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Fig. 6 Thematic map of slope height.
Fig. 7 Thematic map of slope aspect.
Open image in new window Fig. 10 Map of slope rating in the study area.
Fig. 6 Thematic map of slope height (3) Slope aspect The slope aspect information can be obtained from the Majority function within the ArcGIS.
Fig. 7 Thematic map of slope aspect (4) Slope morphology It is known that water concentrates in concave topographic positions and makes the slope susceptible to (sub) surface flow as the main hydrological triggering mechanism.
Fig. 11 Parameter maps of evacuation resilience: a The parameter map of slope layer, b the parameter map of distance within flat areas layer, c the parameter map of distance to buildings layer, d the parameter map of distance to road networks layer.
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The raster maps of slope and topographic openness were constructed for Northeast Honshu, Japan, from 50-m DEMs.
Interferometric analysis of repeat pass radar images (InSAR) enables the mapping of slope movements with high accuracy, being of great relevance for the assessment of landslide risk.
This paper proposes a quantitative method to classify landforms using four morphometric parameters from DEM-derived thematic raster maps of slope and topographic openness.
Fig. 5 Thematic map of the slope angle (2) Slope height Slope height plays an important role in landslide occurrence, especially in loess areas.
The cropland suitability map is a function of slope [61] and potential cereal yield under intensive management [63] where grid cells with gentler slopes and higher potential yield are given higher suitability scores.
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