Assimilating Atmosphere Reanalysis in Coupled Data Assimilation
This paper tests the idea of substituting the atmospheric observations with atmospheric reanalysis when setting up a coupled data assimilation system.The paper focuses on the quantification of the effects on the oceanic analysis resulted from this substitution and designs four different assimilation...
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          | Published in | Acta meteorologica Sinica Vol. 30; no. 4; pp. 572 - 583 | 
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| Main Author | |
| Format | Journal Article | 
| Language | English | 
| Published | 
        Beijing
          The Chinese Meteorological Society
    
        01.06.2016
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| Subjects | |
| Online Access | Get full text | 
| ISSN | 2095-6037 0894-0525 2198-0934 2191-4788  | 
| DOI | 10.1007/s13351-016-6014-1 | 
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| Summary: | This paper tests the idea of substituting the atmospheric observations with atmospheric reanalysis when setting up a coupled data assimilation system.The paper focuses on the quantification of the effects on the oceanic analysis resulted from this substitution and designs four different assimilation schemes for such a substitution.A coupled Lorenz96 system is constructed and an ensemble Kalman filter is adopted.The atmospheric reanalysis and oceanic observations are assimilated into the system and the analysis quality is compared to a benchmark experiment where both atmospheric and oceanic observations are assimilated.Four schemes are designed for assimilating the reanalysis and they differ in the generation of the perturbed observation ensemble and the representation of the error covariance matrix.The results show that when the reanalysis is assimilated directly as independent observations,the root-mean-square error increase of oceanic analysis relative to the benchmark is less than 16%in the perfect model framework;in the biased model case,the increase is less than 22%.This result is robust with sufficient ensemble size and reasonable atmospheric observation quality(e.g.,frequency,noisiness,and density).If the observation is overly noisy,infrequent,sparse,or the ensemble size is insufficiently small,the analysis deterioration caused by the substitution is less severe since the analysis quality of the benchmark also deteriorates significantly due to worse observations and undersampling.The results from different assimilation schemes highlight the importance of two factors:accurate representation of the error covariance of the reanalysis and the temporal coherence along each ensemble member,which are crucial for the analysis quality of the substitution experiment. | 
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| Bibliography: | 11-2277/P This paper tests the idea of substituting the atmospheric observations with atmospheric reanalysis when setting up a coupled data assimilation system.The paper focuses on the quantification of the effects on the oceanic analysis resulted from this substitution and designs four different assimilation schemes for such a substitution.A coupled Lorenz96 system is constructed and an ensemble Kalman filter is adopted.The atmospheric reanalysis and oceanic observations are assimilated into the system and the analysis quality is compared to a benchmark experiment where both atmospheric and oceanic observations are assimilated.Four schemes are designed for assimilating the reanalysis and they differ in the generation of the perturbed observation ensemble and the representation of the error covariance matrix.The results show that when the reanalysis is assimilated directly as independent observations,the root-mean-square error increase of oceanic analysis relative to the benchmark is less than 16%in the perfect model framework;in the biased model case,the increase is less than 22%.This result is robust with sufficient ensemble size and reasonable atmospheric observation quality(e.g.,frequency,noisiness,and density).If the observation is overly noisy,infrequent,sparse,or the ensemble size is insufficiently small,the analysis deterioration caused by the substitution is less severe since the analysis quality of the benchmark also deteriorates significantly due to worse observations and undersampling.The results from different assimilation schemes highlight the importance of two factors:accurate representation of the error covariance of the reanalysis and the temporal coherence along each ensemble member,which are crucial for the analysis quality of the substitution experiment. LIU Huaran1,2, LU Feiyu2, LIU Zhengyu2 , LIU Yun3 ,ZHANG Shaoqing4 ( 1 Department of Atmospheric Sciences, Nanjing University of Information Science & Technology, Nanjing 210044, China; 2 Department of Atmospheric and Oceanic Sciences, University of Wisconsin-Madison, Madison 53706, USA ; 3 Department of Atmospheric and Oceanic Science, University of Maryland, College Park 20742, USA ; 4 Geophysical Fluid Dynamics Laboratory, NOAA, Princeton 08542, USA) data assimilation reanalysis data ensemble Kalman filter ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23  | 
| ISSN: | 2095-6037 0894-0525 2198-0934 2191-4788  | 
| DOI: | 10.1007/s13351-016-6014-1 |