MONITORING THE SLOWLY DEVELOPING LANDSLIDE WITH THE INSAR TECHNIQUE IN SAMSUN PROVINCE, NORTHERN TURKEY

Q2 Social Sciences
S. Coşkun, Ç. Bayık, S. Abdikan, T. Gorum, F. Balik Sanli
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引用次数: 0

Abstract

Abstract. Landslides are prominent natural events with high destructive power. Since they affect large areas, it is important to monitor the areas they cover and analyse their movement. Remote sensing data and image processing techniques have been used to monitor landslides in different areas. Synthetic aperture radar (SAR) data, particularly with the Interferometric SAR (InSAR) method, is used to determine the velocity vector of the surface motion. This study aims to detect the landslide movements in Samsun, located in the north of Turkey, using persistent scattering InSAR method. Archived Copernicus Sentinel-1 satellite images taken between 2017 and 2022 were used in both descending and ascending directions. The results revealed surface movements in the direction of the line of sight, ranging between −6 and 6 mm/year in the study area. Persistent Scatterer (PS) points were identified mainly in human structures such as roads, coasts, ports, and golf courses, especially in settlements. While some regions exhibited similar movements in both descending and ascending results, opposite movements were observed in some regions. The results produced in both descending and ascending directions were used together and decomposed into horizontal and vertical deformation components. It was observed that the western coastal part experienced approximately 4.5 cm/year vertical deformation, while the central part there is more significant horizontal deformation, reaching up to approximately 6 cm/year.
用INSAR技术监测土耳其北部萨姆森省缓慢发展的滑坡
摘要滑坡是突出的自然事件,具有很高的破坏力。由于它们影响的区域很大,因此监测它们所覆盖的区域并分析它们的运动是很重要的。遥感数据和图像处理技术已被用于监测不同地区的山体滑坡。合成孔径雷达(SAR)数据,特别是干涉SAR(InSAR)方法,用于确定表面运动的速度矢量。本研究旨在利用持续散射InSAR方法探测土耳其北部Samsun的滑坡运动。2017年至2022年间拍摄的哥白尼哨兵1号存档卫星图像用于下降和上升方向。结果显示,研究区域内的地表向视线方向移动,范围在−6至6毫米/年之间。持久性散射点主要在道路、海岸、港口和高尔夫球场等人类结构中发现,尤其是在定居点。虽然一些区域在下降和上升结果中表现出相似的运动,但在一些区域观察到相反的运动。在下降和上升方向上产生的结果被一起使用,并分解为水平和垂直变形分量。据观察,西部沿海地区经历了大约4.5厘米/年的垂直变形,而中部地区则出现了更显著的水平变形,达到了大约6厘米/年。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
CiteScore
1.70
自引率
0.00%
发文量
949
审稿时长
16 weeks
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