Monitoring of surface soil moisture based on optical and radar data over agricultural fields

S. Bousbih, M. Zribi, B. Mougenot, P. Fanise, Z. Lili-Chabaane, N. Baghdadi
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引用次数: 5

Abstract

The surface soil moisture is a key parameter that describes and conditions the exchange between the surface and the atmosphere via the energy balance. It is important because of its impact on the evapotranspiration and irrigation management. The most widespread approach is based on the synergy between radar and optical data to retrieve soil moisture. The aim is to study the potential of Sentinel sensors (Sentinel-1 (S-1) and Sentinel-2 (S-2)) for the retrieving of the soil moisture at regional scale. First, an analysis between the radar (S-1) and the measured data (soil moisture, soil roughness and Leaf Area Index (LAI)) is established over bare soils and cereal fields in the Kairouan plain, Tunisia. The results of the sensitivity analysis show that the radar signal in VV (vertical) polarization and soil and vegetation parameters are strongly correlated than in VH cross-polarization. The Water Cloud Model was calibrated using the NDVI (Normalized Difference Vegetation Index) retrieved from Sentinel-2 images. Then, an inversion approach of this model is developed for the mapping of soil moisture at high spatial resolution.
基于光学和雷达数据的农田表层土壤水分监测
地表土壤湿度是通过能量平衡来描述和调节地表与大气之间交换的关键参数。它的重要性在于它对蒸散和灌溉管理的影响。最广泛的方法是基于雷达和光学数据之间的协同作用来检索土壤湿度。目的是研究Sentinel-1 (S-1)和Sentinel-2 (S-2)传感器在区域尺度土壤水分反演中的应用潜力。首先,将雷达(S-1)与实测数据(土壤湿度、土壤粗糙度和叶面积指数(LAI))在突尼斯凯鲁万平原的裸地和谷地上进行了分析。灵敏度分析结果表明,垂直极化雷达信号与土壤、植被参数的相关性强于交叉极化雷达信号。水云模型使用从Sentinel-2图像中检索的归一化植被指数(NDVI)进行校准。在此基础上,提出了基于该模型的高空间分辨率土壤湿度反演方法。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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