通过相位历史生成模拟海洋SAR图像

J. Bennett, J. T. Clinthorne, A. O. Scheffler, J. Lyden
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引用次数: 0

摘要

本文给出了一种模拟海洋合成孔径雷达(SAR)图像的简单内波流图的方法。该方法同时计算振幅图像和雷达信号历史。所使用的仿真模型包括六个阶段。第一阶段,利用作用谱密度方程,从风速和风向计算两个空间坐标下的全波谱;在第二阶段,选择像素大小并将其作为将频谱划分为大尺度运动和小尺度运动的依据。然后计算大尺度海洋表面高度和速度的实现。第三阶段,利用传感器波长和几何形状计算小尺度统计量(雷达截面、相干时间、均方根、径向速度和均方根斜率)。在第四阶段,采用自回归方法生成与径向速度和径向速度方差一致的地表反射率历史实现。在第五阶段,信号历史是通过在适当的时间将反射率与SAR的适当天线加权函数相加来生成的。作为这一过程的结果,散斑自动包含在信号中。在最后阶段,可以通过使用任何传统方法处理信号历史来创建SAR图像,包括可变聚焦和多视处理。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Simulation of ocean SAR images via phase history generation
A method for simulating an ocean synthetic-aperture radar (SAR) image is illustrated for a simple internal wave current pattern. The method calculates both the amplitude image and the radar signal history. The simulation model used consists of six stages. In the first stage, the full wave spectrum in two spatial coordinates is calculated from the wind speed and direction using the action spectral density equation. In the second stage, the pixel size is selected and used as the basis for dividing the spectrum into large and small scale motions. Realizations for the large-scale ocean surface height and velocity are then calculated. In the third stage, the sensor wavelength and geometry are used to calculate the small scale statistics (radar cross section, coherence time, root-mean square (RMS), radial velocity and RMS slope). In the fourth stage, an autoregressive method is used to generate a realization of the surface reflectivity history that is consistent with the radial velocity and the radial velocity variance. In the fifth stage, the signal history is generated by summing the reflectivities at the proper times with the appropriate antenna weighting function for the SAR. As a consequence of this process, speckle is automatically included in the signal. In the final stage, the SAR image can be created by using any of the traditional ways to process the signal history, including variable focusing and multilook processing.<>
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