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首页> 外文期刊>Geoscientific Model Development Discussions >Interactive impacts of fire and vegetation dynamics on global carbon and water budget using Community Land Model version 4.5
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Interactive impacts of fire and vegetation dynamics on global carbon and water budget using Community Land Model version 4.5

机译:使用社区土地模型版本4.5,火灾和植被动态对全球碳和水预算的互动影响

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Fire plays an important role in terrestrial ecosystems. The burning of biomass affects carbon and water fluxes and vegetation distribution. To understand the effect of interactive processes of fire and ecological succession on surface carbon and water fluxes, this study employed the Community Land Model version 4.5 to conduct a series of experiments that included and excluded fire and dynamic vegetation processes. Results of the experiments that excluded the vegetation dynamics showed a global increase in net ecosystem production (NEP) in post-fire regions, whereas the inclusion of vegetation dynamics revealed a fire-induced decrease in NEP in some regions, which was depicted when the dominant vegetation type was changed from trees to grass. Carbon emissions from fires are enhanced by reduction in NEP when vegetation dynamics are considered; however, this effect is somewhat mitigated by the increase in NEP when vegetation dynamics are not considered. Fire-induced changes in vegetation modify the soil moisture profile because grasslands are more dominant in post-fire regions. This results in less moisture within the top soil layer than that in unburned regions, even though transpiration is reduced overall. These findings are different from those of previous fire model evaluations that ignored vegetation dynamics and thus highlight the importance of interactive processes between fires and vegetation dynamics in evaluating recent model developments.
机译:火在陆地生态系统中起着重要作用。生物质的燃烧影响碳和水通量以及植被分布。为了了解火灾和生态演替的互动过程对地表碳和水通量的影响,本研究使用社区土地模型4.5版进行了一系列实验,包括和排除了火灾和动态植被过程。排除植被动态的实验结果表明,火灾后地区的净生态系统产量(NEP)总体增加,而植被动态的包含则表明某些地区火灾引起的NEP下降,这在主要地区植被类型从树木变成了草地。当考虑植被动态时,通过减少NEP可以增加火灾产生的碳排放;但是,当不考虑植被动态时,NEP的增加会在某种程度上减轻这种影响。火灾引起的植被变化会改变土壤水分状况,因为草原在火灾后地区占主导地位。即使蒸腾作用总体降低,这也导致顶部土壤层的水分少于未燃烧区域的水分。这些发现与先前的火灾模型评估不同,后者忽略了植被动力学,因此强调了火灾与植被动力学之间相互作用过程在评估最新模型开发中的重要性。

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