Abstract
We use the global three-dimensional Goddard Earth Observing System chemical transport model with the Universal tropospheric–stratospheric Chemistry eXtension mechanism to examine the contributions of the chemical processes to summertime O3 in the upper troposphere and lower stratosphere (UTLS) over the Tibetan Plateau and the South Asian monsoon region (TP/SASM). Simulated UTLS O3 concentrations are evaluated by comparisons with Microwave Limb Sounder products and net chemical production of O3 (NPO3) are evaluated by comparisons with model results in previous studies. Simulations show that the chemical processes lead to an increase in O3 concentration, which is opposite to the effect of O3 transport in the UTLS over the TP/SASM region throughout the boreal summer. NPO3 in UTLS over the TP/SASM region is the largest in summer. Elevated values (0.016–0.020 Tg year−1) of the seasonal mean NPO3 are simulated to locate at 100 hPa in the TP/SASM region, where the mixing ratios of O3 are low and those of O3 precursors (NOx, VOCs, and CO) are high. The high concentrations of O3 precursors (NOx, VOCs, and CO) together with the active photochemical reactions of NO2 in the UTLS over the TP/SASM region during summertime could be important reasons for the enhancement of \({\text{NP}}_{{{\text{O}}_{3} }}\) over the studied region.
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Acknowledgements
This work was supported by the Science and Technology Commission of Shanghai (Grant No. 16DZ1204607), the National Natural Science Foundation of China (Grant Nos. 91644223, 91637101, and 91744311), and the Shanghai Meteorological Service (Grant No. QM2017015). We gratefully acknowledge NASA, United States, for providing the MLS data on their website.
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Gu, Y., Liao, H., Xu, J. et al. The chemical effects on the summertime ozone in the upper troposphere and lower stratosphere over the Tibetan Plateau and the South Asian monsoon region. Meteorol Atmos Phys 131, 431–441 (2019). https://doi.org/10.1007/s00703-018-0581-x
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DOI: https://doi.org/10.1007/s00703-018-0581-x