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Spatio-temporal data fusion for fine-resolution subsidence estimation

机译:用于微分辨率沉降估计的时空数据融合

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摘要

Land subsidence provides important information about the spatial and temporal changes occurring in the sub-surface (e.g. groundwater levels, geology, etc.). However, sufficient subsidence data are difficult to obtain using only one sensor or survey, often resulting in a tradeoff between spatial resolution and temporal coverage. This study aims to estimate the high spatio-temporal resolution land subsidence by using a kernel-based vector data fusion approach between annual leveling and monthly subsidence monitoring well data, while invoking an invariant relation of subsidence information. Subsidence patterns and processes can be identified when spatiotemporal fusion of sensor data are implemented. In this subsidence investigation in Yunlin and Chunghua counties, Taiwan, the root mean square error (RMSE) is 0.52 cm in the fusion stage, and the mapping RMSE is 0.53 cm in the interpolation. The fused subsidence data readily show that the subsidence hotspot varies with time and space. The subsidence hotspots are in the western region during the winter (related to aquaculture activities) but move to the inland areas of Yunlin County during the following spring (related to agricultural activities). The proposed approach can help explain the spatio-temporal variability of the subsidence pattern.
机译:土地沉降提供关于在子表面(例如地下水位,地质等)中发生的空间和时间变化的重要信息。然而,仅使用一个传感器或调查难以获得足够的沉降数据,通常导致空间分辨率与时间覆盖之间的权衡。本研究旨在通过使用年平衡和月沉降监测井数据之间的基于内核的向量数据融合方法来估算高时空分辨率的土地沉降,同时调用沉降信息不变关系。当实现传感器数据的时空熔化时,可以识别沉降模式和过程。在云林和春化县县沉降调查中,融合阶段的根均方误差(RMSE)是0.52厘米,内插的映射RMSE为0.53厘米。融合沉降数据很容易显示沉降热点随时间和空间而变化。沉降热点在冬季(与水产养殖活动有关),而是在以下春季(与农业活动有关)期间迁至云林县的内陆地区。所提出的方法可以帮助解释沉降模式的时空变异性。

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