A high-resolution satellite-based map of global methane emissions reveals missing wetland, fossil fuel, and monsoon sources
A high-resolution satellite-based map of global methane emissions reveals missing wetland, fossil fuel, and monsoon sources
Xueying Yu,D. Millet,5 Authors,Jianxiong Sheng
2023 · DOI: 10.5194/acp-23-3325-2023
Atmospheric Chemistry and Physics · 21 Citations
Abstract
Abstract. We interpret space-borne observations from the
TROPOspheric Monitoring Instrument (TROPOMI) in a multi-inversion frameworkto characterize the 2018–2019 global methane budget. Evaluation of theinverse solutions indicates that simultaneous source + sink optimizationusing methane observations alone remains an ill-posed problem – even withthe dense TROPOMI sampling coverage. Employing remote carbon monoxide (CO)and hydroxyl radical (OH) observations with independent methane measurementsto distinguish between candidate solutions, we infer from TROPOMI a globalmethane source of 587 (586–589) Tg yr−1 and sink of 571 Tg yr−1 for our analysisperiod. We apply a new downscaling method to map the derived monthlyemissions to 0.1∘ × 0.1∘ resolution, using theresults to uncover key gaps in the prior methane budget. The TROPOMI datapoint to an underestimate of tropical wetland emissions (a posteriori increaseof +13 % [6 %–25 %] or 20 [7–25] Tg yr−1), with adjustments followingregional hydrology. Some simple wetland parameterizations represent thesepatterns as accurately as more sophisticated process-based models. Emissionsfrom fossil fuel activities are strongly underestimated over the Middle East(+5 [2–6] Tg yr−1 a posteriori increase) and over Venezuela. The TROPOMIobservations also reveal many fossil fuel emission hotspots missing from theprior inventory, including over Mexico, Oman, Yemen, Turkmenistan, Iran,Iraq, Libya, and Algeria. Agricultural methane sources are underestimated inIndia, Brazil, the California Central Valley, and Asia. Overall,anthropogenic sources worldwide are increased by +19 [11–31] Tg yr−1 overthe prior estimate. More than 45 % of this adjustment occurs over Indiaand Southeast Asia during the summer monsoon (+8.5 [3.1–10.7] Tg inJuly–October), likely due to rainfall-enhanced emissions from rice, manure, andlandfills/sewers, which increase during this season along with the naturalwetland source.