Spatiotemporal variations of atmospheric XCH4 in China based on multiple spatially continuous satellite-derived products

J Environ Manage. 2025 Jun 26:390:126309. doi: 10.1016/j.jenvman.2025.126309. Online ahead of print.

Abstract

Spatiotemporally continuous satellite CH4 column concentrations (XCH4) are crucial for accurately assessing variations in atmospheric CH4. However, most existing studies rely on single or a limited number of spatiotemporally discontinuous XCH4 satellite observations. This study evaluates the accuracy of three newly developed spatiotemporally continuous reconstructed XCH4 products -Song-XCH4, Wang-XCH4, and Jin-XCH4 using ground-based data from the Total Carbon Column Observing Network (TCCON) and the World Data Centre for Greenhouse Gases (WDCGG), and analyzes the spatiotemporal variations of XCH4 across China. Results show that: 1) All three products exhibit good consistency with ground-based observations, except the Lulin station. The three products align better with TCCON data overall than with WDCGG data, with Wang-XCH4 demonstrates the best overall agreement. 2) All three products consistently reveal a gradient from high values in the southeast to low values in the northwest of China. The national annual average XCH4 from Wang-XCH4 is approximately 10 ppb higher than that from Song and Jin-XCH4, with the largest regional average differences (18.0-33.3 ppb) observed in North, Central, and Southwest China. 3) Although the national annual mean XCH4 increased significantly at an approximate rate of 8.0 ppb yr-1 from 2010 to 2020, Song-XCH4 showed greater spatial variability. It exhibited the highest seasonal growth rates in summer and autumn (8.0 ppb) and the lowest in spring (7.4 ppb), whereas Wang-XCH4 showed the fastest increase in autumn (8.1 ppb) but the slowest in summer (6.9 ppb). Our findings highlight the importance of exercising caution when using satellite-based reconstructed XCH4 products.

Keywords: China; GOSAT; Satellite remote sensing; Spatiotemporally continuous; TROPOMI; XCH(4).