke, Magnusson, Linus, Polichtchouk, Inna, Shepherd, Theodore G., Wedi, Nils, Weisheimer, Antje
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2022
• Subjects: Antarc*; Antarctic; North Atlantic; North Atlantic oscillation
• Online Access: https://centaur.reading.ac.uk/104479/; https://centaur.reading.ac.uk/104479/2/acp-22-4277-2022.pdf; https://centaur.reading.ac.uk/104479/1/acp-2020-1261-manuscript-version5.pdf

We have implemented a new stratospheric ozone model in the European Centre for Medium-Range Weather Forecasts (ECMWF) system and tested its performance for different timescales to assess the impact of stratospheric ozone on meteorological fields. We have used the new ozone model to provide prognostic ozone in medium-range and long-range (seasonal) experiments, showing the feasibility of this ozone scheme for a seamless numerical weather prediction (NWP) modelling approach. We find that the stratospheric ozone distribution provided by the new scheme in ECMWF forecast experiments is in very good agreement with observations, even for unusual meteorological conditions such as Arctic stratospheric sudden warmings (SSWs) and Antarctic polar vortex events like the vortex split of year 2002. To assess the impact it has on meteorological variables, we have performed experiments in which the prognostic ozone is interactive with radiation. The new scheme provides a realistic ozone field able to improve the description of the stratosphere in the ECMWF system, as we find clear reductions of biases in the stratospheric forecast temperature. The seasonality of the Southern Hemisphere polar vortex is also significantly improved when using the new ozone model. In medium-range simulations we also find improvements in high-latitude tropospheric winds during the SSW event considered in this study. In long-range simulations, the use of the new ozone model leads to an increase in the correlation of the winter North Atlantic Oscillation (NAO) index with respect to ERA-Interim and an increase in the signal-to-noise ratio over the North Atlantic sector. In our study we show that by improving the description of the stratospheric ozone in the ECMWF system, the stratosphere–troposphere coupling improves. This highlights the potential benefits of this new ozone model to exploit stratospheric sources of predictability and improve weather predictions over Europe on a range of timescales.