Automated classification of landform elements using object-based image analysis
L Drăguţ, T Blaschke - Geomorphology, 2006 - Elsevier
Geomorphology, 2006•Elsevier
This paper presents an automated classification system of landform elements based on
object-oriented image analysis. First, several data layers are produced from Digital Terrain
Models (DTM): elevation, profile curvature, plan curvature and slope gradient. Second,
relatively homogenous objects are delineated at several levels through image
segmentation. These object primatives are classified as landform elements using a relative
classification model, built both on the surface shape and on the altitudinal position of …
object-oriented image analysis. First, several data layers are produced from Digital Terrain
Models (DTM): elevation, profile curvature, plan curvature and slope gradient. Second,
relatively homogenous objects are delineated at several levels through image
segmentation. These object primatives are classified as landform elements using a relative
classification model, built both on the surface shape and on the altitudinal position of …
This paper presents an automated classification system of landform elements based on object-oriented image analysis. First, several data layers are produced from Digital Terrain Models (DTM): elevation, profile curvature, plan curvature and slope gradient. Second, relatively homogenous objects are delineated at several levels through image segmentation. These object primatives are classified as landform elements using a relative classification model, built both on the surface shape and on the altitudinal position of objects. So far, slope aspect was not used in classification. The classification has nine classes: peaks and toe slopes (defined by the altitudinal position or the degree of dominance), steep slopes and flat/gentle slopes (defined by slope gradients), shoulders and negative contacts (defined by profile curvatures), head slopes, side slopes and nose slopes (defined by plan curvatures). Classes are defined using flexible fuzzy membership functions. Results are visually analyzed by draping them over DTMs. Specific fuzzy classification options were used to obtain an assessment of output accuracy. Two implementations of the methodology are compared using (1) Romanian datasets and (2) Berchtesgaden National Park, Germany. The methodology has proven to be reproducible; readily adaptable for diverse landscapes and datasets; and useful in respect to providing additional information for geomorphological and landscape studies. A major advantage of this new methodology is its transferability, given that it uses only relative values and relative positions to neighboring objects. The methodology introduced in this paper can be used for almost any application where relationships between topographic features and other components of landscapes are to be assessed.
Elsevier