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首页> 外文期刊>Journal of hydrologic engineering >Calibration of Roughness Parameters Using Rainfall-Runoff Water Balance for Satellite Soil Moisture Retrieval
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Calibration of Roughness Parameters Using Rainfall-Runoff Water Balance for Satellite Soil Moisture Retrieval

机译:利用降雨径流水量平衡法反演粗糙度参数的卫星土壤水分反演

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摘要

Soil moisture is an important component in hydrologic and meteorologic processes. Remote sensing devices, such as satellite radiometers, are useful tools to obtain soil moisture information over a large region. However, effective "ground truth" calibration data for satellite sensors are lacking. This paper presents a new approach on the basis of rainfall and river runoff hydrologic data to estimate satellite-based soil moisture. The catchment water storage change from the rainfall and river runoff has a strong link with the soil moisture information and the parameterization of the surface roughness parameters h and Q. The proposed methodology is tested at the Brae catchment in southwest England. Two years of satellite data are used for calibrating and retrieving surface soil moisture, and 1 year of data is used for validation. This study indicates that the estimated daily soil moisture from satellite correlates well with the flow observations after applying the new calibration method, and good agreement (R~2 = 0.74) is shown between the water storage change and the soil moisture change. The results indicate that this new scheme could be a useful approach in improving the satellite soil moisture retrieval for hydrologic applications.
机译:土壤水分是水文和气象过程中的重要组成部分。诸如卫星辐射计之类的遥感设备是获得大范围土壤湿度信息的有用工具。但是,缺少用于卫星传感器的有效“地面真相”校准数据。本文提出了一种基于降雨和河流径流水文数据估算卫星土壤湿度的新方法。由于降雨和河流径流引起的汇水蓄水量变化与土壤水分信息以及表面粗糙度参数h和Q的参数化有很强的联系。所提出的方法在英格兰西南部的Brae流域进行了测试。两年的卫星数据用于校准和获取地表土壤水分,一年的数据用于验证。该研究表明,采用新的标定方法后,卫星估算的每日土壤含水量与流量观测值具有很好的相关性,并且表明储水量变化与土壤含水量变化之间具有良好的一致性(R〜2 = 0.74)。结果表明,该新方案可能是改善卫星水文应用中土壤水分反演的有用方法。

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