Generating an optimal DTM from airborne laser scanning data for landslide mapping in a tropical forest environment

Khamarrul Azahari Razak (1,2), Michele Santangelo (3), Cees J. Van Westen (1), Menno W. Straatsma (1), Steven M. de Jong (4), 2013, Generating an optimal DTM from airborne laser scanning data for landslide mapping in a tropical forest environment, Geomorphology (Amst.) 190 (2013): 112–125. doi_10.1016/j.geomorph.2013.02.021,

Landslide inventory maps are fundamental for assessing landslide susceptibility, hazard, and risk. In tropical mountainous environments, mapping landslides is difficult as rapid and dense vegetation growth obscures land- slides soon after their occurrence. Airborne laser scanning (ALS) data have been used to construct the digital ter- rain model (DTM) under dense vegetation, but its reliability for landslide recognition in the tropics remains surprisingly unknown. This study evaluates the suitability of ALS for generating an optimal DTM for mapping landslides in the Cameron Highlands, Malaysia. For the bare-earth extraction, we used hierarchical robust filter- ing algorithm and a parameterization with three sequential filtering steps. After each filtering step, four interpo- lations techniques were applied, namely_ (i) the linear prediction derived from the SCOP++ (SCP), (ii) the inverse distance weighting (IDW), (iii) the natural neighbor (NEN) and (iv) the topo-to-raster (T2R). We assessed the quality of 12 DTMs in two ways_ (1) with respect to 448 field-measured terrain heights and (2) based on the interpretability of landslides. The lowest root-mean-square error (RMSE) was 0.89 m across the landscape using three filtering steps and linear prediction as interpolation method. However, we found that a less stringent DTM filtering unveiled more diagnostic micro-morphological features, but also retained some of vegetation. Hence, a combination of filtering steps is required for optimal landslide interpretation, especially in forested mountainous areas. IDW was favored as the interpolation technique because it combined computational times more reasonably without adding artifacts to the DTM than T2R and NEN, which performed relatively well in the first and second filtering steps, respectively. The laser point density and the resulting ground point density after filtering are key parameters for producing a DTM applicable to landslide identification. The results showed that the ALS-derived DTMs allowed mapping and classifying landslides beneath equatorial mountainous forests, leading to a better understanding of hazardous geomorphic problems in tropical regions.

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