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首页> 外文期刊>Global change biology >Environmental controls on CH emission from polygonal tundra on the microsite scale in the Lena river delta, Siberia
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Environmental controls on CH emission from polygonal tundra on the microsite scale in the Lena river delta, Siberia

机译:西伯利亚利纳河三角洲微尺度上多边形苔原CH排放的环境控制

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The carbon budgets of the atmosphere and terrestrial ecosystems are closely coupled by vertical gas exchange fluxes. Uncertainties remain with respect to high latitude ecosystems and the processes driving their temporally and spatially highly variable methane (CH) exchange. Problems associated with scaling plot measurements to larger areas in heterogeneous environments are addressed based on intensive field studies on two nested spatial scales in Northern Siberia. CH fluxes on the microsite scale (0.1-100 mpo) were measured in the Lena River Delta from July through September 2006 by closed chambers and were compared with simultaneous ecosystem scale (10t-10e mpo) flux measurements by the eddy covariance (EC) method. Closed chamber measurements were conducted almost daily on 15 plots in four differently developed polygon centers and on a polygon rim. Controls on CH emission were identified by stepwise multiple regression. In contrast to relatively low ecosystem-scale fluxes controlled mainly by near-surface turbulence, fluxes on the microsite scale were almost an order of magnitude higher at the wet polygon centers and near zero at the drier polygon rim and high-center polygon. Microsite scale CH fluxes varied strongly even within the same microsites. The only statistically significant control on chamber-based fluxes was surface temperature calculated using the Stefan-Boltzmann equation in the wet polygon centers, whereas no significant control was found for the low emissions from the dry sites. The comparison with the EC measurements reveals differences in controls and the seasonal dynamics between the two measurement scales, which may have consequences for scaling and process-based models. Despite those differences, closed chamber measurements from within the EC footprint could be scaled by an area-weighting approach of landcover classes based on high-resolution imagery to match the total ecosystem-scale emission. Our nested sampling design allowed for checking scaling results against measurements and to identify potentially missed sources or sinks.
机译:垂直气体交换通量使大气层和陆地生态系统的碳预算紧密耦合。高纬度生态系统及其驱动其在时间和空间上高度可变的甲烷(CH)交换的过程仍存在不确定性。基于在西伯利亚北部两个嵌套空间尺度上的密集实地研究,解决了与在不同环境中将图尺度测量扩展到更大区域相关的问题。在2006年7月至2006年9月期间,通过封闭的小室在利纳河三角洲测量了微场所规模的CH通量(0.1-100 mpo),并通过涡度协方差(EC)方法将其与同时的生态系统规模(10t-10e mpo)通量进行了比较。 。封闭室测量几乎每天在四个不同展开的多边形中心和多边形边缘上的15个地块上进行。通过逐步多元回归确定CH排放的对照。与主要由近地表湍流控制的相对较低的生态系统尺度通量相反,在微场地尺度上的通量在湿多边形中心几乎高一个数量级,而在干燥多边形边缘和高中心多边形上几乎接近零。即使在相同的微场所内,微场所规模的CH通量也变化很大。对基于室的通量的唯一统计上显着的控制是在湿多边形中心使用Stefan-Boltzmann方程计算的表面温度,而对于干燥位置的低排放量则没有发现显着控制。与EC测量值的比较揭示了两个测量尺度之间在控件和季节动态方面的差异,这可能会对缩放和基于过程的模型产生影响。尽管存在这些差异,但可以通过基于高分辨率图像的土地覆盖类别的面积加权方法来缩放EC足迹内的密闭室测量值,以匹配生态系统总排放量。我们的嵌套采样设计允许根据测量结果检查缩放结果,并识别可能遗漏的源或汇。

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