Robust model for retrieval sea surface current from different RADARSAT-1 SAR mode data

M. Marghany
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引用次数: 4

Abstract

This paper presents the application of robust model to simulate sea surface current pattern. We have developed the horizontal surface velocity model which is estimated from the Doppler frequency theory to model out the sea surface current velocity. The robust model was applied to the RADARSAT-1 SAR satellite at three different modes (Wide-3, High extended-6 and Standard-2). The results of the study were validated using real time in situ current measurements that were acquired by AWAC equipment. It is found that the velocity and direction of the current changed through the period of the study according to the changing of Doppler frequency shift. Onshore sea surface current was modeled from Wide-3 mode varied between 0.22 to 0.25 m/s, while sea surface current velocities extracted from the Extended High-6 and Standard-2 modes were ranged between 0.16 to 0.53 m/s and 0.52 to 0.65 m/s, respectively. The RMS difference between the three RADARSAT-1 SAR images is 0.136, 0.364, and 0.485 in the Standard-2, Wide-3, and Extended High-6 mode, respectively. This shows that RADARSAT-1 Standard-2 mode is the best mode which can be used to simulate sea surface current patterns (velocity and direction).
基于RADARSAT-1不同SAR模式数据反演海面洋流的鲁棒模型
本文介绍了鲁棒模型在海面流型模拟中的应用。我们建立了由多普勒频率理论估计的水平海面速度模型来模拟海面流速度。将鲁棒模型应用于RADARSAT-1 SAR卫星的三种模式(Wide-3、High - extended-6和Standard-2)。研究结果通过AWAC设备获取的实时现场电流测量结果进行了验证。根据多普勒频移的变化发现,在整个研究周期内,电流的速度和方向都发生了变化。基于Wide-3模式的近海海流变化范围为0.22 ~ 0.25 m/s,而基于Extended High-6和Standard-2模式的海流速度变化范围分别为0.16 ~ 0.53 m/s和0.52 ~ 0.65 m/s。三幅RADARSAT-1 SAR图像在Standard-2、Wide-3和Extended High-6模式下的均方根差分别为0.136、0.364和0.485。这表明RADARSAT-1标准-2模式是模拟海流模式(速度和方向)的最佳模式。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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