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Validating a scatterometer wind algorithm for ERS-1 SAR

机译:验证ERS-1 SAR的散射仪风算法

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The ocean surface wind field is observed from space operationally using scatterometry. The European Space Agency's (ESAs) ERS-1 satellite scatterometer routinely produces a wind product that is assimilated into forecast models. Scatterometry cannot give accurate wind estimates close to land, however, because the field of view of a spaceborne scatterometer is on the order of 50 km. Side lobe contamination, due to the large contrast in backscatter between land and water, compounds the problem. Synthetic aperture radar (SAR) can provide wind speed and direction estimates on a finer scale, so that high-resolution wind fields can be constructed near shore. An algorithm has been developed that uses the spectral expression of wind in SAR imagery to estimate wind direction and calibrated backscatter to estimate wind strength. Three versions, based on C-band scatterometer algorithms, are evaluated for accuracy in potential operational use. Algorithm estimates are compared with wind measurements from buoys in the Gulf of Alaska, Bering Strait, and off the Pacific Northwest coast by using a data set of 61 near-coincident buoy and ERS-1 SAR observations. Representative figures for the accuracy of the algorithm are /spl plusmn/2 m/s for wind speed and /spl plusmn/37/spl deg/ for wind direction at a 25-km spatial resolution.
机译:使用散射法从空间上观察海洋表面风场。欧洲航天局(ESA)的ERS-1卫星散射仪通常会产生一种风产品,该风产品会被同化为预报模型。但是,由于星载散射仪的视场约为50 km,因此散射测量无法给出接近陆地的准确风速估算值。由于陆地和水之间的反向散射差异很大,因此旁瓣污染加剧了这一问题。合成孔径雷达(SAR)可以提供更精细的风速和风向估计,因此可以在海岸附近构建高分辨率风场。已经开发了一种算法,该算法使用SAR图像中风的频谱表达式来估计风向,并使用校准后向散射来估计风强度。评估了基于C波段散射仪算法的三个版本的潜在操作用途的准确性。通过使用61个重合浮标和ERS-1 SAR观测数据集,将算法估计值与阿拉斯加湾,白令海峡和西北太平洋沿岸浮标的风测量值进行比较。该算法的精度的典型数字是风速为/ spl plusmn / 2 m / s,风速为25 km / s时为/ spl plusmn / 37 / spl deg /。

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