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Detection and Volume Estimation of Large-Scale Landslides Based on Elevation-Change Analysis Using DEMs Extracted From High-Resolution Satellite Stereo Imagery

机译:基于从高分辨率卫星立体图像中提取的DEM的高程变化分析的大型滑坡检测和体积估计

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A new technique for quickly assessing extensive areas of large-scale landslides that uses digital elevation models (DEMs) extracted from high-resolution satellite images is presented in this paper. The proposed technique observes the elevation changes by using multitemporal DEMs. Five-meter-resolution DEMs from SPOT-5 images are applied to two large-scale landslide disasters: the landslides triggered by the 2004 Mid Niigata prefecture earthquake (magnitude 6.8; a moderate-topography area in Central Japan), and the landslides caused by the 2004 typhoon Mindulle (a steep-topography area in Central Taiwan). Both events yielded elevation changes in excess of 10 m. We assess the DEMs produced by the proposed method and their landslide application. We find three main results. 1) The elevation difference error increases with the slope angle. The root-mean-square error was 4-5 m on slopes lower than 30deg in both areas, whereas it was 5-6 m for slopes that exceeded 30deg in moderate topographies and 5-9 m in steep topographies. 2) The proposed technique well delineated the large-scale landslides. The total rate of successful area detection was over 70% for slopes under 40 deg but under 40% for slopes that exceeded 40 deg. 3) The landslide volume could be roughly estimated in units of 100times103 m3. The developed technique well supports damage assessments of large-scale landslides because the location, depth, and volume can be quantitatively determined by remote sensing
机译:本文提出了一种新技术,该技术可使用从高分辨率卫星图像中提取的数字高程模型(DEM)快速评估大规模滑坡的广阔区域。所提出的技术通过使用多时间DEM来观察海拔变化。来自SPOT-5图像的五米分辨率DEM被应用于两次大规模的滑坡灾害:由2004年新泻县地震(震级6.8;日本中部中度地形区)触发的滑坡,以及由中部地区引起的滑坡。 2004年台风Mindulle(台湾中部的陡峭地形区域)。这两个事件都导致海拔变化超过10 m。我们评估了所提方法产生的DEM及其滑坡应用。我们发现三个主要结果。 1)高度差误差随倾斜角度而增加。在两个区域中,低于30度的坡度的均方根误差为4-5 m,而对于中度地形,坡度超过30度的坡度,其均值为5-6 m,在陡峭地势中坡度的均方根误差为5-9 m。 2)所提出的技术很好地描绘了大型滑坡。对于40度以下的坡度,成功的区域检测总成功率超过70%,但对于超过40度的坡度,则不到40%。 3)滑坡量可以粗略估计为100×103立方米。由于可以通过遥感定量确定位置,深度和体积,因此开发的技术很好地支持了大型滑坡的破坏评估

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