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首页> 外文期刊>Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System >Dissolved methane and carbon dioxide fluxes in Subarctic and Arctic regions: Assessing measurement techniques and spatial gradients
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Dissolved methane and carbon dioxide fluxes in Subarctic and Arctic regions: Assessing measurement techniques and spatial gradients

机译:北极和北极地区溶解的甲烷和二氧化碳通量:评估测量技术和空间梯度

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Here we use a portable method to obtain high spatial resolution measurements of concentrations and calculate diffusive water-to-air fluxes of CH4 and CO2 from two Subarctic coastal regions (Kasitsna and Jakolof Bays) and an Arctic lake (Toolik Lake). The goals of this study are to determine distributions of these concentrations and fluxes to (1) critically evaluate the established protocols of collecting discrete water samples for these determinations, and to (2) provide a first-order extrapolation of the regional impacts of these diffusive atmospheric fluxes. Our measurements show that these environments are highly heterogeneous. Areas with the highest dissolved CH4 and CO2 concentrations were isolated, covering less than 21% of the total lake and bay areas, and significant errors can be introduced if the collection of discrete water samples does not adequately characterize these spatial distributions. A first order extrapolation of diffusive fluxes to all Arctic regions with similar characteristics as Toolik Lake suggests that these lakes are likely supplying 0.21 and 15.77 Tg of CH4 and CO2 to the atmosphere annually, respectively. Similarly, we found that the Subarctic Coastal Ocean is likely supplying 0.027 Tg of CH4 annually and is taking up roughly 524 Tg of CO2 per year. Although diffusive fluxes at Toolik Lake may not be as substantial when comparing against present seep ebullition and spring ice-out values, warming in the Arctic may result in the increase of methane discharge and methane emissions to the atmosphere. Thus further work is needed to understand this changing environment. This study suggests that high spatial resolution measurement protocols, similar to the one used here, should be incorporated into field campaigns to reduce regional uncertainty and refine global emission estimates. (C) 2015 Elsevier B.V. All rights reserved.
机译:在这里,我们使用一种便携式方法来获得浓度的高空间分辨率测量值,并计算出两个亚北极沿海地区(Kasitsna和Jakolof海湾)和一个北极湖(Toolik Lake)的CH4和CO2的水-空气扩散通量。这项研究的目的是确定这些浓度和通量的分布,以(1)严格评估用于这些测定的收集离散水样的既定方案,并(2)提供这些扩散的区域影响的一阶外推法。大气通量。我们的测量表明,这些环境是高度异构的。分离出溶解的CH4和CO2浓度最高的区域,覆盖不到湖泊和海湾总面积的21%,如果离散水样的收集不能充分体现这些空间分布的特征,则可能会引入重大误差。对所有与北极地区具有相似特征的北极地区的扩散通量进行一阶外推表明,这些湖泊可能每年分别向大气供应0.21和15.77 Tg的CH4和CO2。同样,我们发现北极近海每年可能供应0.027 Tg的CH4,每年大约吸收524 Tg的CO2。尽管与目前的渗水和春季冰冻值相比,Toolik湖的扩散通量可能不大,但北极的变暖可能导致甲烷向大气的排放和甲烷排放的增加。因此,需要进一步的工作来理解这种不断变化的环境。这项研究表明,应将类似于此处使用的高空间分辨率测量协议纳入野外活动,以减少区域不确定性并完善全球排放估算。 (C)2015 Elsevier B.V.保留所有权利。

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