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170 PROCESS AND FORM


              Landform elements
                                                        contour curvature. Further parameters go beyond local
              From a geomorphological viewpoint, the ground sur-  geometry, placing the element in a wider landscape
              face is composed of landform elements. Landform  setting – distance from the element to the crest, catch-
              elements are recognized as simply-curved geometric sur-  ment area per unit of contour length, dispersal area (the
              faces lacking inflections (complicated kinks) and are  land area down-slope from a short increment of contour).
              considered in relation to upslope, downslope, and lat-  Digitalelevationmodels (DEMs)have largely superseded
              eral elements. Slope is essential in defining them.  the classic work on landform elements and their descrip-
              Landscape elements go by a plethora of names – facets,  tors. Topographic elements of a landscape can be com-
              sites, land elements, terrain components, and facies. The  puted directly from a DEM and these are often classified
              ‘site’ (Linton 1951) was an elaboration of the ‘facet’  into primary (or first-order) and secondary (or second-
              (Wooldridge 1932), and involved altitude, extent, slope,  order) attributes (Moore et al. 1993). Primary attributes
              curvature, ruggedness, and relation to the water table.  are calculated directly from the digital elevation data and
              The other terms appeared in the 1960s (see Speight  the most commonly derived include slope and aspect
              1974). Landform element is perhaps the best term, as  (Table 7.1). Secondary attributes combine primary
              it seems suitably neutral.                attributes and are ‘indices that describe or characterise
                Landform elements are described by local land-  the spatial variability of specific processes occurring in the
              surface geometry. Several parameters are derivatives of  landscape’ (Moore et al. 1993, 15); examples are irradi-
              altitude – slope angle, slope profile curvature, and  ance and a wetness index (Table 7.1). Such methods allow


              Table 7.1 Primary and secondary attributes that can be computed from DEMs
              Attribute     Definition                         Applications

              Primary attributes
              Altitude      Height above mean sea level or local  Climate variables (e.g. pressure, temperature),
                              reference point                   vegetation and soil patterns, material
                                                                volumes, cut-and-fill and visibility calculations,
                                                                potential energy determination
              Slope         Rate of change of elevation – gradient  Steepness of topography, overland and
                                                                subsurface flow, resistance to uphill transport,
                                                                geomorphology, soil water content
              Aspect        Compass direction of steepest downhill  Solar insolation and irradiance,
                              slope – azimuth of slope          evapotranspiration
              Profile curvature  Rate of change of slope       Flow acceleration, erosion and deposition
                                                                patterns and rate, soil and land evaluation
                                                                indices, terrain unit classification
              Plan curvature  Rate of change of aspect        Converging and diverging flow, soil water
                                                                characteristics, terrain unit classification

              Secondary attributes

                                A s
              Wetness Index  ln =  where A s is specific catchment  Index of moisture retention
                                tanb
                              and b is slope
              Irradiance    Amount of solar energy received per unit  Soil and vegetation studies, evapotranspiration
                              area
              Source: Adapted from Huggett and Cheesman (2002, 20)
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