Statistical Analysis of Physical Characteristics Calculated by NEMO Model After Data Assimilation

The main goal of this study is to develop a method for finding the joint probability distribution of the state of the characteristics of the NEMO (Nucleus for European Modeling of the Ocean) ocean dynamics model with data assimilation using the Generalized Kalman filter (GKF) method developed earlier by the authors. The method for finding the joint distribution is based on the Karhunen–Loeve decomposition of the covariance function of the joint characteristics of the ocean. Numerical calculations of the dynamics of ocean currents, surface and subsurface ocean temperatures, and water salinity were carried out, both with and without assimilation of observational data from the Argo project drifters. The joint probability distributions of temperature and salinity at individual points in the world ocean at different depths were obtained and analyzed. The Atlantic Meridional Overturning Circulation (AMOC) system was also simulated using the NEMO model with and without data assimilation, and these results were compared to each other and analyzed.

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Publication Details

Journal
Mathematics
Published
2025-03-13
DOI
https://doi.org/10.3390/math13060948
Primary Topic
Meteorological Phenomena and Simulations
Type
article
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article

Statistical Analysis of Physical Characteristics Calculated by NEMO Model After Data Assimilation

А. А. Кулешов, Ilya Smirnov, Konstantin Belyaev
Mathematics
Meteorological Phenomena and Simulations
article

Statistical Analysis of Physical Characteristics Calculated by NEMO Model After Data Assimilation

А. А. Кулешов, Ilya Smirnov, Konstantin Belyaev
article en

Abstract

The main goal of this study is to develop a method for finding the joint probability distribution of the state of the characteristics of the NEMO (Nucleus for European Modeling of the Ocean) ocean dynamics model with data assimilation using the Generalized Kalman filter (GKF) method developed earlier by the authors. The method for finding the joint distribution is based on the Karhunen–Loeve decomposition of the covariance function of the joint characteristics of the ocean. Numerical calculations of the dynamics of ocean currents, surface and subsurface ocean temperatures, and water salinity were carried out, both with and without assimilation of observational data from the Argo project drifters. The joint probability distributions of temperature and salinity at individual points in the world ocean at different depths were obtained and analyzed. The Atlantic Meridional Overturning Circulation (AMOC) system was also simulated using the NEMO model with and without data assimilation, and these results were compared to each other and analyzed.

MathematicsVol. 13(6)
Lomonosov Moscow State University (RU), Institute of Oceanology. PP Shirshov Russian Academy of Sciences (RU), Keldysh Institute of Applied Mathematics (RU)
Openalex Percentile: Top 96%
Meteorological Phenomena and Simulations
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