利用高分三号SAR影像多普勒异常观测海锋

J. Wang, Yanlang Xu, Xiaoqing Wang, Boting Pan, Mingkai Tao, Haifeng Huang
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引用次数: 0

摘要

海锋、内波和海洋涡旋是常见的海洋物理现象。传统的观察方法是从图像灰度的角度出发,即使现有的深度学习网络也是基于图像灰度通过线检测。本文提出了一种新的观测方法,即相对于卫星天线反演海浪运动的多普勒异常。对于多普勒异常的估计,提出了一种基于贝叶斯估计方法的新算法,该算法通过迭代达到Cramer边界。为了验证算法的有效性,本文以高分三号SLC (single look complex image) SAR图像为例进行了实验。对反演结果的局部径向速度分布进行了分析。局部径向速度梯度分布,即海锋速度变化最大的地方,速度梯度变化最大,可以更好地解释海洋物理中的波浪调制效应。与传统的方法相比,我们的方法可以更好地理解和解释海洋物理现象,通过获取洋流的径向速度。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Observing Ocean Front by Retrieving Doppler Anomaly from GaoFen-3 SAR Images
Ocean front, internal wave and ocean vortex are general marine physical phenomena. The traditional observation method is from the angle of image gray level, even the existing deep learning network is based on image gray level through line detection. In this paper, a new observation method is proposed, that is, the retrieved Doppler anomaly of ocean wave motion relative to satellite antenna. For estimating Doppler anomaly, a new algorithm is proposed, which is based on Bayesian estimation method and reaches Cramer boundary through iteration. To verify the effectiveness of the algorithm, this paper uses GaoFen-3 SLC (single look complex image) SAR image. The results of local radial velocity distribution of inversion results are analyzed. The gradient distribution of local radial velocity, that is, the place where the velocity of ocean front changes the most, has the largest change in velocity gradient, which can better explain the wave modulation effect in ocean physics. Compared with the conventional method, our method can better understand and explain the marine physical phenomena by retrieving the radial velocity of ocean current.
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