1965
DOI: 10.2307/621689
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Trend-Surface Mapping in Geographical Research

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Cited by 129 publications
(30 citation statements)
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“…The interpolation method is a widely used approach for generating raster data from the dispersed data of meteorological observation stations; it is simple and convenient, but it is unable to analyze the spatial variations in scattered data. TSA (Chorley & Haggett 1968, Gittins 1968) is a statistical method that is fully able to describe the variation in the spatial (or spatial-temporal) distribution of certain factors. It uses spatial coordinates as independent variables: abscissa and ordinate in a 2-dimensional TSA or longitude, latitude and elevation in a 3-dimensional TSA.…”
Section: Methodsmentioning
confidence: 99%
“…The interpolation method is a widely used approach for generating raster data from the dispersed data of meteorological observation stations; it is simple and convenient, but it is unable to analyze the spatial variations in scattered data. TSA (Chorley & Haggett 1968, Gittins 1968) is a statistical method that is fully able to describe the variation in the spatial (or spatial-temporal) distribution of certain factors. It uses spatial coordinates as independent variables: abscissa and ordinate in a 2-dimensional TSA or longitude, latitude and elevation in a 3-dimensional TSA.…”
Section: Methodsmentioning
confidence: 99%
“…The generalization in pattern description which the isopleth maps render may be further advanced by utilizing established trend-surface mapping programmes (Chorley & Haggett 1965). Trend-surface mapping refers to the fitting of mathematical polynomials to point reference data, and has mainly been developed in geological studies to facilitate interpretation of structural trends in rock deposits (Whitten 1963).…”
Section: Computer Graphic Techniquesmentioning
confidence: 99%
“…Third, the topographic surface has appeared too complex for wide application of global polynomial approximations. As a result, only low-order orthogonal polynomials have been utilized in trend-surface analysis, a technique to reveal trend and residual components of the topographic surface [24,25]. However, the current progress in the theory and practice of polynomial approximation [26][27][28] suggests that it is now possible to solve such problems.…”
Section: Introductionmentioning
confidence: 99%