2019
DOI: 10.5194/isprs-archives-xlii-3-w8-133-2019
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Landslide Investigation Using Differential Synthetic Aperture Radar Interferometry: A Case Study of Balloran Dam Area in Syria

Abstract: <p><strong>Abstract.</strong> Landslides are one of the main geological hazards that can cause critical damage to the infrastructure in an area and can result in serious risks to the people’s safety there. Landslides can be investigated and monitored using field survey, aerial mapping and high resolution optical satellite data analysis. However, these methods are relatively time-consuming. Interferometric synthetic aperture radar (InSAR) can investigate and monitor landslides and provide sub-… Show more

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Cited by 5 publications
(8 citation statements)
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“…Road networks in the study area are susceptible to be damaged annually due to unforeseen landslides after intense rainfall events. These unforeseen landslides threaten the lives and the properties of people who live there (Hammad et al, 2019).…”
Section: Aim and Objectivesmentioning
confidence: 99%
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“…Road networks in the study area are susceptible to be damaged annually due to unforeseen landslides after intense rainfall events. These unforeseen landslides threaten the lives and the properties of people who live there (Hammad et al, 2019).…”
Section: Aim and Objectivesmentioning
confidence: 99%
“…Landslide hazard investigation, assessment, monitoring and mapping processes become increasingly important in most mountainous and hilly regions around the world where landslides are a major hazard (kervyn et al, 2015) and (Hammad et al, 2019). So, landslide studies in those places are important to evaluate the relative contributions of all elements and factors involved in landslide process within an area and to identify the possible locations that might be affected by landslides in order to reduce risk on people in those areas and help local authorities in the process of future regional planning.…”
Section: Introductionmentioning
confidence: 99%
“…The maximum value of the ground-surface deformation was at the validation point P3 with a deformation value of 75 cm in the southeast direction. However, the ground-surface deformation values of the other validation points were between 2 and 5 cm (Hammad et al, 2019).…”
Section: Comparison Of Interferometry Results With D-gps Field Measurementsmentioning
confidence: 95%
“…Figure 5.40: Ground-surface deformation direction and magnitude values using D-GPS field measurements from 10 validation points in the Balloran Dam area during the study period. The star indicates the location of the landslide that occurred in March 2019 (Hammad et al, 2019).…”
Section: Comparison Of Interferometry Results With D-gps Field Measurementsmentioning
confidence: 99%
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