Landslides are the most common geological disasters that result from large seismic activities and heavy rainfall in mountainous areas. They are destructive events that occur suddenly and have a wide distribution range. Landslide extraction is the primary factor in collecting destruction information and plays a key role in disaster prevention and emergency rescue. This paper presents a method that combines texture analysis and emissivity estimation to extract landslides from different backgrounds. Many researchers have focused on landslide extraction and recognition
and they proposed methods based on the ability of the Normalized Difference Vegetation Index (NDVI) to separate vegetation. However
although NDVI easily extracts landslides from high vegetation areas
it is affected by soil interference in sparse vegetation areas. Thus
extracting landslides is difficult. An NDVI-based method is proposed for landslide extraction in a complicated environment and to make NDVI effective in sparse vegetation zones.In accordance with the research area and remote sensing data
this method consists of four steps on the assumption that image preprocessing has been completed. First
the NDVI image is calculated by using near-infrared and red bands; this approach shows that some local regions have a sharp contrast
whereas others have a weak contrast. Second
texture analysis is conducted to divide the research area into several blocks according to this contrast distribution. NDVI mean and near-infrared Angular Second Moment (ASM) based on Gray-Level Co-occurrence Matrix (GLCM) could be selected as the texture feature to segment zones easily by providing simple thresholds. A continual large vegetation area is outstanding in the Mean feature
and a mountainous landslide area is rough in the ASM feature. The remaining area
except the first two
varies in the ASM feature related to soil components. Thus
the combination of Mean and ASM features facilitates texture analysis. Third
emissivity is estimated in different blocks based on the NDVI image. In this section
the NDVIs of pure soil and pure vegetation from statistics of the NDVI image in different blocks are critical parameters in calculating the Percentage of Vegetation (PV)
thereby obtaining the emissivity. In a limited area
emissivity contrasts within different objects
especially for soil and vegetation
thereby making it more suitable than NDVI for landslide extraction. Finally
the landslides are extracted through emissivity threshold segmentation technology with an appropriate threshold manually.Landsat 5 TM and Terra ASTER data are tested by this method
and the result is favorable given that it is more consistent with that of artificial landslide extraction than that of the other methods
such as maximum likelihood supervised classification
neural net supervised classification
support vector machine-based supervised classification
and NDVI global threshold segmentation. For objective and quantitative evaluation
the result of artificial extraction is considered as the ground-truth data to calculate the confusion matrix of other results
with the Kappa coefficient being used to demonstrate the performance of each method. As a result
the method described in this article achieves a high Kappa coefficient
namely
0.8531 (TM) and 0.9271 (ASTER). By contrast
maximum likelihood classification achieves 0.7634 (TM)
neural net classification achieves 0.66 (TM)
SVM-based classification achieves 0.6896 (TM)
NDVI global threshold (0.3) segmentation achieves 0.622 (TM)
and NDVI global threshold (0.5) segmentation achieves 0.7487% (TM). Evidently
this method can effectively eliminate omission and misclassification. With the increase in the resolution of remote sensing data
ASTER (15 m) provides a better result compared with TM (30 m)
thereby showing that this method does not rely on data sources
and a high resolution contributes to a good result.Comparative analysis between different methods and data sources indicates the following results: The NDVI mean and near-infrared ASM are good texture features for separating different background environment blocks
especially with soil as the leading factor. Emissivity reflects the spatial difference in objects
although it is estimated by NDVI. The estimated emissivity not only separates vegetation from NDVI but also increases the difference between soils
thereby resulting in good landslide extraction. The advantages of texture analysis and emissivity estimation enhance landslide extraction in complicated research areas. Finally
the threshold selection problem in NDVI global threshold segmentation method is solved
and the sample selection and learning process in supervised classification are avoided. This method is designed for a medium resolution that ranges between 10 m to 50 m; thus
this method can be used with other data sources with a similar resolution
such as Landsat 5 TM and Terra ASTER. We proposed an effective method for landslide extraction for medium resolution. To handle high-resolution remote sensing data
this method will be combined with object-oriented methods in follow-up studies for accurate landslide extraction. The proposed method has a strong dependency on manual threshold selection; this dependency is inconvenient in the auto-extraction process. Therefore
self-adaptive threshold extraction is another challenge in future work.