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首页> 外文期刊>Journal of hydrologic engineering >ANN-Based Soil Moisture Retrieval over Bare and Vegetated Areas Using ERS-2 SAR Data
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ANN-Based Soil Moisture Retrieval over Bare and Vegetated Areas Using ERS-2 SAR Data

机译:基于ERS-2 SAR数据的基于ANN的裸露和植被地区土壤水分反演

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Active microwave remote sensing data (e.g., radar) can be used for estimation of soil moisture beneath the ground surfaces up to 0 to 5 cm depths. A number of analytical and empirical models are available that relate the synthetic aperture radar (SAR) data to the surface soil moisture. Each of these models has its own merits and demerits. In this paper, results obtained from a study on the application of artificial neural networks (ANN) for soil moisture retrieval from ERS-2 SAR data over bare and vegetated surfaces is presented. SAR images of three dates (i.e., July 28, 2003, March 29, 2004, and May 3, 2004) were acquired over a portion of the Solani river catchment in India. A feed forward back-propagation neural network was used for establishing the relationship between surface soil moisture and terrain as well as sensor variables. A maximum of seven input variables were considered for training the ANN. These are: Digital number (DN) or backscatter coefficient (σ deg) (as the case may be) of each pixel of SAR image selected individually, incidence angle of radar beam, land cover, surface roughness height, terrain height, leaf area index, and plant water content. Several ANN experiments were conducted and the coefficient of determination (R~2) and root-mean-square error (RMSE) were determined between the ANN derived soil moisture and the observed soil moisture through in-situ measurements taken concurrently with the satellite pass. It has been observed that it is the backscattering coefficient σ deg rather than DN, used as one of the inputs that produced high R2 (~0.9) and low RMSE. The results also indicate that only a few number of input variables may be sufficient to retrieve the soil moisture with high accuracies using the ANN. The leaf area index has been found to be as good as the single bulk variable representing the vegetation characteristics in the study area. In addition, the ANN technique has yielded more accurate results than the traditional statistical regression, indicating its usefulness for soil moisture estimation from microwave remote sensing data.
机译:有源微波遥感数据(例如雷达)可用于估计0至5厘米深度的地表下的土壤水分。可以使用许多分析和经验模型,这些模型将合成孔径雷达(SAR)数据与地表土壤湿度相关联。这些模型中的每一个都有其优点和缺点。本文介绍了从人工神经网络(ANN)在ERS-2 SAR数据在裸露和植被表面上获取土壤水分的应用中获得的结果。在印度索拉尼河流域的一部分上,采集了三个日期(即2003年7月28日,2004年3月29日和2004年5月3日)的SAR图像。前馈反向传播神经网络用于建立表层土壤水分与地形以及传感器变量之间的关系。最多可以考虑七个输入变量来训练ANN。它们是:单独选择的SAR图像每个像素的数字(DN)或后向散射系数(σdeg)(视情况而定),雷达波束的入射角,土地覆盖,表面粗糙度高度,地形高度,叶面积指数,以及植物的水分含量。进行了几次人工神经网络实验,并通过与卫星通行同时进行的原位测量,确定了人工神经网络得出的土壤水分与观测土壤水分之间的测定系数(R〜2)和均方根误差(RMSE)。已经观察到,它是反向散射系数σdeg而不是DN,用作产生高R2(〜0.9)和低RMSE的输入之一。结果还表明,只有少数几个输入变量可能足以使用ANN高精度地获取土壤水分。已经发现叶面积指数与代表研究区域的植被特征的单一体积变量一样好。此外,与传统的统计回归相比,人工神经网络技术产生的结果更准确,这表明该方法对于根据微波遥感数据估算土壤湿度很有用。

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