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Radar backscatter inversion techniques for estimation of surface soil moisture: EFEDA-Spain and HAPEX-Sahel case studies

机译:估计土壤表层水分的雷达反向散射反演技术:EFEDA-西班牙和HAPEX-Sahel案例研究

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摘要

Soil moisture is considered to be the link between the water and energy balance at the land surface. The extraction of information on soil moisture from remotely sensed data, especially from microwave instruments, has always received a lot of attention. Most methods that are used to extract this information are empirical in nature. In this paper, a semiempirical model from Y. Oh et al., (1992) and a numerical inversion of the Integral Equation Method (IEM) model, introduced as "INVIEM," are applied to retrieve soil moisture over bare soil surfaces from active microwave data. The two models are compared using data from the Jet Propulsion Laboratory (JPL) air synthetic aperture radar (AirSAR) taken during the EFEDA-Spain'91 experiment and ERS-1 data from the HAPEX-Sahel'92 experiment. The comparison is performed within a general framework to estimate soil moisture from radar data, describing all necessary steps. The range of soil moisture values estimated by the INVIEM model, using the AirSAR and ERS-1 data, is in agreement with the soil moisture variation found in the field.
机译:土壤水分被认为是陆地表面水与能量平衡之间的联系。从遥感数据中,特别是从微波仪器中提取土壤水分信息,一直备受关注。本质上,用于提取此信息的大多数方法都是经验性的。在本文中,Y。Oh等人(1992年)的半经验模型和积分方程方法(IEM)模型的数值反演(称为“ INVIEM”)被应用于从活性土壤中获取裸露土壤表面的土壤水分微波数据。使用在EFEDA-Spain'91实验期间获得的喷气推进实验室(JPL)空气合成孔径雷达(AirSAR)数据和从HAPEX-Sahel'92实验获得的ERS-1数据对这两个模型进行了比较。比较是在一个通用框架内进行的,以根据雷达数据估算土壤湿度,并描述所有必要步骤。利用AirSAR和ERS-1数据,由INVIEM模型估算的土壤水分值范围与现场发现的土壤水分变化一致。

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