Research Article
Early Identifying and Monitoring Landslides in Guizhou Province with InSAR and Optical Remote Sensing
Table 4
Identification Result of Possible Landslide Area Based on Time Series NDVI.
| Landslide number | Study area | Variation characteristics of time series NDVI | Potential landslide (yes/no) |
| #6 | Liupanshui | NDVI gradually decreased during the monitoring period | Yes | #31 | Continuous decline in the short term, and then rebound to normal value in the later period | Yes | #39 | During the monitoring period, the NDVI value continued to decrease | Yes | #19 | Guian | During the monitoring period, the NDVI value decreased significantly in the short term, and then gradually returned to the normal value level | Yes | #1 | Tongren | There is no abnormal change in the NDVI value | No | #3 | NDVI value is at a lower level compared to the same period in previous years | Yes | #4 | During the monitoring period, the NDVI value has a tendency to decrease slowly, and a sudden drop in the later period occurs | Yes | #10 | | | #11 | | | #12 | Although the NDVI value is disturbed, the overall trend is decreasing continuously | Yes | #15 | During the monitoring period, the NDVI curve showed a slow downward trend, and NDVI continued to be below 0.1 for a period of time | Yes | #16 | | | #17 | | | #19 | During the monitoring period, NDVI fell suddenly, and remained at a level close to 0 in the later period. | Yes |
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