资源环境科技发展态势分析平台

Ice‐wedge degradation is a wide‐spread occurrence across the circumpolar Arctic causing extreme spatial heterogeneity in water distribution, vegetation, and energy balance across landscapes. These heterogeneities influence carbon dioxide (CO₂) and methane (CH₄) fluxes, yet there is little understanding of how they effect change in landscape‐level carbon (C) gas flux over time. We measured CO₂ and CH₄ fluxes in an area undergoing ice‐wedge degradation near Prudhoe Bay, Alaska, and combined with repeat imagery analysis to estimate seasonal landscape‐level C flux response to geomorphic change. Net CO₂ and CH₄ emissions changed by ‐25% and +42% respectively, resulting in a 14% increase in seasonal CO₂‐C equivalent emissions over 69 years as ice‐wedge degradation formed water‐filled troughs. The dynamic ice‐wedge degradation/stabilization process can cause significant changes in CO₂ and CH₄ fluxes over time, and the integration of this process is important to forecasting landscape‐level C fluxes in permafrost regions abundant in ice wedges.