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基于SAR子孔径分解的海表面二维流场反演

张佳辉 苗洪利 杨忠昊 刘昆池

张佳辉,苗洪利,杨忠昊,等. 基于SAR子孔径分解的海表面二维流场反演[J]. 海洋学报,2023,45(8):24–30 doi: 10.12284/hyxb2023094
引用本文: 张佳辉,苗洪利,杨忠昊,等. 基于SAR子孔径分解的海表面二维流场反演[J]. 海洋学报,2023,45(8):24–30 doi: 10.12284/hyxb2023094
Zhang Jiahui,Miao Hongli,Yang Zhonghao, et al. Two-dimensional sea surface current field inversion based on SAR sub-aperture decomposition[J]. Haiyang Xuebao,2023, 45(8):24–30 doi: 10.12284/hyxb2023094
Citation: Zhang Jiahui,Miao Hongli,Yang Zhonghao, et al. Two-dimensional sea surface current field inversion based on SAR sub-aperture decomposition[J]. Haiyang Xuebao,2023, 45(8):24–30 doi: 10.12284/hyxb2023094

基于SAR子孔径分解的海表面二维流场反演

doi: 10.12284/hyxb2023094
基金项目: 国家自然科学重点基金(62031005);山东省自然科学基金(ZR2020MD097)。
详细信息
    作者简介:

    张佳辉(1998-),男,山东省青岛市人,主要从事海洋微波遥感研究。E-mail: zhangjiahui@stu.ouc.edu.cn

    通讯作者:

    苗洪利(1964-),男,山东省青岛市人,教授,主要从事海洋微波遥感研究。E-mail: oumhl@ouc.edu.cn

  • 中图分类号: P714+.1;P731.21

Two-dimensional sea surface current field inversion based on SAR sub-aperture decomposition

  • 摘要: 对Radarsat-2和Sentinel-1A分别观测的两个海域的单景SAR图像进行子孔径分解,各自得到不同方位角上的两幅SAR子孔径图像。使用多普勒质心频移法分别对不同方位角的两幅SAR图像进行海流反演,并进行海流矢量合成,采用经过时空匹配的HYCOM模式数据对反演结果进行检验,结果表明:Radarsat-2观测的SAR图像分解的两幅子孔径SAR图像矢量合成后的海流与HYCOM模式数据相比,速度均方根值为0.09 m/s,相关系数为0.64;方向均方根值为10.49°,相关系数为0.78。Sentinel-1A观测的SAR图像分解的两幅子孔径SAR图像矢量合成后的海流与HYCOM模式数据相比,速度均方根值为0.06 m/s,相关系数为0.82;方向均方根值为2.85°,相关系数为0.86。由此可见,基于单景SAR分解的两幅子孔径SAR图像可以有效反演二维海流。其反演精度与雷达视向和真实海流矢量的方向有关,二者的角度越小,反演海流矢量的精度越高。
  • 图  1  子孔径分解流程

    Fig.  1  Sub-aperture decomposition flowchart

    图  2  流速矢量几何关系

    Fig.  2  Geometric relation of current velocity vector

    图  3  Radarsat-2卫星全孔径SAR强度图

    Fig.  3  Full-aperture SAR intensity image of Radarsat-2 satellite

    图  4  Sentinel-1A卫星全孔径SAR强度图

    Fig.  4  Full-aperture SAR intensity image of Sentinel-1A satellite

    图  5  分解后各子孔径SAR图像

    Fig.  5  SAR images of each sub-aperture after decomposition

    图  6  全孔径雷达视向海流

    Fig.  6  Sea surface current at full-aperture radar looking direction

    图  7  子孔径海表面流图

    Fig.  7  Sea surface current of sub-aperture images

    图  8  SAR反演的海流矢量与HYCOM海流矢量对比图

    Fig.  8  Comparison diagram of SAR inverted current vector and HYCOM current vector

    图  9  反演海流矢量与HYCOM值散点图

    Fig.  9  Scatter plots of inverted current vector and HYCOM values

    图  10  SAR反演的海流矢量与HYCOM海流矢量对比图

    Fig.  10  Comparison diagram of SAR inverted current vector and HYCOM current vector

    图  11  合成海流矢量与HYCOM值相关散点图

    Fig.  11  Scatter plots of synthesized current vector and HYCOM values

    表  1  反演海流矢量与HYCOM值统计结果

    Tab.  1  Statistical results of inverted current vector and HYCOM values

    速度方向
    平均偏差−0.08 m/s9.98°
    均方根差0.09 m/s10.49°
    相关系数0.640.78
    下载: 导出CSV

    表  2  合成海流矢量与HYCOM值统计结果

    Tab.  2  Statistical results of synthesized current vector and HYCOM values

    速度方向
    平均偏差−0.05 m/s2.72°
    均方根差0.06 m/s2.85°
    相关系数0.820.86
    下载: 导出CSV
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出版历程
  • 收稿日期:  2022-12-30
  • 修回日期:  2023-03-23
  • 网络出版日期:  2023-08-18
  • 刊出日期:  2023-08-31

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