利用空间插值技术重建潜在侵蚀地形——一种实证方法（英文）

编号 zgly0001584685

文献类型 期刊论文

文献题名 利用空间插值技术重建潜在侵蚀地形——一种实证方法（英文）

作者 RafaelloBergonse  EusebioReis 

作者单位 CenterforGeographicalStudies  UniversityofLisbon 

母体文献 Journal of Geographical Sciences 

年卷期 2015年02期

年份 2015 

分类号 P931.1 

关键词 pre-erosiontopography  surfacereconstruction  spatialinterpolation  splineinterpolation  triangulatedirregularnetworks  erosivelandforms  gullyerosion 

文摘内容 Understanding the topographic context preceding the development of erosive landforms is of major relevance in geomorphic research,as topography is an important factor on both water and mass movement-related erosion,and knowledge of the original surface is a condition for quantifying the volume of eroded material.Although any reconstruction implies assuming that the resulting surface reflects the original topography,past works have been dominated by linear interpolation methods,incapable of generating curved surfaces in areas with no data or values outside the range of variation of inputs.In spite of these limitations,impossibility of validation has led to the assumption of surface representativity never being challenged.In this paper,a validation-based method is applied in order to define the optimal interpolation technique for reconstructing pre-erosion topography in a given study area.In spite of the absence of the original surface,different techniques can be nonetheless evaluated by quantifying their capacity to reproduce known topography in unincised locations within the same geomorphic contexts of existing erosive landforms.A linear method(Triangulated Irregular Network,TIN) and 23 parameterizations of three distinct Spline interpolation techniques were compared using 50 test areas in a context of research on large gully dynamics in the South of Portugal.Results show that almost all Spline methods produced smaller errors than the TIN,and that the latter produced a mean absolute error 61.4% higher than the best Spline method,clearly establishing both the better adjustment of Splines to the geomorphic context considered and the limitations of linear approaches.The proposed method can easily be applied to different interpolation techniques and topographic contexts,enabling better calculations of eroded volumes and denudation rates as well as the investigation of controls by antecedent topographic form over erosive processes.