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Implementation and evaluation of a new methane model within a dynamic global vegetation model: LPJ-WHyMe v1.3

机译:在动态全球植被模型中实施和评估新的甲烷模型:LPJ-WHyMe v1.3

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For the first time, a model that simulates methane emissions from northern peatlands is incorporated directly into a dynamic global vegetation model. The model, LPJ-WHyMe (LPJ-Wetland Hydrology and Methane), was previously modified in order to simulate peatland hydrology, permafrost dynamics and peatland vegetation. LPJ-WHyMe simulates methane emissions using a mechanistic approach, although the use of some empirical relationships and parameters is unavoidable. The model simulates methane production, three pathways of methane transport (diffusion, plant-mediated transport and ebullition) and methane oxidation. Two sensitivity tests were conducted, first to identify the most important factors influencing methane emissions and secondly to justify the choice of parameters. A comparison of model results to observations from seven sites revealed in general good agreement but also highlighted some problems. Circumpolar methane emissions for the period 1961–1990 were estimated to be between 40.8 and 73.7 Tg CH4 a-1.
机译:第一次将模拟北部泥炭地甲烷排放的模型直接纳入动态的全球植被模型中。先前对模型LPJ-WHyMe(LPJ-湿地水文学和甲烷)进行了修改,以模拟泥炭地的水文,多年冻土动力学和泥炭地植被。 LPJ-WHyMe使用机械方法模拟甲烷排放,尽管不可避免地要使用一些经验关系和参数。该模型模拟甲烷的产生,甲烷运输的三个途径(扩散,植物介导的运输和沸腾)和甲烷氧化。进行了两次敏感性测试,首先确定影响甲烷排放的最重要因素,其次证明参数选择的合理性。将模型结果与七个地点的观察结果进行比较,发现总体上吻合良好,但也突出了一些问题。据估计,1961-1990年期间的极极性甲烷排放量在40.8至73.7 Tg CH 4 a -1 之间。

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