Rapid SO<sub>2</sub> emission reductions significantly increase tropospheric ammonia concentrations over the North China Plain

<p>The North China Plain has been identified as a significant hotspot of ammonia (<span class="inline-formula">NH<sub>3</sub></span>) due to extensive agricultural activities. Satellite observations suggest a significant increase of about 30&thinsp;% in tr...

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Bibliographic Details
Main Authors: M. Liu, X. Huang, Y. Song, T. Xu, S. Wang, Z. Wu, M. Hu, L. Zhang, Q. Zhang, Y. Pan, X. Liu, T. Zhu
Format: Article
Language:English
Published: Copernicus Publications 2018-12-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/18/17933/2018/acp-18-17933-2018.pdf
Description
Summary:<p>The North China Plain has been identified as a significant hotspot of ammonia (<span class="inline-formula">NH<sub>3</sub></span>) due to extensive agricultural activities. Satellite observations suggest a significant increase of about 30&thinsp;% in tropospheric gas-phase <span class="inline-formula">NH<sub>3</sub></span> concentrations in this area during 2008–2016. However, the estimated <span class="inline-formula">NH<sub>3</sub></span> emissions decreased slightly by 7&thinsp;% because of changes in Chinese agricultural practices, i.e., the transition in fertilizer types from ammonium carbonate fertilizer to urea, and in the livestock rearing system from free-range to intensive farming. We note that the emissions of sulfur dioxide (<span class="inline-formula">SO<sub>2</sub></span>) have rapidly declined by about 60&thinsp;% over the recent few years. By integrating measurements from ground and satellite, a long-term anthropogenic <span class="inline-formula">NH<sub>3</sub></span> emission inventory, and chemical transport model simulations, we find that this large <span class="inline-formula">SO<sub>2</sub></span> emission reduction is responsible for the <span class="inline-formula">NH<sub>3</sub></span> increase over the North China Plain. The simulations for the period 2008–2016 demonstrate that the annual average sulfate concentrations decreased by about 50&thinsp;%, which significantly weakens the formation of ammonium sulfate and increases the average proportions of gas-phase <span class="inline-formula">NH<sub>3</sub></span> within the total <span class="inline-formula">NH<sub>3</sub></span> column concentrations from 26&thinsp;% (2008) to 37&thinsp;% (2016). By fixing <span class="inline-formula">SO<sub>2</sub></span> emissions of 2008 in those multi-year simulations, the increasing trend of the tropospheric <span class="inline-formula">NH<sub>3</sub></span> concentrations is not observed. Both the decreases in sulfate and increases in <span class="inline-formula">NH<sub>3</sub></span> concentrations show highest values in summer, possibly because the formation of sulfate aerosols is more sensitive to <span class="inline-formula">SO<sub>2</sub></span> emission reductions in summer than in other seasons. Besides, the changes in <span class="inline-formula">NO<sub><i>x</i></sub></span> emissions and meteorological conditions both decreased the <span class="inline-formula">NH<sub>3</sub></span> column concentrations by about 3&thinsp;% in the study period. Our simulations suggest that the moderate reduction in <span class="inline-formula">NO<sub><i>x</i></sub></span> emissions (16&thinsp;%) favors the formation of particulate nitrate by elevating ozone concentrations in the lower troposphere.</p>
ISSN:1680-7316
1680-7324