Extending ensemble Kalman filter algorithms to assimilate observations with an unknown time offset

IF 1.7 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Elia Gorokhovsky, Jeffrey L. Anderson
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引用次数: 0

Abstract

Abstract. Data assimilation (DA), the statistical combination of computer models with measurements, is applied in a variety of scientific fields involving forecasting of dynamical systems, most prominently in atmospheric and ocean sciences. The existence of misreported or unknown observation times (time error) poses a unique and interesting problem for DA. Mapping observations to incorrect times causes bias in the prior state and affects assimilation. Algorithms that can improve the performance of ensemble Kalman filter DA in the presence of observing time error are described. Algorithms that can estimate the distribution of time error are also developed. These algorithms are then combined to produce extensions to ensemble Kalman filters that can both estimate and correct for observation time errors. A low-order dynamical system is used to evaluate the performance of these methods for a range of magnitudes of observation time error. The most successful algorithms must explicitly account for the nonlinearity in the evolution of the prediction model.
扩展集合卡尔曼滤波算法以同化具有未知时间偏移的观测
摘要数据同化(DA)是计算机模型与测量的统计组合,应用于各种科学领域,包括动力系统的预测,最突出的是大气科学和海洋科学。误报或未知观测时间(时间误差)的存在给DA带来了一个独特而有趣的问题。将观测结果映射到不正确的时间会导致先前状态的偏差,并影响同化。描述了在存在观测时间误差的情况下,可以提高组合卡尔曼滤波器DA性能的算法。还开发了可以估计时间误差分布的算法。然后将这些算法组合在一起,以产生组合卡尔曼滤波器的扩展,卡尔曼滤波器既可以估计观测时间误差,也可以校正观测时间误差。使用低阶动力系统来评估这些方法在观测时间误差范围内的性能。最成功的算法必须明确说明预测模型进化过程中的非线性。
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来源期刊
Nonlinear Processes in Geophysics
Nonlinear Processes in Geophysics 地学-地球化学与地球物理
CiteScore
4.00
自引率
0.00%
发文量
21
审稿时长
6-12 weeks
期刊介绍: Nonlinear Processes in Geophysics (NPG) is an international, inter-/trans-disciplinary, non-profit journal devoted to breaking the deadlocks often faced by standard approaches in Earth and space sciences. It therefore solicits disruptive and innovative concepts and methodologies, as well as original applications of these to address the ubiquitous complexity in geoscience systems, and in interacting social and biological systems. Such systems are nonlinear, with responses strongly non-proportional to perturbations, and show an associated extreme variability across scales.
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