Simulation of the impact of thunderstorm activity on atmospheric gas composition

• Published in: Izvestiya. Atmospheric and oceanic physics 2010-08, Vol.46 (4), p.451-467
• Main Authors: Smyshlyaev, S. P., Mareev, E. A., Galin, V. Ya
• Format: Article
• Language: English
• Subjects: Atmosphere; Atmospheric chemistry; Atmospheric models; Climate models; Climatology; Earth and Environmental Science; Earth Sciences; Experiments; Gases; Geophysics/Geodesy; Hydroxyl radicals; Marine; Nitrogen oxides; Ozone; Photochemicals; Storms; Stratosphere; Troposphere
• ISSN: 0001-4338; 1555-628X
• DOI: 10.1134/S0001433810040043

A chemistry-climate model of the lower and middle atmosphere has been used to estimate the sensitivity of the atmospheric gas composition to the rate of thunderstorm production of nitrogen oxides at upper tropospheric and lower stratospheric altitudes. The impact that nitrogen oxides produced by lightning have on the atmospheric gas composition is treated as a subgrid-scale process and included in the model parametrically. The natural uncertainty in the global production rate of nitrogen oxides in lightning flashes was specified within limits from 2 to 20 Tg N/year. Results of the model experiments have shown that, due to the variability of thunderstorm-produced nitrogen oxides, their concentration in the upper troposphere and lower stratosphere can vary by a factor of 2 or 3, which, given the influence of nitrogen oxides on ozone and other gases, creates the potential for a strong perturbation of the atmospheric gas composition and thermal regime. Model calculations have shown the strong sensitivity of ozone and the OH hydroxyl to the amount of lightning nitrogen oxides at different atmospheric altitudes. These calculations demonstrate the importance of nitrogen oxides of thunderstorm origin for the balance of atmospheric odd ozone and gases linked to it, such as ozone and hydroxyl radicals. Our results demonstrate that one important task is to raise the accuracy of estimates of the rate of nitrogen oxide production by lightning discharges and to use physical parametrizations that take into account the local lightning effects and feedbacks arising in this case rather than climatological data in models of the gas composition and general circulation of the atmosphere.