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Kriging and Semivariogram Deconvolution in the Presence of Irregular Geographical Units

机译:存在不规则地理单位的Kriging和半变异函数反卷积

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摘要

This paper presents a methodology to conduct geostatistical variography and interpolation on areal data measured over geographical units (or blocks) with different sizes and shapes, while accounting for heterogeneous weight or kernel functions within those units. The deconvolution method is iterative and seeks the pointsupport model that minimizes the difference between the theoretically regularized semivariogram model and the model fitted to areal data. This model is then used in area-to-point (ATP) kriging to map the spatial distribution of the attribute of interest within each geographical unit. The coherence constraint ensures that the weighted average of kriged estimates equals the areal datum.This approach is illustrated using health data (cancer rates aggregated at the county level) and population density surface as a kernel function. Simulations are conducted over two regions with contrasting county geographies: the state of Indiana and four states in the Western United States. In both regions, the deconvolution approach yields a point support semivariogram model that is reasonably close to the semivariogram of simulated point values. The use of this model in ATP kriging yields a more accurate prediction than a naïve point kriging of areal data that simply collapses each county into its geographic centroid. ATP kriging reduces the smoothing effect and is robust with respect to small differences in the point support semivariogram model. Important features of the point-support semivariogram, such as the nugget effect, can never be fully validated from areal data. The user may want to narrow down the set of solutions based on his knowledge of the phenomenon (e.g., set the nugget effect to zero). The approach presented avoids the visual bias associated with the interpretation of choropleth maps and should facilitate the analysis of relationships between variables measured over different spatial supports.
机译:本文提出了一种方法,可以对在具有不同大小和形状的地理单位(或块)上测量的面数据进行地统计变异和插值,同时考虑这些单位内的异质权重或核函数。反卷积方法是迭代的,它寻求的点支持模型使理论上正则化的半变异函数模型与拟合到面数据的模型之间的差异最小。然后将此模型用于点对点(ATP)克里金法,以绘制每个地理单位内关注属性的空间分布。一致性约束确保克里金估计的加权平均值等于面积数据。此方法通过使用健康数据(县级癌症比率汇总)和人口密度表面作为核函数来说明。模拟是在两个县域不同的地区进行的:印第安纳州和美国西部的四个州。在这两个区域中,反卷积方法都会产生一个点支持半变异函数模型,该模型可以合理地接近模拟点值的半变异函数。与简单地将区域县折叠成其地理中心的区域数据的朴素点克里金法相比,在ATP克里金法中使用此模型可产生更准确的预测。 ATP克里金法降低了平滑效果,并且相对于点支持半变异函数模型中的小差异具有鲁棒性。点支持半变异函数的重要特征(例如金块效应)永远无法从面数据中得到充分验证。用户可能希望基于他对现象的了解来缩小解决方案的范围(例如,将金块效应设置为零)。提出的方法避免了与解释脉络线图有关的视觉偏见,并应有助于分析在不同空间支持下测得的变量之间的关系。

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