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Observation operators for assimilation of satellite observations in fluvial inundation forecasting

机译:观测员对河流淹没预报中卫星观测的同化

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Images from satellite-based synthetic aperture radar (SAR) instruments contain large amounts of information about the position of floodwater during a river flood event. This observational information typically covers a large spatial area but is only relevant for a short time if water levels are changing rapidly. Data assimilation allows us to combine valuable SAR-derived observed information with continuous predictions from a computational hydrodynamic model and thus to produce a better forecast than using the model alone. In order to use observations in this way, a suitable observation operator is required. In this paper we show that different types of observation operators can produce very different corrections to predicted water levels; this impacts the quality of the forecast produced. We discuss the physical mechanisms by which different observation operators update modelled water levels and introduce a novel observation operator for inundation forecasting. The performance of the new operator is compared in synthetic experiments with that of two more conventional approaches. The conventional approaches both use observations of water levels derived from SAR to correct model predictions. Our new operator is instead designed to use backscatter values from SAR instruments as observations; such an approach has not been used before in an ensemble Kalman filtering framework. Direct use of backscatter observations opens up the possibility of using more information from each SAR image and could potentially speed up the time taken to produce observations needed to update model predictions. We compare the strengths and weaknesses of the three different approaches with reference to the physical mechanisms with which each of the observation operators allow data assimilation to update water levels in synthetic twin experiments in an idealised domain.
机译:来自卫星的合成孔径雷达(SAR)仪器的图像包含有关河流洪水事件期间洪水位置的大量信息。该观测信息通常覆盖较大的空间区域,但仅在水位快速变化的情况下才短时间使用。数据同化使我们能够将有价值的SAR派生的观测信息与来自计算流体力学模型的连续预测相结合,从而产生比单独使用模型更好的预测。为了以这种方式使用观察,需要合适的观察操作员。在本文中,我们表明,不同类型的观测算子可以对预测的水位产生非常不同的校正。这会影响所生成的预测的质量。我们讨论了不同观察员更新模拟水位的物理机制,并介绍了一种用于淹没预报的新型观察员。在合成实验中,将新操作员的性能与两种其他常规方法的性能进行了比较。常规方法都使用从SAR得出的水位观测值来校正模型预测。我们的新运算符被设计为使用SAR仪器的反向散射值作为观测值。集成卡尔曼滤波框架中从未使用过这种方法。直接使用反向散射观测结果为使用来自每个SAR图像的更多信息提供了可能性,并可能潜在地加快产生更新模型预测所需的观测结果所花费的时间。我们参照物理观测机制比较了三种不同方法的优缺点,每个观测算子都使用这些物理机制允许数据同化以更新理想域中的合成双生实验中的水位。

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