不规则地理单元存在下的Kriging和半变差反卷积。

Mathematical geology Pub Date : 2008-01-01
Pierre Goovaerts
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引用次数: 0

摘要

本文提出了一种方法,对不同大小和形状的地理单元(或块)上测量的面积数据进行地质统计变异和插值,同时考虑这些单元内的异质权值或核函数。反卷积方法是迭代的,并寻求点支持模型,使理论上正则化的半变异函数模型与拟合的面数据模型之间的差异最小化。然后在区域到点(ATP)克里格中使用该模型来绘制每个地理单元内感兴趣属性的空间分布。相干约束保证了克里格估计的加权平均值等于面基准。使用健康数据(在县一级汇总的癌症发病率)和人口密度面作为核心函数来说明这种方法。模拟是在两个地区进行的,这些地区的县地理位置截然不同:印第安纳州和美国西部的四个州。在这两个区域中,反褶积方法产生的点支持半变异函数模型与模拟点值的半变异函数相当接近。在ATP克里格中使用这个模型,可以产生比naïve点克里格的区域数据更准确的预测,后者只是将每个县折叠成其地理质心。ATP克里金降低了平滑效果,并且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,如块金效应,永远不能从实际数据中得到充分验证。用户可能希望根据他对该现象的了解来缩小解决方案的范围(例如,将块金效应设置为零)。所提出的方法避免了与解释地形图相关的视觉偏差,并应有助于分析在不同空间支持上测量的变量之间的关系。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Kriging and Semivariogram Deconvolution in the Presence of Irregular Geographical Units.

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.

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