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星载SAR浅海水下地形和水深测量模拟仿真──水下地形高度、坡度和方向与可测水深分析

傅斌 黄韦艮 周长宝 杨劲松 史爱琴 厉冬玲

傅斌, 黄韦艮, 周长宝, 杨劲松, 史爱琴, 厉冬玲. 星载SAR浅海水下地形和水深测量模拟仿真──水下地形高度、坡度和方向与可测水深分析[J]. 海洋学报, 2001, 23(1): 35-42.
引用本文: 傅斌, 黄韦艮, 周长宝, 杨劲松, 史爱琴, 厉冬玲. 星载SAR浅海水下地形和水深测量模拟仿真──水下地形高度、坡度和方向与可测水深分析[J]. 海洋学报, 2001, 23(1): 35-42.
FU Bin, HUANG Wei-gen, ZHOU Chang-bao, YANG Jing-song, SHI Ai-qin, LI Dong-lin. Simulation study of sea bottom topography mapping by spaceborne SAR——Relationship between topographic parameters and measurement of water depth[J]. Haiyang Xuebao, 2001, 23(1): 35-42.
Citation: FU Bin, HUANG Wei-gen, ZHOU Chang-bao, YANG Jing-song, SHI Ai-qin, LI Dong-lin. Simulation study of sea bottom topography mapping by spaceborne SAR——Relationship between topographic parameters and measurement of water depth[J]. Haiyang Xuebao, 2001, 23(1): 35-42.

星载SAR浅海水下地形和水深测量模拟仿真──水下地形高度、坡度和方向与可测水深分析

基金项目: 总装备部卫星应用资助项目(Y96#09);国家“863”项目资助项目(818-06-02);航天“863”项目资助项目(863-2-7-4-15);国家海洋局第二海洋研究所青年基金资助项目(9705).

Simulation study of sea bottom topography mapping by spaceborne SAR——Relationship between topographic parameters and measurement of water depth

  • 摘要: 根据星载合成孔径雷达(SAR)浅海水下地形和水深成像机理,建立了浅海水下地形和水深雷达后向散射截面仿真模型.利用该模型模拟并分析了不同地形条件下,浅海水下地形的雷达后向散射截面.分析结果表明,水下地形高度越高,SAR可测量的水深越深;水下地形坡度越大,越易被SAR所观测.水下地形的星载SAR测量还与水下地形的方向有关,与卫星飞行方向平行的水下地形最易被SAR观测,与卫星飞行方向垂直的水下地形最不易被SAR观测.
  • de LOOR G P.The observation of tidal patterns,currents and bathymetry with SLAR imagery of the sea[J].IEEE Trans Geosci Electron,1981,OE-6:124~129.
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    黄韦艮,高曼娜,周长宝,等.SAR浅海水下地形测量[A].郭华东,徐冠华.星载SAR雷达应用研究[M].北京:科学出版社,1996.172~180.
    ALPERS W,HENNINGS I.A theory of the imaging mechanism of underwater bottom topography by real and synthetic aperture radar[J].Journal of Geophysical Research,1984,89:10 529~10 546.
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出版历程
  • 收稿日期:  1999-05-28
  • 修回日期:  2000-06-02

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