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Measuring Deformation in Jakarta through Long Term Synthetic Aperture Radar (SAR) Data Analysis

机译:通过长期合成孔径雷达(SAR)数据分析测量雅加达的变形

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Jakarta as a home for more than 10 millions habitant facing complex environmental problems due to physical development that cause physical deformation. Physical deformation issues such as decreasing environmental carrying capacity, land cover changes and land subsidence have occurred. Recent studies shows that the long of shoreline changes in a span of 13 years from 2002 to 2015 around 14 km due to land reclamation in Jakarta bay. Previous studies also concluded that Jakarta suffer a sinking phenomena due to its rapid subsidence rate, approximately 260 mm/year in northern part of Jakarta. During the 2007 to 2011, the land subsidence phenomena in Jakarta was observed by InSAR based on ALOS-PALSAR data and found that the subsided areas only occurred in certain areas, mainly in Pluit and Cengkareng regions, with a subsidence of approximately 70 cm for 4 years. Land subsidence is generally related to geological subsidence i.e. sediment consolidation due to its own weight and tectonic movements; or related to human activities such as withdrawal of ground water and geothermal fluid, oil and gas extraction from underground reservoirs, and collapse of underground mines. The amount of subsidence or uplift can be estimated from the number of concentric fringes that appear in the interferogram. This research utilizes Synthetic Aperture Radar (SAR) data observed from ALOS-2 (L-band) and Sentinel-1 (C-band) satellites. By interfering two single look complex (SLC) images from different observation epoch, it is found that the subsided area that has been identified before continues to subside. This occurs especially in Pluit region and has been revealed by interfering ALOS-2 data up to year 2016. The deformation in this area is approximately 12 cm from November 2015 to September 2016. The process of land reclamation also clearly identified by Sentinel-1 image by series data processing in Sentinels Application Platform (SNAP) software.
机译:雅加达作为一个超过10万升的家庭习惯,面临复杂的环境问题,因为物理发展导致身体变形。发生了物理变形问题,如环保承载力,陆地覆盖变化和土地沉降。最近的研究表明,由于在雅加达湾的土地填海陆地垦区,2002年至2015年截至2002年至2015年的跨度,长期的海岸线变化。以前的研究还得出结论,雅加达由于其临时率快,雅加达北部约260毫米/年而遭受沉没现象。在2007年至2011年期间,雅加达的土地沉降现象是根据Alos-Palsar数据的初始观察到的,发现该区域仅发生在某些领域,主要在塑料和旧乐都地区,沉降约70厘米年。土地沉降通常与地质沉降有关,因为它的重量和构造运动导致沉积物整合;或与人类活动有关,例如从地下水库撤出地下水和地热流体,油气提取,以及地下矿山的崩溃。可以从干涉图中出现的同心条纹的数量估计沉降或隆起的量。该研究利用从AlOS-2(L波段)和Sentinel-1(C波段)卫星观察到的合成孔径雷达(SAR)数据。通过干扰来自不同观察时代的两个单眼复杂(SLC)图像,发现之前已经识别的消退区域继续下划。这尤其是在Pluit地区发生,并且通过干扰2016年的Alos-2数据已经揭示。该领域的变形从2015年11月到2016年11月约为12厘米。土地填海过程也明确通过Sentinel-1图像确定了土地填海过程通过Sentinels应用程序平台(SNAP)软件中的序列数据处理。

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