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Soil moisture monitoring over a semiarid region using Envisat ASAR data

机译:使用Envisat ASAR数据监测半干旱地区的土壤湿度

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Soil moisture (SM) is of fundamental importance to many agricultural, hydrological and climate studies. In this paper, a simple approach for mapping near-surface SM from Envisat ASAR data was developed. Four high-resolution images covering a semiarid region in Algeria were acquired with the same sensor configuration. We performed the pretreatment using the Basic Envisat SAR Toolbox of the European Space Agency. Then, we extracted the backscattering coefficient σ~0 (dB) from the filtered and calibrated images. On the other hand, five training sites with different soil physical properties and vegetation cover were selected for monitoring SM. The field campaigns were conducted concurrent to satellite image acquisitions to measure soil water content in the top five centimeters using the gravimetric method. The study of linear regressions associated to the change detection approach allowed the expression of the backscattering coefficient as a function of volumetric soil moisture (σ~0 = a*θ + b). The coefficients "a" and "b" of the equation slightly differ from one site to another and also from one season to the next. This difference is mainly due to the effects of surface roughness and vegetation biomass variations. Our study confirms a good agreement between the volumetric near-surface SM and the radar backscattering coefficient for all the test fields. The comparison between measured and estimated SM proves the accuracy of the inversion models used here with a mean average error of less than 5%. At the end, high resolution maps of soil moisture distribution were obtained from the acquired radar images.
机译:土壤水分(SM)对于许多农业,水文和气候研究至关重要。本文提出了一种从Envisat ASAR数据绘制近地表SM的简单方法。使用相同的传感器配置获取了覆盖阿尔及利亚半干旱地区的四张高分辨率图像。我们使用欧洲航天局的Basic Envisat SAR工具箱进行了预处理。然后,我们从滤波和校准后的图像中提取后向散射系数σ〜0(dB)。另一方面,选择了五个具有不同土壤物理特性和植被覆盖度的培训地点来监测SM。野外活动与卫星图像采集同时进行,以使用重量分析法测量顶部五厘米的土壤水分。对与变化检测方法相关的线性回归的研究允许将反向散射系数表示为土壤水分的函数(σ〜0 = a *θ+ b)。该方程的系数“ a”和“ b”在一个站点之间到另一个站点之间以及从一个季节到下一个季节都略有不同。这种差异主要是由于表面粗糙度和植被生物量变化的影响。我们的研究证实了所有测试场的体积近地表SM与雷达反向散射系数之间的良好一致性。测量的和估计的SM之间的比较证明了这里使用的反演模型的准确性,平均平均误差小于5%。最后,从获得的雷达图像中获得了高分辨率的土壤水分分布图。

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