How Sampling Errors in Covariance Estimates Cause Bias in the Kalman Gain and Impact Ensemble Data Assimilation

IF 2.8 3区 地球科学 Q3 METEOROLOGY & ATMOSPHERIC SCIENCES Monthly Weather Review Pub Date : 2023-06-09 DOI:10.1175/mwr-d-23-0029.1
D. Hodyss, M. Morzfeld
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Abstract

Localization is the key component to the successful application of ensemble data assimilation (DA) to high-dimensional problems in the geosciences. We study the impact of sampling error and its amelioration through localization using both analytical development and numerical experiments. Specifically, we show how sampling error in covariance estimates accumulates and spreads throughout the entire domain during the computation of the Kalman gain. This results in a bias, which is the dominant issue in unlocalized ensemble DA and, surprisingly, we find that it depends directly on the number of independent observations, but only indirectly on the state dimension. Our derivations and experiments further make it clear that an important aspect of localization is a significant reduction of bias in the Kalman gain, which in turn leads to an increased accuracy of ensemble DA. We illustrate our findings on a variety of simplified linear and nonlinear test problems, including a cycling ensemble Kalman filter applied to the Lorenz-96 model.
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协方差估计中的抽样误差如何导致卡尔曼增益偏差并影响集合数据同化
定位是集成数据同化技术成功应用于高维地球科学问题的关键。我们研究了采样误差的影响,并通过分析开发和数值实验的定位改进。具体来说,我们展示了在计算卡尔曼增益期间,协方差估计中的抽样误差是如何在整个域内累积和扩散的。这导致了偏差,这是非局域集合数据分析的主要问题,令人惊讶的是,我们发现它直接取决于独立观测的数量,而仅间接取决于状态维。我们的推导和实验进一步清楚地表明,定位的一个重要方面是卡尔曼增益中的偏差显著减少,这反过来又导致集合数据分析的准确性提高。我们在各种简化的线性和非线性测试问题上说明了我们的发现,包括应用于Lorenz-96模型的循环集合卡尔曼滤波器。
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来源期刊
Monthly Weather Review
Monthly Weather Review 地学-气象与大气科学
CiteScore
6.40
自引率
12.50%
发文量
186
审稿时长
3-6 weeks
期刊介绍: Monthly Weather Review (MWR) (ISSN: 0027-0644; eISSN: 1520-0493) publishes research relevant to the analysis and prediction of observed atmospheric circulations and physics, including technique development, data assimilation, model validation, and relevant case studies. This research includes numerical and data assimilation techniques that apply to the atmosphere and/or ocean environments. MWR also addresses phenomena having seasonal and subseasonal time scales.
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