Finding the right pixel size

  • Authors:
  • Tomislav Hengl

  • Affiliations:
  • European Commission, Directorate General JRC, Institute for Environment and Sustainability, Soil and Waste Unit, TP 280, Via E. Fermi 1, I-21020 Ispra (VA), Italy

  • Venue:
  • Computers & Geosciences
  • Year:
  • 2006

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Abstract

This paper discusses empirical and analytical rules to select a suitable grid resolution for output maps and based on the inherent properties of the input data. The choice of grid resolution was related with the cartographic and statistical concepts: scale, computer processing power, positional accuracy, size of delineations, inspection density, spatial autocorrelation structure and complexity of terrain. These were further related with the concepts from the general statistics and information theory such as Nyquist frequency concept from signal processing and equations to estimate the probability density function. Selection of grid resolution was demonstrated using four datasets: (1) GPS positioning data-the grid resolution was related to the area of circle described by the error radius, (2) map of agricultural plots-the grid resolution was related to the size of smallest and narrowest plots, (3) point dataset from soil mapping-the grid resolution was related to the inspection density, nugget variation and range of spatial autocorrelation and (4) contour map used for production of digital elevation model-the grid resolution was related with the spacing between the contour lines i.e. complexity of terrain. It was concluded that no ideal grid resolution exists, but rather a range of suitable resolutions. One should at least try to avoid using resolutions that do not comply with the effective scale or inherent properties of the input dataset. Three standard grid resolutions for output maps were finally recommended: (a) the coarsest legible grid resolution-this is the largest resolution that we should use in order to respect the scale of work and properties of a dataset; (b) the finest legible grid resolution-this is the smallest grid resolution that represents 95% of spatial objects or topography; and (c) recommended grid resolution-a compromise between the two. Objective procedures to derive the true optimal grid resolution that maximizes the predictive capabilities or information content of a map are further discussed. This methodology can now be integrated within a GIS package to help inexperienced users select a suitable grid resolution without doing extensive data preprocessing.