首页> 外文会议>International Society for Photogrammetry and Remote Sensing Commission Technical Commission Symposium >CONTINUOUS MONITORING OF LANDSLIDES AREA CAUSED BY IWATE-MIYAGI NAIRIKU EARTHQUAKE IN 2008 USING ALOS IMAGES
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CONTINUOUS MONITORING OF LANDSLIDES AREA CAUSED BY IWATE-MIYAGI NAIRIKU EARTHQUAKE IN 2008 USING ALOS IMAGES

机译:2008年使用ALOS图像持续监测2008年IWATE-Miyagi Nairiku地震引起的山体滑坡区域

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The Iwate-Miyagi Nairiku earthquake struck inland area in northern Japan on June 14, 2008. This earthquake triggered landslides in mountainous area. The landslides changed land coverage from forest to bare soil. Aftermath of the disaster occurrence, many satellites observed target area to identify the damage. In this study, we report on long-term observation for damaged area using ALOS satellite after the earthquake occurrence. The landslide on north of the Aratozawa-dam lake is the largest one by this earthquake. The landslide area is identified by PALSAR single polarization intensity image. Sediments by the landslide were deposited into the dam lake and they caused rise of water level immediately after the earthquake. Temporal change of water level is observed by PALSAR single polarization intensity images. Normalized difference calculation from two of AVNIR-2 band 3 data is helpful to extract temporal change of landslide area. Pan-sharpen image of AVNIR-2 and PRISM is effective to extract small scale change on the damaged area. Satellite remote sensing data is records of reconstruction process and secondary damage for time span of several years.
机译:2008年6月14日,IWATE-Miyagi Nairiku地震袭击了日本北部的内陆地区。这种地震触发了山区的山体滑坡。山体滑坡从森林变为赤土土。发生灾难发生后,许多卫星观察了目标区域以识别损坏。在这项研究中,我们在地震发生后使用Alos卫星进行了损坏区域的长期观察。 Aratozawa-Dam Lake北部的滑坡是这种地震最大的山体滑坡。滑坡区域由Palsar单极化强度图像识别。山体滑坡沉积物沉积在坝湖中,并在地震后立即引起水位的上升。观察Palsar单极化强度图像观察水位的时间变化。 AVNIR-2频段3数据中的两个数据归一化差异计算有助于提取滑坡区域的时间变化。 AVNIR-2和棱镜的PAN锐化图像有效地提取受损区域的小规模变化。卫星遥感数据是重建过程的记录和几年的时间范围的次要损坏。

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