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Mapping carbon sequestration in forests at the regional scale - a climate biomonitoring approach by example of Germany

机译:绘制区域森林中的碳固存图-以德国为例的气候生物监测方法

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Background The United Nations Framework Convention on Climate Change recognizes carbon (C) fixation in forests as an important contribution for the reduction of atmospheric pollution in terms of greenhouse gases. Spatial differentiation of C sequestration in forests either at the national or at the regional scale is therefore needed for forest planning purposes. Hence, within the framework of the Forest Focus regulation, the aim of this investigation was to statistically analyse factors influencing the C fixation and to use the corresponding associations in terms of a predictive mapping approach at the regional scale by example of the German federal state North Rhine-Westphalia. The results of the methodical scheme outlined in this article should be compared with an already-published approach applied to the same data which were used in the investigation at hand. Methods Site-specific data on C sequestration in humus, forest trees/dead wood and soil from two forest monitoring networks were intersected with available surface information on topography, soil, climate and forestal growing areas and districts. Next, the association between the C sequestration and the influence factors were examined and modelled by linear regression analyses. The resulting regression equations were applied on the surface data to predicatively map the C sequestration for the entire study area. Results The computations yielded an estimation of 146.7 mio t C sequestered in the forests of North Rhine-Westphalia corresponding to 168.6 t/ha. The calculated values correspond well to according specifications given by the literature. Furthermore, the results are almost identical to those of another pilot study where a different statistical methodology was applied on the same database. Nevertheless, the underlying regression models contribute only a low degree of explanation to the overall variance of the C fixation. This might mainly be due to data quality aspects and missing influence factors in the analyses. Discussion In another study, an alternative approach was introduced to map the spatial differentiation of C sequestration in North Rhine-Westphalia based on the combination of geostatistics, decision tree analyses and GIS techniques. As a result, the overall mean of C sequestration amounted for 177 t C/ha which is 8.4 t C/ha higher than what was calculated in the study at hand and 14 t C/ha below the roughly guessed German-wide mean of 191 t C/ha. Conclusions The surface estimations of C pools in living forest trees/dead wood, the humus layer and the mineral soil enable to map the fixation of the greenhouse gas CO2 in forests at the regional scale. The estimations that were derived in this study are in good accordance with estimations based on techniques which, in contrast, did neither allow for spatial differentiation nor for mapping. The presented approach should be validated by application of other statistical techniques and by use of German wide inventory data. Furthermore, C sequestration should be modelled according to different climate change scenarios by combining statistical methods and dynamic modelling.
机译:背景技术《联合国气候变化框架公约》认为,固定森林中的碳(C)是减少温室气体对大气污染的重要贡献。因此,出于森林规划目的,需要在国家或地区范围内对森林中的固碳进行空间区分。因此,在“森林焦点”法规的框架内,本研究的目的是对影响固色的因素进行统计分析,并在区域范围内以预测性作图方法(例如德国联邦州北部)使用相应的关联。莱茵-威斯特法伦州。应该将本文概述的方法性方案的结果与已经发布的应用于手边调查的相同数据的方法进行比较。方法将来自两个森林监测网络的腐殖质,林木/死木和土壤中固碳的特定地点数据与地形,土壤,气候以及森林生长地区和地区的可用表面信息相交。接下来,通过线性回归分析检查并建立了C固存与影响因素之间的关联。将所得的回归方程式应用于表面数据,以预测整个研究区域的碳固存。结果计算得出在北莱茵-威斯特法伦州森林中固存的146.7 t C碳的估计值相当于168.6吨/公顷。计算值非常符合文献中给出的规格。此外,结果几乎与另一项试验研究的结果相同,在另一项试验研究中,对同一数据库使用了不同的统计方法。然而,基础回归模型仅对C固定的总体方差做出了很小的解释。这可能主要是由于数据质量方面以及分析中缺少影响因素。讨论在另一项研究中,基于地质统计学,决策树分析和GIS技术的结合,引入了另一种方法来绘制北莱茵-威斯特法伦州碳固存的空间差异图。结果,固碳的总平均值为177 t C / ha,比当前的研究结果高8.4 t C / ha,比德国大概的平均水平191低了14 t C / ha。吨碳/公顷。结论活林树木/枯木,腐殖质层和矿质土壤中碳库的表面估算值可以绘制区域尺度上森林中温室气体CO2的固定情况。在这项研究中得出的估计值与基于技术的估计值非常吻合,而这些技术既不允许空间区分,也不允许映射。所提出的方法应通过使用其他统计技术并使用德国广泛的库存数据进行验证。此外,应通过结合统计方法和动态建模,根据不同的气候变化情景对固碳进行建模。

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