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Research on upwelling region wind speed correction method for wind retrieval from SAR imagery along the Zhejiang coast

机译:浙江沿海SAR图像上涌区域风速校正方法研究。

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The synthetic aperture radar (SAR) has been proven to be a valuable tool for high resolution ocean surface wind measurements, which is especially important for coastal waters. However, oceanic surface phenomena observed by SAR and oceanic processes which can cause the change of backscatter in SAR imagery will influence the SAR wind retrieval. Upwelling is one of the main factors and it is prevalent in summer along the Zhejiang Coast. It smoothes the sea surface which results in the lower backscatter cross section in SAR imagery. In this article, using sea surface temperature (SST) and chlorophyll2-a data derived from EOS MODIS, the low backscatter features in ENVISAT ASAR imagery are analyzed along the Zhejiang Coast in the East China Sea. And then CMOD4 algorithm is adopted to retrieve the sea surface wind speed, using wind directions from interpolated NCEP / NCAR reanalysis data. The result of wind speed is negatively biased due to the low Normalized Radar Cross Section (NRCS) associated with the Zhejiang Coastal Upwelling. In order to resolve impact of the coastal upwelling on SAR wind retrieval, combining high resolution numerical meteorological model wind field data, a wind speed correction model is proposed using linear robust regression. Results show that the accuracy of SAR wind retrieval is improved in upwelling region.
机译:合成孔径雷达(SAR)已被证明是高分辨率海面风测量的重要工具,这对沿海水域尤其重要。然而,由SAR观测到的海洋表面现象和可能导致SAR影像反向散射变化的海洋过程将影响SAR风的反演。上升流是主要因素之一,在浙江沿海夏季盛行。它可以平滑海面,从而在SAR图像中产生较低的反向散射横截面。在本文中,使用海面温度(SST)和来自EOS MODIS的叶绿素2-a数据,对ENVISAT ASAR图像中的低反向散射特征进行了分析,并研究了东海浙江沿岸的情况。然后,采用CMOD4算法,根据内插NCEP / NCAR再分析数据中的风向,检索海面风速。由于与浙江沿海上升流相关的归一化雷达横截面(NRCS)低,风速的结果产生了负偏倚。为了解决沿海上升流对SAR风反演的影响,结合高分辨率数值气象模型风场数据,提出了一种采用线性鲁棒回归的风速校正模型。结果表明,在上升流区,SAR风的反演精度得到了提高。

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