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However, current understanding of how this CH\n                    <jats:sub>4<\/jats:sub>\n                    sink responds to global climate change remains limited. To address this, we integrated 1092 observational data points to construct a dataset covering multiple global change factors and used meta\u2010analysis to quantify the response mechanisms of the upland CH\n                    <jats:sub>4<\/jats:sub>\n                    sink. Results show that warming, reduced precipitation, and elevated carbon dioxide concentrations significantly strengthened the CH\n                    <jats:sub>4<\/jats:sub>\n                    sink, while increased precipitation and nitrogen addition weakened it. Interactive effects were also observed: low\u2010level nitrogen deposition acted antagonistically with increased precipitation, but synergistically with warming. We subsequently optimized a CH\n                    <jats:sub>4<\/jats:sub>\n                    oxidation model to explore the global distribution patterns and future trends under different climate scenarios. The current global upland soil CH\n                    <jats:sub>4<\/jats:sub>\n                    sink is estimated at approximately 37 Tg year\n                    <jats:sup>\u22121<\/jats:sup>\n                    and generally shows an increasing temporal trend. Spatially, the sink exhibits heterogeneity: a greater extent of desert areas in the Northern Hemisphere leads to a lower CH\n                    <jats:sub>4<\/jats:sub>\n                    sink per unit area compared to the Southern Hemisphere. Future spatiotemporal trends of the soil CH\n                    <jats:sub>4<\/jats:sub>\n                    sink will depend on the climate pathway. Under the Shared Socioeconomic Pathway (SSP) 1\u20132.6 scenario, the CH\n                    <jats:sub>4<\/jats:sub>\n                    sink declines over time, whereas under SSP5\u20108.5, it follows a unimodal trajectory. Variations in the soil CH\n                    <jats:sub>4<\/jats:sub>\n                    sink also differ across regions. These changes are primarily associated with atmospheric CH\n                    <jats:sub>4<\/jats:sub>\n                    concentrations under different climate pathways, as well as alterations in soil temperature and moisture resulting from various climate change drivers. These findings underscore the importance of the upland CH\n                    <jats:sub>4<\/jats:sub>\n                    sink in the global CH\n                    <jats:sub>4<\/jats:sub>\n                    cycle and significantly advance our understanding of its response mechanisms to climate change.\n                  <\/jats:p>","DOI":"10.1111\/gcb.70747","type":"journal-article","created":{"date-parts":[[2026,2,16]],"date-time":"2026-02-16T09:28:03Z","timestamp":1771234083000},"update-policy":"https:\/\/doi.org\/10.1002\/crossmark_policy","source":"Crossref","is-referenced-by-count":9,"title":["Upland Methane Sinks Under Climate Change: Global Patterns, Drivers and Trends"],"prefix":"10.1111","volume":"32","author":[{"given":"Li","family":"Cheng","sequence":"first","affiliation":[{"name":"Zhejiang Tiantong Forest Ecosystem National Observation and Research Station, Zhejiang Zhoushan Island Ecosystem Observation and Research Station, School of Ecological and Environmental 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