Abstract

Unfavorable land cover leads to excessive damage from landslides and other natural hazards, whereas the presence of vegetation is expected to mitigate rainfall-induced landslide potential. Hence, unexpected and rapid changes in land cover due to deforestation would be detrimental in landslide-prone areas. Also, vegetation cover is subject to phenological variations and therefore, timely classification of land cover is an essential step in effective evaluation of landslide hazard potential. The work presented here investigates methods that can be used for land cover classification based on the Normalized Difference Vegetation Index (NDVI), derived from up-to-date satellite images, and the feasibility of application in landslide risk prediction. A major benefit of this method would be the eventual ability to employ NDVI as a stand-alone parameter for accurate assessment of the impact of land cover in landslide hazard evaluation. An added benefit would be the timely detection of undesirable practices such as deforestation using satellite imagery. A landslide-prone region in Oregon, USA is used as a model for the application of the classification method. Five selected classification techniques—k-nearest neighbor, Gaussian support vector machine (GSVM), artificial neural network, decision tree and quadratic discriminant analysis support the viability of the NDVI-based land cover classification. Finally, its application in landslide risk evaluation is demonstrated.

Highlights

  • Thick vegetation cover improves the shear strength of soil by increasing cohesion and suction through evapotranspiration [1]

  • Since R radiation is absorbed while NIR radiation is reflected by green vegetation, the Normalized Difference Vegetation Index (NDVI) increases with the increase of vegetation density

  • Risks due to natural disasters faced by humankind such as landslides can be escalated by unfavorable variations in land cover conditions and unplanned construction

Read more

Summary

Introduction

Thick vegetation cover improves the shear strength of soil by increasing cohesion and suction through evapotranspiration [1]. The presence of vegetation indicates conditions that are unfavorable for landsliding. The lack of vegetation cover would create favorable conditions for erosion and slope failure. The destruction of vegetation cover due to deforestation, construction and urbanization invariably enhances the potential for erosion and landsliding [2]. There are two types of factors that can affect the potential for landslide occurrence at a given location: (1) factors that can be attributed to that location and (2) factors that trigger mass soil movement [3]. If the conditions of the above attributes are favorable for landsliding, such as low vegetation cover, landslides can be triggered by rainfall, earthquakes, Geosciences 2016, 6, 45; doi:10.3390/geosciences6040045 www.mdpi.com/journal/geosciences

Objectives
Methods
Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call