Inverse modelling of Chinese NO<sub><i>x</i></sub> emissions using deep learning: integrating in situ observations with a satellite-based chemical reanalysis

oleh: T.-L. He, T.-L. He, D. B. A. Jones, K. Miyazaki, K. W. Bowman, Z. Jiang, X. Chen, R. Li, Y. Zhang, K. Li

Format: Article
Diterbitkan: Copernicus Publications 2022-11-01

Deskripsi

<p>Nitrogen dioxide (<span class="inline-formula">NO<sub>2</sub></span>) column density measurements from satellites have been widely used in constraining emissions of nitrogen oxides (<span class="inline-formula">NO<sub><i>x</i></sub></span> <span class="inline-formula">=</span> NO <span class="inline-formula">+</span> <span class="inline-formula">NO<sub>2</sub></span>). However, the utility of these measurements is impacted by reduced observational coverage due to cloud cover and their reduced sensitivity toward the surface. Combining the information from satellites with surface observations of <span class="inline-formula">NO<sub>2</sub></span> will provide greater constraints on emission estimates of <span class="inline-formula">NO<sub><i>x</i></sub></span>. We have developed a deep-learning (DL) model to integrate satellite data and in situ observations of surface <span class="inline-formula">NO<sub>2</sub></span> to estimate <span class="inline-formula">NO<sub><i>x</i></sub></span> emissions in China. A priori information for the DL model was obtained from satellite-derived emissions from the Tropospheric Chemistry Reanalysis (TCR-2). A two-stage training strategy was used to integrate in situ measurements from the China Ministry of Ecology and Environment (MEE) observation network with the TCR-2 data. The DL model is trained from 2005 to 2018 and evaluated for 2019 and 2020. The DL model estimated a source of 19.4 Tg NO for total Chinese <span class="inline-formula">NO<sub><i>x</i></sub></span> emissions in 2019, which is consistent with the TCR-2 estimate of 18.5 <span class="inline-formula">±</span> 3.9 Tg NO and the 20.9 Tg NO suggested by the Multi-resolution Emission Inventory for China (MEIC). Combining the MEE data with TCR-2, the DL model suggested higher <span class="inline-formula">NO<sub><i>x</i></sub></span> emissions in some of the less-densely populated provinces, such as Shaanxi and Sichuan, where the MEE data indicated higher surface <span class="inline-formula">NO<sub>2</sub></span> concentrations than TCR-2. The DL model also suggested a faster recovery of <span class="inline-formula">NO<sub><i>x</i></sub></span> emissions than TCR-2 after the Chinese New Year (CNY) holiday in 2019, with a recovery time scale that is consistent with Baidu “Qianxi” mobility data. In 2020, the DL-based analysis estimated about a 30 % reduction in <span class="inline-formula">NO<sub><i>x</i></sub></span> emissions in eastern China during the COVID-19 lockdown period, relative to pre-lockdown levels. In particular, the maximum emission reductions were 42 % and 30 % for the Jing-Jin-Ji (JJJ) and the Yangtze River Delta (YRD) mega-regions, respectively. Our results illustrate the potential utility of the DL model as a complementary tool for conventional data-assimilation approaches for air quality applications.</p>