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Comparing methods for partitioning a decade of carbon dioxide and water vapor fluxes in a temperate forest

机译:比较在温带森林中分配十年二氧化碳和水蒸气通量的方法

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The eddy covariance (EC) method is routinely used to measure net ecosystem fluxes of carbon dioxide (CO2) and evapotranspiration (ET) in terrestrial ecosystems. It is often desirable to partition CO2 flux into gross primary production (GPP) and ecosystem respiration (RE), and to partition ET into evaporation and transpiration. We applied multiple partitioning methods, including the recently-developed flux variance similarity (FVS) partitioning method, to a ten-year record of ET and CO2 fluxes measured using EC at Morgan Monroe State Forest, a temperate, deciduous forest located in south-central Indiana, USA. While the FVS method has previously been demonstrated in croplands and grasslands, this is the first evaluation of the method in a forest. CO2 fluxes were partitioned using nonlinear regressions, FVS, and sub-canopy EC measurements. ET was partitioned using FVS and sub-canopy EC measurements, and sub-canopy potential evapotranspiration was calculated as an additional constraint on forest floor evaporation. Leaf gas exchange measurements were used to parameterize a model of water use efficiency (WUE) necessary for the FVS method. Scaled leaf gas exchange measurements also provided additional independent estimates of GPP and transpiration. There was good agreement among partitioning methods for transpiration and GPP, which also agreed well with scaled leaf gas exchange measurements. There was higher variability among methods for RE and evaporation. The sub-canopy flux method yielded lower estimates of evaporation and RE than FVS and lower estimates of RE than the nonlinear regression method, likely due to the exclusion of flux sources within the canopy but above the top of the sub-canopy tower for the sub-canopy flux method. Based on a sensitivity test, FVS flux partitioning was moderately sensitive to errors in WUE values, and underestimates of WUE significantly reduced the rate at which the algorithm was able to produce a physically valid solution. FVS partitioning has unique potential for retroactive ET partitioning at EC sites, because it relies on the same continuous measurements as EC and does not require additional specialized equipment. FVS also has advantages for partitioning CO2 fluxes, since it does not rely on the mechanistic assumptions necessary for the commonly used nonlinear regression technique. (C) 2016 Elsevier B.V. All rights reserved.
机译:涡度协方差(EC)方法通常用于测量陆地生态系统中的净生态系统通量二氧化碳(CO2)和蒸散量(ET)。通常需要将CO2通量划分为初级生产总值(GPP)和生态系统呼吸(RE),并将ET划分为蒸发和蒸腾。我们使用了多种分区方法,包括最近开发的通量方差相似度(FVS)分区方法,对使用EC在位于中南部的温带落叶森林Morgan Monroe State Forest进行的ET和CO2通量的十年记录进行了记录。美国印第安纳州。虽然FVS方法先前已在农田和草地上得到证明,但这是在森林中对该方法的首次评估。使用非线性回归,FVS和亚冠层EC测量来划分CO2通量。使用FVS和亚冠层EC测量值对ET进行分区,并计算了亚冠层潜在蒸散量,作为对林地蒸发的附加约束。使用叶片气体交换测量参数化FVS方法所需的用水效率(WUE)模型。缩放的叶片气体交换测量结果还提供了GPP和蒸腾作用的其他独立估计。蒸腾和GPP的分配方法之间达成了很好的协议,这也与规模化的叶片气体交换测量非常吻合。 RE和蒸发方法之间的差异较大。子冠层通量方法产生的蒸发量和RE估计值比FVS更低,而RE的估计值则比非线性回归方法低,这可能是由于排除了冠层内但在子冠层顶部以下的通量源-冠层通量法。根据灵敏度测试,FVS通量分配对WUE值的误差中等敏感,而WUE的低估会大大降低该算法能够产生物理上有效的解决方案的速度。 FVS分区具有在EC站点进行追溯ET分区的独特潜力,因为它依赖于与EC相同的连续测量,并且不需要额外的专用设备。 FVS还具有划分CO2通量的优势,因为它不依赖于常用非线性回归技术所必需的机械假设。 (C)2016 Elsevier B.V.保留所有权利。

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