Abstract

Ensemble methods such as the Ensemble Kalman Filter (EnKF) are widely used for data assimilation in large-scale geophysical applications, as for example in numerical weather prediction. There is a growing interest for physical models with higher and higher resolution, which brings new challenges for data assimilation techniques because of the presence of non-linear and non-Gaussian features that are not adequately treated by the EnKF. We propose two new localized algorithms based on the Ensemble Kalman Particle Filter, a hybrid method combining the EnKF and the Particle Filter (PF) in a way that maintains scalability and sample diversity. Localization is a key element of the success of EnKF in practice, but it is much more challenging to apply to PFs. The algorithms that we introduce in the present paper provide a compromise between the EnKF and the PF while avoiding some of the problems of localization for pure PFs. Numerical experiments with a simplified model of cumulus convection based on a modified shallow water equation show that the proposed algorithms perform better than the local EnKF. In particular, the PF nature of the method allows to capture non-Gaussian characteristics of the estimated fields such as the location of wet and dry areas.

Highlights

  • In many large-scale environmental applications, estimating the evolution of a geophysical system, such as the atmosphere, is of utmost interest

  • We show the results as figures only as we believe that they are only indicative of some possible advantages but should not be taken too literally as the system under study is very artificial and the results can vary with different choice of parameters

  • We introduced two new localized algorithms based on the enkpf in order to address the problem of non-linear and non-Gaussian data assimilation, which is becoming increasingly relevant in large-scale applications with higher resolution

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Summary

Introduction

In many large-scale environmental applications, estimating the evolution of a geophysical system, such as the atmosphere, is of utmost interest. Data assimilation solves this problem iteratively by alternating between a forecasting step and an updating step. In the former, information about the dynamic of the system is incorporated, while in the latter, called analysis, partial and noisy observations are used to correct the current estimate. The analysis consists in deriving the posterior distribution of the current state of the system, combining the prior distribution and the new observations, which can be done with Bayes’ rule

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