r.param.scale.html 3.5 KB

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  1. <h2>DESCRIPTION</h2>
  2. <em>r.param.scale</em> extracts terrain parameters from a digital elevation model. Uses a
  3. multi-scale approach by fitting a bivariate quadratic polynomial to a given
  4. window size using least squares.
  5. <p>The module calculates the following parameters (terminology is from Wood,
  6. 1996 with related terminology used in other GRASS modules listed in
  7. brackets):
  8. <ul>
  9. <li>
  10. <i>elev</i>: Generalised elevation value (for resampling purposes at different
  11. scale)</li>
  12. <li>
  13. <i>slope</i>: Magnitude of maximum gradient (steepest slope angle)</li>
  14. <li>
  15. <i>aspect</i>: Direction of maximum gradient (steepest slope direction=flow direction)</li>
  16. <li>
  17. <i>profc</i>: profile curvature (curvature intersecting with the plane
  18. defined by <i>Z</i> axis and maximum gradient direction). Positive values
  19. describe convex profile curvature, negative values concave profile
  20. curvature.</li>
  21. <li>
  22. <i>planc</i>: plan curvature (horizontal curvature, intersecting with
  23. the <i>XY</i> plane)</li>
  24. <li>
  25. <i>longc</i>: longitudinal curvature (profile curvature intersecting
  26. with the plane defined by the surface normal and maximum gradient direction)</li>
  27. <li>
  28. <i>crosc</i>: cross-sectional curvature (tangential curvature intersecting
  29. with the plane defined by the surface normal and a tangent to the contour
  30. - perpendicular to maximum gradient direction)</li>
  31. <li>
  32. <i>maxic</i>: maximum curvature (can be in any direction)</li>
  33. <li>
  34. <i>minic</i>: minimum curvature (in direction perpendicular to the direction
  35. of of maximum curvature)</li>
  36. <!--
  37. <li>
  38. <i>meanc</i> or mean curvature (average of maximum and minimum curvatures).</li>
  39. -->
  40. <li>
  41. <i>feature</i>: Morphometric features: peaks, ridges, passes, channels, pits and planes</li>
  42. </ul>
  43. <h2>NOTES</h2>
  44. In <i>r.param.scale</i> the direction of maximum gradient (considered
  45. downslope) is stored as (West is 0 degree, East is +/- 180 degree):
  46. <ul>
  47. <li>
  48. 0..+180 degree from West to North to East</li>
  49. <li>
  50. 0..-180 degree from West to South to East</li>
  51. </ul>
  52. Note that the aspect map is calculated differently from
  53. <em><a href="r.slope.aspect.html">r.slope.aspect</a></em>.
  54. <h2>EXAMPLE</h2>
  55. The next commands will create a geomorphological map of the Spearfish region:
  56. <div class="code"><pre>
  57. g.region raster=elevation.10m -p
  58. r.param.scale in=elevation.10m output=morphology param=feature size=9
  59. </pre></div>
  60. <p><center>
  61. <img src="r_param_scale_morph.jpg" alt="r.param.scale generated geomorphological map"><br>
  62. <i>Geomorphological map of a subregion in the Spearfish (SD) area</i>
  63. </center>
  64. <h2>TODO</h2>
  65. Fix bug when `constrain through central cell' option selected. Create color
  66. tables for all output files (presently only on features).
  67. <h2>REFERENCES</h2>
  68. <ul>
  69. <li>Wood, J. (1996): The Geomorphological characterisation of
  70. Digital Elevation Models. Diss., Department of Geography, University
  71. of Leicester, U.K<br>online at:
  72. <a href="http://hdl.handle.net/2381/34503">http://hdl.handle.net/2381/34503</a></li>
  73. <li>Java Code in
  74. <a href="http://www.geog.le.ac.uk/jwo/research/LandSerf">LandSerf</a>
  75. that implements the same procedure</li>
  76. </ul>
  77. <h2>SEE ALSO</h2>
  78. <!-- not ported to GRASS 6 due to non-GPLness of numerical recipes.
  79. <i><a href="d.param.scale.html">d.param.scale</a></i>
  80. -->
  81. <em>
  82. <a href="r.slope.aspect.html">r.slope.aspect</a>
  83. </em>
  84. <h2>AUTHORS</h2>
  85. <address>
  86. <a href="MAILTO:jwo@le.ac.uk">jwo@le.ac.uk</a>
  87. - <a href="http://www.geog.le.ac.uk/assist/index.html">ASSIST's home</a></address>
  88. <p>Update to FP 3/2002: L. Potrich, M. Neteler, S. Menegon (ITC-irst)
  89. <p>
  90. <i>Last changed: $Date$</i>