首页> 外文会议>2013 US National Committee of URSI National Radio Science Meeting >On the estimation of wind vectors over the sea surface from near-nadir radar observations
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On the estimation of wind vectors over the sea surface from near-nadir radar observations

机译:从近天底雷达观测估计海面风矢量

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The remote sensing of wind vectors over the sea surface using microwave scatterometry has a long history. Traditional scatterometer systems operate at moderate incidence angles in order to emphasize the Bragg scatter component of the sea surface normalized radar cross section (NRCS), and typically require multiple azimuth “looks” in order to reduce ambiguities in the determination of wind direction. In contrast, radar systems designed for atmospheric sensing from aircraft frequently operate in a near-nadir configuration, with cross-track scanning utilized in some cases. This study explores the potential use of such atmospheric radar measurements for wind vector retrieval through a Monte Carlo simulation method. A maximum likelihood estimation of wind vectors is utilized for simulated measurements corrupted by speckle and thermal noise.
机译:使用微波散射法对海面上的风向进行遥感已有很长的历史。传统散射仪系统以中等入射角运行,以强调海面归一化雷达横截面(NRCS)的布拉格散射分量,并且通常需要多个方位角“外观”,以减少确定风向时的歧义。相比之下,为飞机的大气感应而设计的雷达系统通常以接近天底的配置运行,在某些情况下会使用跨轨扫描。这项研究探索了通过蒙特卡洛模拟方法将此类大气雷达测量结果用于风矢量检索的潜在用途。风矢量的最大似然估计用于被斑点和热噪声破坏的模拟测量。

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