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Globally significant changes in biological processes of the Amazon Basin: results of the Large-scale Biosphere-Atmosphere Experiment

机译:亚马逊盆地生物过程的全球重大变化:大规模生物圈-大气实验的结果

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The Amazon River, its huge basin, and the changes in biological processes that are rapidly occurring in this region are unquestionably of global significance. Hence, Global Change Biology is delighted to host a special thematic issue devoted to the Large-scale Biosphere-Atmosphere Experiment in Amazonia (LBA), which is a multinational, interdisciplinary research program led by Brazil. The goal of LBA is no less modest than its subject: to understand how Amazonia functions as a regional entity in the Earth system and how these functions are changing as a result of ongoing changes in land use. This compilation of 26 papers resulting from LBA-related research covers a broad range of topics: forest stocks of carbon (C) and nitrogen (N); fluxes of greenhouse gases and volatile organic compounds from vegetation, soils and wetlands; mapping and modeling land-use change, fire risk, and soil properties; measuring changes caused by logging, pasturing and cultivating; and new research approaches in meteorology to estimate nocturnal fluxes of C from forests and pastures. Some important new synthesis can be derived from these and other studies. The aboveground biomass of intact Amazonian forests appears to be a sink for atmospheric carbon dioxide (CO2), while the wetlands and soils are a net source of atmospheric methane (CH4) and nitrous oxide (N2O), respectively. Land-use change has, so far, had only a minor effect on basin-wide emissions of CH4 and N2O, but the net effect of deforestation and reforestation appears to be a significant net release of CO2 to the atmosphere. The sum of the 100-year global warming potentials (GWP) of these annual sources and sinks of CH4, N2O, and CO2 indicate that the Amazonian forest-river system currently may be nearly balanced in terms of the net GWP of these biogenic atmospheric gases. Of course, large uncertainties remain for these estimates, but the papers published here demonstrate tremendous progress, and also large remaining hurdles, in narrowing these uncertainties in our understanding of how Amazonia functions as a regional entity in the Earth system.
机译:毫无疑问,亚马孙河,其巨大的流域以及该地区迅速发生的生物过程变化具有全球意义。因此,全球变化生物学很高兴主办一个专门的专题课题,专门研究亚马逊地区的大型生物圈-大气层实验(LBA),这是一个由巴西牵头的跨国,跨学科研究计划。 LBA的目标不亚于其主题:了解Amazonia如何在地球系统中作为区域实体,以及这些功能由于土地用途的不断变化而如何变化。本次LBA相关研究的26篇论文的汇编涵盖了广泛的主题:碳(C)和氮(N)的森林资源;来自植被,土壤和湿地的温室气体和挥发性有机化合物的通量;绘制土地利用变化,火灾风险和土壤特性的图并建模;测量由伐木,牧草和耕种引起的变化;以及新的气象学研究方法来估算森林和牧场中碳的夜间通量。这些研究和其他研究可以得出一些重要的新合成方法。完整的亚马逊森林的地上生物量似乎是大气二氧化碳(CO2)的汇,而湿地和土壤分别是大气甲烷(CH4)和一氧化二氮(N2O)的净来源。迄今为止,土地用途的变化对整个流域的CH4和N2O排放仅产生了很小的影响,但是森林砍伐和再造林的净效应似乎是向大气中大量释放的CO2。这些每年的CH4,N2O和CO2汇和汇的100年全球变暖潜势(GWP)的总和表明,就这些生物源性大气的净全球升温潜能值而言,亚马逊河森林系统目前可能已接近平衡。 。当然,对于这些估计,仍然存在很大的不确定性,但是在我们了解亚马逊河如何在地球系统中作为区域实体发挥作用的认识方面,此处发表的论文证明了缩小这些不确定性方面的巨大进步以及巨大的障碍。

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