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Soil moisture evaluation by means of multi-temporal ERS SAR PRI images and interferometric coherence

机译:利用多时相ERS SAR PRI图像和干涉相干性评估土壤湿度

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The feasibility of using multi-temporal spaceborne Synthetic Aperture Radar (SAR) imagery for the evaluation of soil moisture at a field and regional scale is evaluated through the use of European Remote Sensing Satellite (ERS-1 and ERS-2) images. Six pairs of Single Look Complex (SLC) images and six Precision Images (PRI) were acquired during the 1996 Tandem mission for the test site of Gembloux, in Belgium. The SLC images of each Tandem pair were processed by the "Centre Spatial de Liege" (CSL) in order to produce interferometric coherence images, and the PRI were calibrated; all the images were coregistered and rectified. The backscattering coefficient values and the mean coherence values were calculated for each pilot field and compared with soil moisture and crop characteristics measurements. Our study confirms that for bare soil fields, a Linear relationship exists between the volumetric near-surface soil moisture and the backscattering coefficient for unsaturated soils, with a determination coefficient of 0.75. The innovative key point of the study shows an excellent correlation between the backscatter value of the image subset of the test site (80 sq. km), and the corresponding mean soil moisture measurements, with a determination coefficient of 0.98. The image subset comprises mostly agricultural fields but also forests, meadows and urban areas. Moreover, the relation is as valid in the spring, before the growing season, as in the summer, when the vegetation cover is high. The study also reveals that coherence images are useful to identify bare soil fields. (C) 2000 Elsevier Science B.V. All rights reserved. [References: 10]
机译:通过使用欧洲遥感卫星(ERS-1和ERS-2)图像,评估了使用多时空星载合成孔径雷达(SAR)图像在野外和区域范围内评估土壤湿度的可行性。在1996年Tandem任务期间,在比利时Gembloux的测试地点获得了六对单眼复杂图像(SLC)和六幅精确图像(PRI)。每个串联对的SLC图像均由“中央空间局”(CSL)处理,以产生干涉相干图像,并校准PRI。所有图像均已注册并校正。计算每个试验田的反向散射系数值和平均相干值,并将其与土壤水分和作物特性测量值进行比较。我们的研究证实,对于裸露的土壤田,近地表土壤含水量与非饱和土壤的反向散射系数之间存在线性关系,确定系数为0.75。该研究的创新重点表明,测试地点的图像子集(80平方公里)的反向散射值与相应的平均土壤湿度测量值之间具有极好的相关性,测定系数为0.98。图像子集主要包括农田,但也包括森林,草地和城市地区。而且,这种关系在春季,生长季节之前和夏季在植被覆盖度高的情况下同样有效。该研究还揭示了相干图像对于识别裸露的土壤田地很有用。 (C)2000 Elsevier Science B.V.保留所有权利。 [参考:10]

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