Strongly Coupled Data Assimilation Using Leading Averaged Coupled Covariance (LACC). Part III: Assimilation of Real World Reanalysis

Author:

Sun Jingzhe1,Liu Zhengyu2,Lu Feiyu3,Zhang Weimin4,Zhang Shaoqing5

Affiliation:

1. College of Computer, National University of Defense Technology, Changsha, and Open Studio for Ocean-Climate-Isotope Modeling, Qingdao National Laboratory for Marine Science and Technology, Qingdao, China, and Atmospheric Science Program, Department of Geography, The Ohio State University, Columbus, Ohio, and Nelson Institute Center for Climatic Research, and Department of Atmospheric and Oceanic

2. Atmospheric Science Program, Department of Geography, The Ohio State University, Columbus, Ohio

3. Atmospheric and Oceanic Sciences Program, Princeton University, and NOAA/Geophysical Fluid Dynamics Laboratory, Princeton, New Jersey

4. College of Meteorology and Oceanography, National University of Defense Technology, and Laboratory of Software Engineering for Complex Systems, Changsha, China

5. Physical Oceanography Laboratory, College of Oceanic and Atmospheric Sciences, and Institute for Advanced Ocean Study, Ocean University of China, and Function Laboratory for Ocean Dynamics and Climate, Qingdao National Laboratory for Marine Science and Technology, and International Laboratory for High-Resolution Earth System Prediction, Qingdao, China

Abstract

Abstract Recent studies proposed leading averaged coupled covariance (LACC) as an effective strongly coupled data assimilation (SCDA) method to improve the coupled state estimation over weakly coupled data assimilation (WCDA) in a coupled general circulation model (CGCM). This SCDA method, however, has been previously evaluated only in the perfect model scenario. Here, as a further step toward evaluating LACC for real world data assimilation, LACC is evaluated for the assimilation of reanalysis data in a CGCM. Several criteria are used to evaluate LACC against the benchmark WCDA. It is shown that despite significant model bias, LACC can improve the coupled state estimation over WCDA. Compared to WCDA, LACC increases the globally averaged anomaly correlation coefficients (ACCs) of sea surface temperature (SST) by 0.036 and atmosphere temperature at the bottom level (Ts) by 0.058. However, there also exist regions where WCDA outperforms LACC. Although the reduction in the anomaly root-mean-square error (RMSE) is not as consistently clear as the increase in ACC, LACC can largely correct the biased model climatology.

Funder

National Key R&D Program of China

Chinese MOST

National Natural Science Foundation of China

National Science Foundation

Publisher

American Meteorological Society

Subject

Atmospheric Science

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