Climate warming will lead to changes in soil properties, which in turn will affect the uptake of methane (CH 4 ) in meadows. Currently there is artificial reclamation of alpine meadows, and the effect of reclamation on CH 4 uptake in alpine meadow ecosystems is still unclear. Therefore, we investigated the effects of warming, reclamation and their interactions on soil CH 4 uptake in alpine meadows on the Tibetan Plateau. From May to December 2021 and from March to May 2022, CH 4 uptake was determined under four treatments: control (CK), warming, reclamation and warming under reclamation. Soil C and N nutrient contents and three enzyme activities were determined in 2021, and their effects on CH 4 uptake were elucidated using the Mantel test as well as structural equation modelling. The results showed that warming significantly increased CH 4 uptake by 23.84 %, reclamation significantly reduced CH 4 uptake by 58.64 %, warming interacted with reclamation significantly reduced CH 4 uptake by 33.45 % in growing season, and warming interacted with reclamation significantly reduced CH 4 uptake by 21.46 % in the non-growing season, as compared to CK. Warming promoted CH 4 uptake by increasing soil nutrient content and increasing the activities of methane monooxygenase and soil sucrase. Reclamation reduced the content of soil soluble carbon and nitrogen and inhibited the uptake of CH 4 . Therefore, in the context of global warming, the destruction of natural grassland should be avoided as far as possible and the area of cultivated land should be rationally planned, so as to maintain the higher CH 4 uptake capacity of grassland.