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A Monte Carlo based adaptive Kalman filtering framework for soil moisture data assimilation

机译:基于蒙特卡罗的自适应卡尔曼过滤框架,用于土壤水分数据同化

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The main sources of global soil moisture information are remote sensing observations and land surface model estimates. Data assimilation (DA) aims at optimally combining these data sources through statistical merging. To properly parameterize such merging, one needs to obtain accurate knowledge of model and observation uncertainties, which is the crux of a successful DA system. In this paper, we propose a new Monte Carlo based adaptive Kalman filtering framework (MadKF) that estimates model and observation uncertainties (Q and R) and updates soil moisture forecasts simultaneously. Spatially distributed uncertainties are estimated by applying triple collocation analysis (TCA) to Monte Carlo simulations of the model open-loop, the model analysis, and the observation time series at each grid cell. Error cross-covariances, which are inevitable between these time series, are diagnosed from their ensembles and used to iteratively correct biases they cause in Q and R estimates, and hence, in the Kalman filter gain. The proposed MadKF is tested in a synthetic environment and by assimilating real satellite soil moisture retrievals from the Advanced SCATterometer (ASCAT) into the Antecedent Precipitation Index (API) model forced with daily aggregated satellite precipitation. Synthetic experiments indicate a good convergence of Q and R estimates. Internal DA diagnostics, i.e., the innovation auto-correlation (IAC) and the variance of the normalized innovations, asymptotically converge to their desired values, which indicates that the filter is operating near its optimum and reliably estimates analysis uncertainty. Real-data experiments assimilating ASCAT observations into the API model further indicate that the MadKF is robust against observation error auto-correlations, which typically cause problems in conventional IAC-tuning based adaptive filtering approaches. A performance evaluation over 264 in situ sites within the contiguous United States shows that the MadKF leads to
机译:全球土壤水分信息的主要来源是遥感观测和陆地面模型估计。数据同化(DA)通过统计合并最佳地结合这些数据来源。为了适当地参数化这种合并,需要获得准确的模型和观察不确定性的知识,这是成功DA系统的关键。在本文中,我们提出了一种新的蒙特卡罗基于适应性的卡尔曼滤波框架(MADKF),其估计模型和观察不确定性(Q和R)并同时更新土壤水分预测。通过将三重裂缝分析(TCA)应用于模型开环,模型分析和观察时间序列的Monte Carlo模拟来估计空间分布的不确定性。错误的交叉协方差,这些时间序列之间是不可避免的,被诊断出从它们的集合中诊断出来,并且用于迭代地纠正它们在Q和R估计中导致的偏差,并且因此在卡尔曼滤波器增益中。拟议的MADKF在合成环境中进行测试,并通过从先进的散射仪(ASCAT)中的真实卫星土壤水分检索到迫使日常占卫星沉淀的前散沉指数(API)模型中。合成实验表明Q和R估计的良好收敛性。内部DA诊断,即创新自相关(IAC)和标准化创新的方差,渐近地会聚到其所需的值,这表明过滤器在其最佳和可靠地估计分析不确定性附近。将ASCAT观测的实验实验进入API模型进一步表明MADKF对观察误差自相关的稳健性,这通常在基于传统的基于IAC调整的自适应滤波方法中引起问题。在连续的美国中,264岁以上的绩效评估显示MADKF导致

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