首页> 外文会议>International conference on remote sensing for marine and coastal environments >MORPHODYNAMIC IN THE ELBE ESTUARY AS SEEN BY ERS SYNTHETIC APERTURE RADAR Edzard Romaneessen; Susanne Lehner; Andreas Niedermeier; Jochen Horstmann
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MORPHODYNAMIC IN THE ELBE ESTUARY AS SEEN BY ERS SYNTHETIC APERTURE RADAR Edzard Romaneessen; Susanne Lehner; Andreas Niedermeier; Jochen Horstmann

机译:ERS合成孔径雷达观察到的易北河口形态动力学苏珊·莱纳(Susanne Lehner); Andreas Niedermeier;约臣·霍斯特曼(Jochen Horstmann)

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The intertidal area of the German Bight is continuously changing its topography due to morphodynamic processes. This fact has serious impact on the German waterways, requiring a huge amount dragging with costs of about 80 mio DM per annum. In order to better monitor these morphodynamic processes and to continuously update the changing bottom topography, Synthetic Aperture Radar (SAR) data of the European Remote Sensing Satellite (ERS)-l and 2 are used in the estuary of the river Elbe. The SAR is an active sensor and therefore very useful for this study as it is possible to extract the land water boundary - the shoreline - during all weather conditions as well as during day and night. In this paper a combination of wavelet and active contour model is used to extract the shoreline information from 12 ERS SAR images acquired between 19 December 1996 and 25 July 1998. These shorelines are combined with hight information from the nearby tide gauge at Cuxhaven Steubenhoeft and interpolated to DEM of the small sandbank Medemsand. The comparison with a conventional generated DEM provided by the German Federal Waterway Engineering and Research Institute (BAW) using using vessel mounted echo sounder measurements from 1997 show a general very good agreement. Difference between both images can be explained by changes in the bottom topography due to morphodynamic processes.
机译:由于形态动力学过程,德国湾的潮间带地区不断改变其地形。这一事实对德国水道产生了严重影响,需要大量的拖曳,每年的成本约为80 mio DM。为了更好地监视这些形态动力学过程并不断更新变化的底部地形,在易北河河口使用了欧洲遥感卫星(ERS)-1和2的合成孔径雷达(SAR)数据。 SAR是一种有源传感器,因此对本研究非常有用,因为在所有天气条件下以及白天和黑夜都可以提取陆地边界水域-海岸线。本文采用小波和主动轮廓模型相结合的方法,从1996年12月19日至1998年7月25日之间采集的12幅ERS SAR图像中提取海岸线信息。到小型沙岸Medemsand的DEM。与德国联邦水道工程与研究所(BAW)提供的常规生成的DEM的比较,使用的是1997年以来的船载回声测深仪测量结果,显示出总体非常好的一致性。两个图像之间的差异可以通过形态动力学过程导致的底部地形变化来解释。

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