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Spatial evaluation of pedotransfer functions using wavelet analysis

机译:基于小波分析的pedotransfer函数的空间评估

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If predictions of pedotransfer functions (PTFs) are distributed in space, then they require a spatial evaluation. Three aspects of performance can be considered in the evaluation of a spatially distributed PTF: (i) the correlation of observed and predicted quantities across different spatial scales; (ii) the reproduction of observed variance across different spatial scales; and (iii) the spatial pattern of the model error. Further, when there is more than one PTF available, we must be able to choose which is the most appropriate for a particular spatial scale. In this study, we observed soil hydraulic properties (water retention and saturated hydraulic conductivity) at 100 regularly spaced Locations on a 5000-m transect in southern Italy. Four PTFs (referred to as Model V, Model S, Model. W, and Mode( L) were then used to predict the hydraulic properties at the sampled locations. We used wavelet analysis to examine how the variances and correlations of the observed and predicted properties varied with spatial scale and location in the landscape. This spatial analysis revealed aspects of variability that could not be investigated under assumptions of stationarity (e.g. by geostatistics). These results included: the underestimation of observed variances at particular spatial scales; the failure of the predictions to correlate adequately with the observed variables at particular spatial. scales; and, also, evidence of scale- and location-dependent correlations, which imply that non-spatial correlation coefficients do not suffice to describe the joint spatial variation of the observations and predictions. We also found significant correlations between model errors and auxiliary variables, which indicated how the site-specific predictions of the PTFs might be improved. Finally, we proposed a wavelet concordance correlation to rank the performance of each PTF, thereby enabling the choice of the best PTF at a particular spatial scale. In general. terms, we found that a locally calibrated PTF (Model L) yielded the best results. (c) 2006 Elsevier B.V. All rights reserved.
机译:如果将pedotransfer函数(PTF)的预测分布在空间中,则它们需要进行空间评估。在评估空间分布的PTF时,可以考虑性能的三个方面:(i)跨不同空间尺度的观测量和预测量的相关性; (ii)在不同空间尺度上观察到的方差的再现; (iii)模型误差的空间格局。此外,当有多个PTF可用时,我们必须能够选择最适合特定空间比例的那个。在这项研究中,我们观察了意大利南部5000米横断面上100个规则间隔位置的土壤水力特性(保水率和饱和水力传导率)。然后使用四个PTF(分别称为V型,S型,W型和L型)来预测采样位置的水力特性。我们使用小波分析来检查观测值和预测值之间的方差和相关性。性质随空间尺度和景观的位置而变化。这种空间分析揭示了在平稳性假设下无法研究的可变性方面(例如通过地统计学),这些结果包括:在特定空间尺度上低估了观测到的方差;与特定空间尺度上的观测变量充分相关的预测;以及与尺度和位置相关的相关性的证据,这意味着非空间相关系数不足以描述观测值和空间的联合空间变化我们还发现了模型误差与辅助变量之间的显着相关性,这表明了现场规范如何PTF的ic预测可能会得到改善。最后,我们提出了一种小波一致性相关性来对每个PTF的性能进行排名,从而能够在特定的空间尺度上选择最佳PTF。一般来说。而言,我们发现本地校准的PTF(L型)产生了最佳结果。 (c)2006 Elsevier B.V.保留所有权利。

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