SAR-image derived soil moisture enhancement using GPR data

M. Nottebaere, M. Ardekani, S. Lambot, X. Neyt
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引用次数: 1

Abstract

Measuring the spatial distribution of soil moisture is important for agricultural, hydrological, meteorological and climatological research and applications. In this study, a new technique is developed to create soil moisture maps, based on the inversion of SAR measurements (RADARSAT-2, fine quad polarization) combined with GPR measurements. The Integral Equation Model is used to invert the SAR measurements, assuming a constant surface roughness and correlation length for the entire field, while the GPR data are inverted using a full wave inversion method. High resolution GPR measurements taken at different times under different land and weather conditions are used to generate a relative soil moisture landscape. We assume that these soil moisture difference patterns show little variation over time. By combining the inverted SAR data with a transformation of the soil moisture difference landscape, a high resolution soil moisture map is generated. The high resolution soil moisture maps show good agreement with the measured GPR soil moisture maps. The advantage of this technique is that once the relative soil moisture difference landscape is created, it allows the creation of new high resolution soil moisture maps later, by only taking a SAR image.
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利用探地雷达数据增强sar图像的土壤湿度
测量土壤水分的空间分布对农业、水文、气象和气候学的研究和应用具有重要意义。在本研究中,基于SAR测量(RADARSAT-2,精细四极化)与GPR测量相结合的反演,开发了一种创建土壤湿度图的新技术。采用积分方程模型对SAR测量数据进行反演,假设整个场的表面粗糙度和相关长度恒定,而GPR数据则采用全波反演方法进行反演。在不同的土地和天气条件下,采用不同时间的高分辨率探地雷达测量来生成相对土壤湿度景观。我们假设这些土壤湿度差异模式随时间变化不大。将反演的SAR数据与土壤水分差异景观转换相结合,生成高分辨率的土壤水分图。高分辨率土壤湿度图与探地雷达实测土壤湿度图吻合较好。这种技术的优点是,一旦相对土壤湿度差异景观被创建,它允许创建新的高分辨率土壤湿度地图之后,只需要一个SAR图像。
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