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Correction of real-time satellite precipitation with satellite soil moisture observations

机译:利用卫星土壤湿度观测值校正实时卫星降水

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Rainfall and soil moisture are two key elements in modeling the interactionsbetween the land surface and the atmosphere. Accurate and high-resolutionreal-time precipitation is crucial for monitoring and predicting the onset offloods, and allows for alert and warning before the impact becomes adisaster. Assimilation of remote sensing data into a flood-forecasting modelhas the potential to improve monitoring accuracy. Space-borne microwaveobservations are especially interesting because of their sensitivity tosurface soil moisture and its change. In this study, we assimilate satellitesoil moisture retrievals using the Variable Infiltration Capacity (VIC) landsurface model, and a dynamic assimilation technique, a particle filter, toadjust the Tropical Rainfall Measuring Mission Multi-satellite PrecipitationAnalysis (TMPA) real-time precipitation estimates. We compare updatedprecipitation with real-time precipitation before and after adjustment andwith NLDAS gauge-radar observations. Results show that satellite soilmoisture retrievals provide additional information by correcting errors inrainfall bias. The assimilation is most effective in the correction of mediumrainfall under dry to normal surface conditions, while limitedegativeimprovement is seen over wet/saturated surfaces. On the other hand,high-frequency noises in satellite soil moisture impact the assimilation byincreasing rainfall frequency. The noise causes larger uncertainty in thefalse-alarmed rainfall over wet regions. A threshold of 2 mm day?1soil moisture change is identified and applied to the assimilation, whichmasked out most of the noise.
机译:降雨和土壤水分是模拟陆地表面与大气之间相互作用的两个关键要素。准确,高分辨率的实时降水对于监测和预测暴发洪水至关重要,并且可以在灾害造成灾难之前发出警报和警告。将遥感数据同化为洪水预报模型有可能提高监测精度。太空微波观测特别有趣,因为它们对地表土壤水分及其变化敏感。在这项研究中,我们使用可变渗透能力(VIC)地表模型,动态同化技术,颗粒过滤器来吸收卫星土壤水分反演,以调整热带降雨测量任务多卫星降水分析(TMPA)的实时降水估算。我们将更新前后的降水量与调整前后的实时降水量以及NLDAS液位雷达观测值进行了比较。结果表明,卫星土壤水分反演通过纠正降雨偏向误差提供了更多信息。在干燥到正常表面条件下,同化作用最有效地校正中等降雨,而在潮湿/饱和表面上则观察到有限/负面的改善。另一方面,卫星土壤水分中的高频噪声会通过增加降雨频率来影响同化。噪声在湿润地区的虚假降雨中引起更大的不确定性。可以确定2 mm day ?1 土壤水分变化的阈值并将其应用于同化过程,从而掩盖了大部分噪声。

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