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Merging Alternate Remotely-Sensed Soil Moisture Retrievals Using a Non-Static Model Combination Approach

机译:使用非静态模型组合方法合并替代的遥感土壤水分检索

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Soil moisture is an important variable in the coupled hydrologic and climate system. In recent years, microwave-based soil moisture products have been shown to be a viable alternative to in situ measurements. A popular way to measure the performance of soil moisture products is to calculate the temporal correlation coefficient (R) against in situ measurements or other appropriate reference datasets. In this study, an existing linear combination method improving R was modified to allow for a non-static or nonstationary model combination as the basis for improving remotely-sensed surface soil moisture. Previous research had noted that two soil moisture products retrieved using the Japan Aerospace Exploration Agency (JAXA) and Land Parameter Retrieval Model (LPRM) algorithms from the same Advanced Microwave Scanning Radiometer 2 (AMSR2) sensor are spatially complementary in terms of R against a suitable reference over a fixed period. Accordingly, a linear combination was proposed to maximize R using a set of spatially-varying, but temporally-fixed weights. Even though this approach showed promising results, there was room for further improvements, in particular using non-static or dynamic weights that take account of the time-varying nature of the combination algorithm being approximated. The dynamic weighting was achieved by using a moving window. A number of different window sizes was investigated. The optimal weighting factors were determined for the data lying within the moving window and then used to dynamically combine the two parent products. We show improved performance for the dynamically-combined product over the static linear combination. Generally, shorter time windows outperform the static approach, and a 60-day time window is suggested to be the optimum. Results were validated against in situ measurements collected from 124 stations over different continents. The mean R of the dynamically-combined products was found to be 0.57 and 0.62 for the cases using the European Centre for Medium-Range Weather Forecasts Reanalysis-Interim (ERA-Interim) and Modern-Era Retrospective Analysis for Research and Applications Land (MERRA-Land) reanalysis products as the reference, respectively, outperforming the statically-combined products (0.55 and 0.54).
机译:土壤水分是水文和气候系统耦合的重要变量。近年来,基于微波的土壤水分产品已被证明是现场测量的可行替代方案。衡量土壤水分产品性能的一种常用方法是针对现场测量值或其他适当的参考数据集计算时间相关系数(R)。在这项研究中,对改进R的现有线性组合方法进行了修改,以允许使用非静态或非平稳模型组合作为改进遥感表面土壤水分的基础。先前的研究已经指出,使用日本航空航天局(JAXA)和相同的先进微波扫描辐射计2(AMSR2)传感器的土地参数检索模型(LPRM)算法检索到的两种土壤水分产品,在R值与合适的R值方面在空间上互补固定期限内的参考。因此,提出了一种线性组合,以使用一组空间变化但时间固定的权重来最大化R。即使此方法显示出令人鼓舞的结果,也仍有进一步改进的空间,尤其是考虑到近似的组合算法随时间变化的性质而使用非静态或动态权重时。动态加权是通过使用移动窗口来实现的。研究了许多不同的窗口尺寸。确定位于移动窗口内的数据的最佳加权因子,然后将其动态组合两个父产品。与静态线性组合相比,我们显示了动态组合产品的改进性能。通常,较短的时间窗口优于静态方法,建议使用60天的时间窗口为最佳。针对从不同大陆的124个站点收集的现场测量结果验证了结果。对于欧洲中距离天气预报再分析临时研究中心(ERA-Interim)和研究和应用土地现代时代回顾分析(MERRA),发现动态组合产品的平均R分别为0.57和0.62 -Land)重新分析产品分别作为参考,胜过静态组合产品(0.55和0.54)。

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