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Estimating regional-scale methane flux and budgets using CARVE aircraft measurements over Alaska

机译:使用CARVE飞机在阿拉斯加的测量来估算区域规模的甲烷通量和预算

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摘要

Methane (CH) is the second most important greenhouse gas but itsemissions from northern regions are still poorly constrained. In this study,we analyze a subset of in situ CH aircraft observations made overAlaska during the growing seasons of 2012–2014 as part of the Carbon inArctic Reservoirs Vulnerability Experiment (CARVE). Net surface CHfluxes are estimated using a Lagrangian particle dispersion model whichquantitatively links surface emissions from Alaska and the western Yukon withobservations of enhanced CH in the mixed layer. We estimate thatbetween May and September, net CH emissions from the region ofinterest were 2.2 ± 0.5 Tg, 1.9 ± 0.4 Tg, and2.3 ± 0.6 Tg of CH for 2012, 2013, and 2014, respectively. If emissionsare only attributed to two biogenic eco-regions within our domain, thentundra regions were the predominant source, accounting for over half of theoverall budget despite only representing 18 % of the total surface area.Boreal regions, which cover a large part of the study region, accounted forthe remainder of the emissions. Simple multiple linear regression analysisrevealed that, overall, CH fluxes were largely driven by soiltemperature and elevation. In regions specifically dominated by wetlands,soil temperature and moisture at 10 cm depth were important explanatoryvariables while in regions that were not wetlands, soil temperature andmoisture at 40 cm depth were more important, suggesting deepermethanogenesis in drier soils. Although similar environmental drivers havebeen found in the past to control CH emissions at local scales, thisstudy shows that they can be used to generate a statistical model to estimatethe regional-scale net CH budget.
机译:甲烷(CH)是第二重要的温室气体,但其来自北部地区的排放仍然受到限制。在这项研究中,我们分析了2012-2014年生长季节在阿拉斯加各地进行的原位CH飞机观测的子集,这是“碳在北极储层脆弱性实验(CARVE)”的一部分。使用拉格朗日粒子弥散模型估算净表面CHflux,该模型将阿拉斯加和育空地区西部的表面排放定量地与混合层中CH的增加联系起来。我们估计,在5月和9月之间,感兴趣区域CH的净排放量分别为2012年,2013年和2014年的CH的2.2±0.5 Tg,1.9±0.4 Tg和2.3±0.6 Tg。如果排放仅归因于我们域内的两个生物生态区域,则苔原地区是主要来源,尽管仅占总表面积的18%,但占总预算的一半以上。北方地区,占研究的大部分占排放的其余部分。简单的多元线性回归分析表明,总体而言,CH通量主要由土壤温度和海拔高度驱动。在以湿地为主的地区,土壤温度和10 cm深度处的水分是重要的解释变量,而在非湿地地区,40 temperaturecm深度处的土壤温度和湿度则更为重要,这表明在较干燥的土壤中甲烷形成较深。尽管过去已经发现类似的环境驱动因素可以控制地方规模的CH排放,但是这项研究表明,可以将它们用于生成统计模型来估算区域规模的CH净预算。

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