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Comparing soil moisture anomalies from multiple independent sources over different regions across the globe

机译:将土壤水分异常从全球不同地区的不同地区进行比较

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Agricultural drought events can affect large regions across the world, implying the need for a suitable global tool for an accurate monitoring of this phenomenon. Soil moisture anomalies are considered a good metric to capture the occurrence of agricultural drought events, and they have become an important component of several operational drought monitoring systems. In the framework of the JRC Global Drought Observatory (GDO, http://edo.jrc.ec.europa. eu/gdo/), the suitability of three datasets as possible representations of root zone soil moisture anomalies has been evaluated: (1) the soil moisture from the Lisflood distributed hydrological model (namely LIS), (2) the remotely sensed Land Surface Temperature data from the MODIS satellite (namely LST), and (3) the ESA Climate Change Initiative combined passive/active microwave skin soil moisture dataset (namely CCI). Due to the independency of these three datasets, the triple collocation (TC) technique has been applied, aiming at quantifying the likely error associated with each dataset in comparison to the unknown true status of the system. TC analysis was performed on five macro-regions (namely North America, Europe, India, southern Africa and Australia) detected as suitable for the experiment, providing insight into the mutual relationship between these datasets as well as an assessment of the accuracy of each method. Even if no definitive statement on the spatial distribution of errors can be provided, a clear outcome of the TC analysis is the good performance of the remote sensing datasets, especially CCI, over dry regions such as Australia and southern Africa, whereas the outputs of LIS seem to be more reliable over areas that are well monitored through meteorological ground station networks, such as North America and Europe. In a global drought monitoring system, the results of the error analysis are used to design a weighted-average ensemble system that exploits the advantages of each dataset.
机译:农业干旱事件可能会影响全球大型地区,这意味着需要适合适当的全球工具,以准确监测这种现象。土壤水分异常被认为是捕获农业干旱事件的发生的良好指标,它们已成为若干操作干旱监测系统的重要组成部分。在JRC全球干旱天文台的框架中(GDO,http://edo.jrc.ec.europa。欧盟/ gdo /),评估了三个数据集的适用性,作为根区土壤水分异常的可能表示:(1 )从螺丝翅片分布水文模型(即LIS)的土壤水分,(2)来自MODIS卫星的远程感测的陆地表面温度数据(即LST),以及(3)ESA气候变化倡议联合被动/活性微波皮肤土壤湿度数据集(即CCI)。由于这三个数据集的独立性,已经应用了三重搭配(TC)技术,而是定量与每个数据集相关联的可能的错误与系统的未知真实状态相比。在五个宏观区域(即北美,欧洲,印度,南非和澳大利亚)进行TC分析检测适用于实验,提供对这些数据集之间的相互关系的洞察,以及对每种方法的准确性的评估。即使可以提供关于错误的空间分布的明确陈述,TC分析的明确结果是遥感数据集,特别是CCI,尤其是CCI,澳大利亚和南部非洲的干旱地区,而LIS的产出似乎在通过气象地面网络(如北美和欧洲)监控的区域更可靠。在全球干旱监测系统中,错误分析的结果用于设计加权平均集合系统,该系统利用每个数据集的优势。

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