首页> 外文会议>International Society for Photogrammetry and Remote Sensing Commission Technical Commission Symposium >FLOOD HAZARD MAPPING BY SATELLITE IMAGES AND SRTM DEM IN THE VU GIA - THU BON ALLUVIAL PLAIN, CENTRAL VIETNAM
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FLOOD HAZARD MAPPING BY SATELLITE IMAGES AND SRTM DEM IN THE VU GIA - THU BON ALLUVIAL PLAIN, CENTRAL VIETNAM

机译:卫星图像和SRTM DEM在VU GIA的洪水危险 - Thu Bon Illuvial Plane,中央越南

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The objective of this study is to generate a flood hazard map based on geomorphologic approach employing Shuttle Radar Topographic Mission (SRTM) DEM and satellite image data (ASTER and LANDSAT). Supervised classification of satellite images is implemented to characterize land cover types. Moreover, the Modified Normalized Difference Water Index (MNDWI) is undertaken to identify moist surface or saturated areas to separate flood and non-flooded areas. SRTM DEM categorization of height range is incorporated with the results of surface analysis from unsupervised classification and MNDWI to delineate the flood affected areas in relation with geomorphologic features. The results are compared with landform classification map and flood hazard map generated by image visual interpretation, field survey, topographic maps and past flood inundation maps. A case study is conducted in the alluvial plain of the Vu Gia - Thu Bon River system, central Vietnam. The extraction of moist soil by MNDWI can help to detect flooded sites and this result is compared with the landform classification map, SRTM DEM elevation ranges and land cover classification. The comparison reveals close relationship between water saturated areas, elevation ranges, and flood condition that the areas with elevation lower than 4m and classified as flood basin and deltaic lowland are inundated deeply and for rather long duration. Higher areas such as terraces and sand dunes are not flooded and natural levees are less flood-affected. Moreover, this study proves the significance of MNDWI for separating moist soil for flood prediction.
机译:本研究的目的是基于采用穿梭雷达地形任务(SRTM)DEM和卫星图像数据(ASter和Landsat)的地貌方法产生洪水危险地图。监督卫星图像的分类被实施为表征陆地覆盖类型。此外,修改的归一化差异水指数(MNDWI)进行了鉴定潮湿的表面或饱和区域,以分离洪水和非洪水区域。 SRTM DEM对高度范围的分类是由无监督分类和MNDWI的表面分析结果的结果,以描绘与地貌特征相关的洪水影响区域。结果与图像视觉解释,现场调查,地形图和过去的洪水淹没地图生成的地形分类图和洪水危险地图进行了比较。越南市中部vu Gia - Thu Bon River System的冲积平原,案例研究。 MNDWI的湿润土壤提取可以帮助检测淹没的位置,并将这种结果与地形分类图进行比较,SRTM DEM海拔和陆地覆盖分类。比较揭示了水饱和面积,海拔范围和洪水条件之间的密切关系,即高度低于4米并被归类为洪水盆地和德伦兰低地的区域深入淹没,持续长期。梯田和沙丘等更高的区域不会被淹没,天然的levees缺乏洪水影响。此外,该研究证明了MNDWI对洪水预测分离湿土的重要性。

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