资源环境科技发展态势分析平台

Peatlands are among the largest natural sources of atmospheric methane (CH₄) worldwide. Peatland emissions are projected to increase under climate change, as rising temperatures and shifting precipitation accelerate microbial metabolic pathways favorable for CH₄ production. However, how these changing environmental factors will impact peatland emissions over the long term remains unknown. Here, we investigate a novel dataset spanning an exceptionally long 11 years to analyze the influence of soil temperature and water table elevation on peatland CH₄ emissions. We show that higher water tables dampen the springtime increases in CH₄ emissions as well as their subsequent decreases during late summer to fall. These results imply that any hydro‐climatological changes in northern peatlands that shift seasonal water availability from winter to summer will increase annual CH₄ emissions, even if temperature remains unchanged. Therefore, advancing hydrological understanding in peatland watersheds will be crucial for improving predictions of CH₄ emissions.