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首页> 外文期刊>Remote Sensing of Environment: An Interdisciplinary Journal >Ensemble member generation for sequential data assimilation
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Ensemble member generation for sequential data assimilation

机译:集合成员生成以进行顺序数据同化

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Using an ensemble of model forecasts to describe forecast error covariance extends linear sequential data assimilation schemes to nonlinear applications. This approach forms the basis of the Ensemble Kalman Filter and derivative filters such as the Ensemble Square Root Filter. While ensemble data assimilation approaches are commonly reported in the scientific literature, clear guidelines for effective ensemble member generation remain scarce. As the efficiency of the filter is reliant on the accurate determination of forecast error covariance from the ensemble, this paper describes an approach for the systematic determination of random error. Forecast error results from three factors: errors in initial condition, forcing data and model equations. The method outlined in this paper explicitly acknowledges each of these sources in the generation of an ensemble. The initial condition perturbation approach presented optimally spans the dynamic range of the model states and allows an appropriate ensemble size to be determined. The forcing data perturbation approach treats forcing observations differently according to their nature. While error from model physics is not dealt with in detail, discussion of some commonly used approaches and their limitations is provided. The paper concludes with an example application for a synthetic coastal hydrodynamic experiment assimilating sea surface temperature (SST) data, which shows better prediction capability when contrasted with standard approaches in the literature. (C) 2007 Elsevier Inc. All rights reserved.
机译:使用模型预测的整体来描述预测误差的协方差将线性顺序数据同化方案扩展到非线性应用程序。此方法构成了“集合卡尔曼滤波器”和诸如“集合平方根滤波器”之类的派生滤波器的基础。尽管科学文献中普遍报告了集成数据同化方法,但是仍然缺乏有效的集成成员生成的清晰指南。由于滤波器的效率取决于整体的预测误差协方差的准确确定,因此本文介绍了一种系统确定随机误差的方法。预测误差来自三个因素:初始条件中的误差,强制数据和模型方程式。本文概述的方法在集成的生成中明确地承认了这些来源中的每一个。提出的初始条件摄动方法最佳地跨越了模型状态的动态范围,并允许确定适当的集合大小。强制数据扰动方法根据其性质对强制观测进行不同的处理。尽管没有详细处理模型物理学中的错误,但提供了一些常用方法及其局限性的讨论。本文以同化海面温度(SST)数据的合成海岸流体力学实验为例,并与文献中的标准方法相比,具有更好的预测能力。 (C)2007 Elsevier Inc.保留所有权利。

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