Why Permafrost Thaw Triggers Nonlinear Methane Release Through Thermokarst Lake Formation
永久冻土融化为何通过热喀斯特湖形成引发非线性甲烷释放
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Thermokarst lakes form when ground ice melts unevenly, causing surface subsidence and subsequent water accumulation in depressions.
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Submerged lake sediments create anaerobic conditions ideal for methanogenic archaea, accelerating decomposition of millennia-old organic matter.
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