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Toward High-Resolution Soil Moisture Monitoring by Combining Active-Passive Microwave and Optical Vegetation Remote Sensing Products with Land Surface Model

机译:结合有源无源微波和光学植被遥感产品与陆面模型的高分辨率土壤水分监测

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摘要

The assimilation of radiometer and synthetic aperture radar (SAR) data is a promising recent technique to downscale soil moisture products, yet it requires land surface parameters and meteorological forcing data at a high spatial resolution. In this study, we propose a new downscaling approach, named integrated passive and active downscaling (I-PAD), to achieve high spatial and temporal resolution soil moisture datasets over regions without detailed soil data. The Advanced Microwave Scanning Radiometer (AMSR-E) and Phased Array-type L-band SAR (PALSAR) data are combined through a dual-pass land data assimilation system to obtain soil moisture at 1 km resolution. In the first step, fine resolution model parameters are optimized based on fine resolution PALSAR soil moisture and moderate-resolution imaging spectroradiometer (MODIS) leaf area index data, and coarse resolution AMSR-E brightness temperature data. Then, the 25 km AMSR-E observations are assimilated into a land surface model at 1 km resolution with a simple but computationally low-cost algorithm that considers the spatial resolution difference. Precipitation data are used as the only inputs from ground measurements. The evaluations at the two lightly vegetated sites in Mongolia and the Little Washita basin show that the time series of soil moisture are improved at most of the observation by the assimilation scheme. The analyses reveal that I-PAD can capture overall spatial trends of soil moisture within the coarse resolution radiometer footprints, demonstrating the potential of the algorithm to be applied over data-sparse regions. The capability and limitation are discussed based on the simple optimization and assimilation schemes used in the algorithm.
机译:辐射计和合成孔径雷达(SAR)数据的同化是降低土壤水分含量的一种有前途的最新技术,但它需要具有高空间分辨率的地面参数和气象强迫数据。在这项研究中,我们提出了一种新的降尺度方法,称为无源和主动降尺度集成(I-PAD),以在没有详细土壤数据的区域上实现高时空分辨率的土壤水分数据集。先进的微波扫描辐射计(AMSR-E)和相控阵型L波段SAR(PALSAR)数据通过双程土地数据同化系统结合在一起,以1 km的分辨率获得土壤湿度。第一步,基于高分辨率PALSAR土壤湿度和中分辨率成像光谱仪(MODIS)叶面积指数数据以及粗糙分辨率AMSR-E亮度温度数据,优化高分辨率模型参数。然后,将25 km AMSR-E观测值同一个1 km分辨率的陆面模型同化,采用一种简单但计算成本低的算法,该算法考虑了空间分辨率差异。降水数据被用作地面测量的唯一输入。在蒙古和Little Washita盆地这两个轻度植被的地点进行的评估表明,大多数情况下通过同化方案可以改善土壤水分的时间序列。分析表明,I-PAD可以捕获粗分辨率辐射计足迹内土壤水分的总体空间趋势,证明了该算法在数据稀疏区域中的应用潜力。基于算法中使用的简单优化和同化方案,讨论了功能和限制。

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