Abstract
The importance in hydrology of generating two-dimensional surfaces from data measured at points cannot be overstated. Transformation from point to raster data structures is often accomplished through interpolation of point data to form a two-dimensional surface. The difficulty with some interpolation methods is that the surface is organized around the point locations. The inverse distance weighting interpolation assigns a grid value based on the surrounding point values and distance away. If interpolated with the IDW method, it can appear that rain preferentially falls around the gauge, rather than having a more natural distribution geographically. It is important to understand how these surfaces are generated and the influence of the resulting surface on hydrologic modeling. The subject of this chapter is the methods and pitfalls of interpolation.
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Vieux, B.E. (2016). Surface Generation. In: Distributed Hydrologic Modeling Using GIS. Water Science and Technology Library, vol 74. Springer, Dordrecht. https://doi.org/10.1007/978-94-024-0930-7_3
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DOI: https://doi.org/10.1007/978-94-024-0930-7_3
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