Mathematical Geology

, Volume 32, Issue 6, pp 683–700 | Cite as

Understanding Anisotropy Computations

  • Marian Eriksson
  • Peter P. Siska
Article

Abstract

Most descriptions of anisotropy make reference to reduced distances and conversion of anisotropic models to isotropic counterparts and equations are presented for a certain class of range-anisotropic models. Many descriptions state that sill anisotropy is modelled using a range-anisotropic structure having a very elongated ellipse. The presentations typically have few or no intervening steps. Students and applied researchers rarely follow these presentations and subsequently regard the programs that compute anisotropic variograms as black-boxes, the contents of which are too complex to try to understand. We provide the geometry necessary to clarify those computations. In so doing, we provide a general way to model any type of anisotropy (range, sill, power, slope, nugget) on an ellipse. We note cases in the literature in which the printed descriptions of anisotropy on an ellipse do not match the stated or coded models. An example is provided in which both range- and sill-anisotropic structures are fitted to the experimental variogram values from an elevation data set using the provided equations and weighted nonlinear regression. The original variogram values are plotted with the fitted surfaces to view the fit and anisotropic structure in many directions at once.

ellipse nested structures range sill slope variogram 

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Copyright information

© International Association for Mathematical Geology 2000

Authors and Affiliations

  • Marian Eriksson
    • 1
  • Peter P. Siska
    • 2
  1. 1.Department of Forest ScienceTexas A&M UniversityCollege Station
  2. 2.Department of Forest ScienceTexas A&M UniversityCollege Station

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