利用landsat 7-etm +卫星影像与水利模型hec-ras对比分析洪涝地区。案例研究:吉家河,斯洛博齐亚-丁格尼河段

Elena HuÈ›anu, Andrei Urzică, L. Paveluc, C. Stoleriu, A. Grozavu
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引用次数: 1

摘要

本研究的目的是将HEC-RAS水力模型得到的洪水带与Landsat 7-ETM+卫星图像处理得到的NDWI指数进行比较。研究区位于罗马尼亚东北部Moldavian高原的Jijia河上游,受2010年7月的洪水影响,卫星图像很好地捕捉到了这一影响。在那次事件中,丁格尼水文站的鸡家河水位达到了579厘米,远远超过了洪水水位。通过对相关河段进行不同的洪水模拟,应用NDWI指数发现了15.80 km的淹没面积,使用HEC-RAS水力模型发现了16.26 km的淹没面积。在现场分析之后,验证了HEC-RAS获得的值。Landsat 7-ETM+图像的淹水面积小了0.46 km,这可以用分辨率或云层的误差来解释。
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COMPARATIVE ANALYSIS OF FLOODED AREAS USING SATELLITE IMAGES LANDSAT 7-ETM+ AND HYDRAULIC MODEL HEC-RAS. CASE STUDY: THE JIJIA RIVER, SLOBOZIA-DINGENI SECTION
This study aims to make a comparison between flooded areas identified using the flood bands obtained with HEC-RAS hydraulic model, and the NDWI index resulted by processing Landsat 7-ETM+ satellite imagery. The study area was the upper sector of the Jijia River in Moldavian Plateau (North-Eastern Romania), affected by the July 2010 flood that was well caught in the satellite images. During that event the level of the Jijia River at Dingeni hydrometric station reached a value of 579 cm, far exceeding the level of flooding. Performing different flood simulations on the concerned river sector, a flooded area of 15.80 km has been revealed when applied the NDWI index, and a flooded area of 16.26 km when used the HEC-RAS hydraulic model. Following the field analysis, the values obtained with HEC-RAS are validated. The flooded area smaller by 0.46 km in the case of images Landsat 7-ETM+ could be explained by errors due to resolution or cloudiness.
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