Multi-level data assimilation for simplified ocean models

IF 1.7 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Florian Beiser, Håvard Heitlo Holm, Kjetil Olsen Lye, Jo Eidsvik
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引用次数: 0

Abstract

Abstract. Multi-level Monte Carlo methods have established as a tool in uncertainty quantification for decreasing the computational costs while maintaining the same statistical accuracy as in single-level Monte Carlo. Lately, there have also been theoretical efforts to use similar ideas to facilitate multi-level data assimilation. By applying a multi-level ensemble Kalman filter for assimilating sparse observations of ocean currents into a simplified ocean model based on the shallow-water equations, we study the practical challenges of applying these method to more complex problems. We present numerical results from a realistic test case where small-scale perturbations lead to chaotic behaviour, and in this context we conduct state estimation and drift trajectories forecasting using multi-level ensembles. This represents a new step on the path of making multi-level data assimilation feasible for real-world oceanographic applications.
简化海洋模型的多级数据同化
摘要多级蒙特卡洛方法已成为不确定性量化的一种工具,可在降低计算成本的同时保持与单级蒙特卡洛相同的统计精度。最近,理论界也在努力利用类似的思想来促进多级数据同化。通过应用多级集合卡尔曼滤波器将稀疏的洋流观测数据同化到基于浅水方程的简化海洋模型中,我们研究了将这些方法应用于更复杂问题的实际挑战。我们介绍了小尺度扰动导致混沌行为的现实测试案例的数值结果,在这种情况下,我们使用多级集合进行状态估计和漂移轨迹预测。这标志着多级数据同化在实际海洋学应用的可行性道路上迈出了新的一步。
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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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