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Data assimilation for improving soil moisture estimation at hillslope scales: experiments with synthetic SMAP radar data

机译:用于改善Hillslope尺度土壤水分估计的数据同化:合成Smap Radar数据的实验

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In a series of synthetic experiments we test the hypothesis that data assimilation algorithms can be employed to improve soil moisture estimation at spatial scales of hillslopes (e.g. 10°-102 m). We use the Ensemble Kalman Filter (EnKF) to update an ensemble of hillslope-scale soil moisture fields simulated by a physically-based ecohydrology model with synthetic SMAP radar observations. For sparse vegetation, assimilation of the synthetic observations substantially reduces estimation error in near-surface soil moisture (e.g. top 5 cm), relative to the synthetic true soil moisture conditions. Key components of our data assimilation system are: (1) explicit representation of the impact of hillslope-scale topography on microwave observation, and (2) a Latin Hypercube-based soil parameter generator that preserves the correlation between soil properties and improves the reproducibility of soil moisture ensemble statistics.
机译:在一系列合成实验中,我们测试了数据同化算法的假设,可以采用数据同化算法来改善山坡空间尺度的土壤水分估计(例如10°-102米)。我们使用合奏卡尔曼滤波器(ENKF)来更新通过基于物理的生态水解模型模拟的山坡级土壤水分田的集合,具有合成的微量雷达观测。对于稀疏植被,合成观察的同化显着降低了近表面土壤水分(例如前5厘米)的估计误差,相对于合成的真土水分条件。我们的数据同化系统的关键组成部分是:(1)明确表示山坡级地形对微波观察的影响,(2)基于拉丁超立体的土壤参数发生器,可以保留土壤性质之间的相关性并提高了重复性土壤湿度合奏统计。

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