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Extension of the Hapke bidirectional reflectance model to retrieve soil water content

机译:HAPKE双向反射模型的延伸,检测土壤含水量

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Soil moisture links the hydrologic cycle and the energy budget of land surfaces by regulating latent heat fluxes. An accurate assessment of the spatial and temporal variation of soil moisture is important to the study of surface biogeophysical processes. Although remote sensing has proven to be one of the most powerful tools for obtaining land surface parameters, no effective methodology yet exists for in situ soil moisture measurement based on a Bidirectional Reflectance Distribution Function (BRDF) model, such as the Hapke model. To retrieve and analyze soil moisture, this study applied the soil water parametric (SWAP)-Hapke model, which introduced the equivalent water thickness of soil, to ground multi-angular and hyperspectral observations coupled with, Powell-Ant Colony Algorithm methods. The inverted soil moisture data resulting from our method coincided with in situ measurements (R2 = 0.867, RMSE = 0.813) based on three selected bands (672 nm, 866 nm, 2209 nm). It proved that the extended Hapke model can be used to estimate soil moisture with high accuracy based on the field multi-angle and multispectral remote sensing data.
机译:土壤水分通过调节潜热通量来连接水文周期和陆地表面的能量预算。对土壤水分的空间和时间变异的准确评估对于表面生物果程的研究是重要的。虽然遥感已经被证明是获得土地表面参数最强大的工具之一,但没有基于双向反射率分布函数(BRDF)模型的原位土壤湿度测量的有效方法,例如HAPKE模型。本研究采取土壤水分,本研究应用了土壤水参数(交换) - 哈萨克模型,介绍了土壤等同水厚度,与地面多角度和高光谱观测,耦合,鲍威尔 - 蚁群算法方法。基于三个选定的带(672nm,866nm,2209nm),我们的方法由我们的方法与原位测量相一致(R2 = 0.867,RMSE = 0.813)掺入倒土。事实证明,扩展的HAPKE模型可用于估计基于场多角度和多光谱遥感数据的高精度的土壤湿度。

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