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A parameterized surface reflectivity model for L-band radiometer

机译:L波段辐射计的参数化表面反射型模型

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Soil moisture is an important parameter for hydrological and climatic investigations. Future satellite missions with L-band passive microwave radiometers will significantly increase the capability of monitoring Earth's soil moisture globally. Understanding the effects of surface roughness on microwave emission and developing quantitative bare surface soil moisture retrieval algorithms is one of the essential components in many applications of geophysical properties in the complex earth terrain by microwave remote sensing. In this study, we explore the use of the Integral Equation Model (IEM) for modeling microwave emission. This model was validated using a three-dimensional Monte Carlo model. The results indicate that the IEM model can be used to simulate the surface emission quite well for a wide range of surface roughness conditions with high confidence. Several important characteristics of the effects of surface roughness on radiometer emission signals at L-band 1.4 GHz that have not been adequately addressed in the current semi-empirical surface effective reflectivity models are demonstrated by using IEM simulated data. Using an IEM simulated database for a wide range of surface soil moisture and roughness properties, we developed a parameterized surface effective reflectivity model with three typically used correlation functions.
机译:土壤水分是水文和气候调查的重要参数。具有L波段无源微波辐射仪的未来卫星任务将大大提高全球监测地球土壤水分的能力。了解表面粗糙度对微波排放和开发定量裸露表面土壤水分检索算法的影响是通过微波遥感通过微波遥感在复杂地球地形中的地球物理性质的许多基本组成部分之一。在这项研究中,我们探讨了整体方程模型(IEM)来建模微波发射。使用三维蒙特卡罗模型进行验证该模型。结果表明,IEM模型可用于模拟表面排放,对于具有高置信度的广泛的表面粗糙度条件。通过使用IEM模拟数据证明了在电流半经验表面有效反射率模型中未充分寻址的L波段1.4GHz的表面粗糙度对辐射计发射信号的几个重要特征。使用IEM模拟数据库进行广泛的表面土壤水分和粗糙度,我们开发了一种参数化表面有效的反射率模型,具有三种通常使用的相关函数。

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