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Simulation of Sentinel-2 data using Hyperspectral Data for Bare Surface Soil Moisture Estimation

机译:利用高光谱数据模拟Sentinel-2数据估算裸露地表土壤水分

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Soil moisture is one of the driving variables for precision irrigation management, drought assessment etc. Various approaches for measuring and monitoring soil moisture have been devised in the past, including laboratory techniques, point-based sensors, and remote sensing. However, the use of simulated optical data for bare surface soil moisture estimation is limited to date. The main objective of this study is the assessment of simulated Sentinel-2 data for bare surface soil moisture estimation. Hyperspectral soil moisture data provided by [1] in the spectral range of 450-950 nm over the test site in Germany has been utilized in this study. Hyperspectral images (50 x 50 pixels) were captured using the Cubert UHD 285 hyperspectral snapshot camera. The data available for public use consist of mean spectra of soil surface (average of 50 x 50 pixels) in 125 spectral bands. Simulation of 8 bands (B2-B8A) of Sentinel2 covering the same spectral range as that of hyperspectral camera was carried out using spectral response curve of Sentinel-2. Random Forest Regression based model was developed using all bands. Moreover, important features were selected based on a percent increase in mean squared error (%IncMSE). Selected bands include B2, B4, B5 and B7. Evaluation of models developed using all the 8 bands and selected 4 bands was carried out using the independant testing data based on Root Mean Sqaure Error (RMSE). We have obtained an RMSE of 1.01 and R2 value of 0.91 for a model with 8 bands. However, RMSE was reduced to 0.96 and R2 was increased to 0.94 in the case of selected 4 bands. In addition to this, validation of the model developed using the selected simulated bands was carried out using actual Sentinel-2 satellite observations on the TCS Demo Farm located in Pune, India. Estimated soil moisture was compared with the In-situ soil moisture observations available during Nov-Dec 2017. The difference between actual and estimated soil moisture was found to be between -2.10 to 3.18 %. The obtained outcomes depict that the results are significant and models developed on simulated Sentinel-2 data can be applied on Sentinel-2 satellite observations to estimate bare surface soil moisture.
机译:土壤水分是精确灌溉管理、干旱评估等的驱动变量之一。过去已经设计了各种测量和监测土壤水分的方法,包括实验室技术、基于点的传感器和遥感。然而,迄今为止,利用模拟光学数据估算裸露地表土壤湿度的方法还很有限。本研究的主要目的是评估模拟Sentinel-2数据,以估算裸露地表土壤水分。本研究使用了[1]在德国试验场地450-950 nm光谱范围内提供的高光谱土壤水分数据。使用Cubert UHD 285高光谱快照相机拍摄高光谱图像(50 x 50像素)。可供公众使用的数据包括125个光谱波段的土壤表面平均光谱(平均50 x 50像素)。利用Sentinel-2的光谱响应曲线,模拟了Sentinel-2的8个波段(B2-B8A),覆盖与高光谱相机相同的光谱范围。随机森林回归模型是使用所有波段建立的。此外,重要特征的选择基于均方误差的百分比增加(%IncMSE)。选定的波段包括B2、B4、B5和B7。使用基于均方根误差(RMSE)的独立测试数据,对使用所有8个波段和选定的4个波段开发的模型进行评估。我们获得了1.01的RMSE和R

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