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Improved resolution backscatter measurements with the SeaWinds pencil-beam scatterometer

机译:使用SeaWinds笔形光束散射仪改善分辨率的反向散射测量

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摘要

The SeaWinds scatterometer was launched on the NASA QuikSCAT spacecraft in June 1999 and is planned for the Japanese ADEOS-II mission in 2000. In addition to generating a global Ku-band backscatter data set useful for a variety of climate studies, these flights will provide ocean-surface wind estimates for use in operational weather forecasting. SeaWinds employs a compact "pencil-beam" design rather than the "fan-beam" approach previously used with SASS on Seasat, NSCAT on ADEOS-I, and the AMI scatterometer on ERS-1, 2. As originally envisioned and reported, the resolution of the SeaWinds backscatter measurements were to be antenna-beamwidth limited. In order to satisfy an emerging demand for higher resolution backscatter data, however, the SeaWinds signal-processing design has been significantly modified. Here, the various options considered for improving the resolution of the SeaWinds measurements are discussed, and the selected hardware modification (the addition of deramp processing for range discrimination) is described. The radar equation specific to a rotating pencil-beam scatterometer with digital range filtering is developed, and the new challenges associated with calibrating the resulting improved resolution measurements are discussed. A formulation for assessing the variance of the measurements due to fading and thermal noise is presented. Finally, the utility of improved resolution SeaWinds measurements for land and ice studies is demonstrated by simulated enhanced-resolution imaging of a synthetic Earth backscatter scene.
机译:SeaWinds散射仪于1999年6月在NASA QuikSCAT航天器上发射升空,计划于2000年进行日本ADEOS-II任务。除了生成可用于各种气候研究的全球性Ku波段反向散射数据集外,这些飞行还将提供海洋地表风估计,用于业务天气预报。 SeaWinds采用紧凑的“铅笔束”设计,而不是先前与Seasat上的SASS,ADEOS-I上的NSCAT和ERS-1 2上的AMI散射计一起使用的“扇形束”方法。 SeaWinds背向散射测量的分辨率受到天线波束宽度的限制。为了满足对高分辨率反向散射数据的新兴需求,SeaWinds信号处理设计已进行了重大修改。在此,讨论了用于提高SeaWinds测量分辨率的各种选项,并描述了所选的硬件修改(增加了用于范围识别的deramp处理)。开发了具有数字范围滤波功能的旋转铅笔射束散射仪特有的雷达方程,并讨论了与校准由此产生的改进的分辨率测量相关的新挑战。提出了一种用于评估由于衰落和热噪声导致的测量方差的公式。最后,通过模拟增强分辨率的合成地球反向散射场景的成像,证明了高分辨率SeaWinds测量在陆地和冰雪研究中的实用性。

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