Articles | Volume 19, issue 16
https://doi.org/10.5194/gmd-19-8003-2026
https://doi.org/10.5194/gmd-19-8003-2026
Model evaluation paper
 | 
27 Aug 2026
Model evaluation paper |  | 27 Aug 2026

Improving simulation of Earth system variability through weakly coupled ocean data assimilation in E3SM

Pengfei Shi, L. Ruby Leung, Zhaoxia Pu, Samson Hagos, and Karthik Balaguru

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Cited articles

Adler, R. F., Huffman, G. J., Chang, A., Ferraro, R., Xie, P. P., Janowiak, J., Rudolf, B., Schneider, U., Curtis, S., Bolvin, D., Gruber, A., Susskind, J., Arkin, P., and Nelkin, E.: The version-2 Global Precipitation Climatology Project (GPCP) monthly precipitation analysis (1979–present), J. Hydrometeorol., 4, 1147–1167, https://doi.org/10.1175/1525-7541(2003)004<1147:TVGPCP>2.0.CO;2, 2003. 
Boer, G. J., Smith, D. M., Cassou, C., Doblas-Reyes, F., Danabasoglu, G., Kirtman, B., Kushnir, Y., Kimoto, M., Meehl, G. A., Msadek, R., Mueller, W. A., Taylor, K. E., Zwiers, F., Rixen, M., Ruprich-Robert, Y., and Eade, R.: The Decadal Climate Prediction Project (DCPP) contribution to CMIP6, Geosci. Model Dev., 9, 3751–3777, https://doi.org/10.5194/gmd-9-3751-2016, 2016. 
Browne, P. A., De Rosnay, P., Zuo, H., Bennett, A., and Dawson, A.: Weakly coupled ocean–atmosphere data assimilation in the ECMWF NWP system, Remote Sensing, 11, 234, https://doi.org/10.3390/rs11030234, 2019. 
Carton, J. A. and Giese, B. S.: A reanalysis of ocean climate using Simple Ocean Data Assimilation (SODA), Mon. Weather Rev., 136, 2999–3017, https://doi.org/10.1175/2007MWR1978.1, 2008. 
Chiang, J. C. H. and Sobel, A. H.: Tropical tropospheric temperature variations caused by ENSO and their influence on the remote tropical climate, J. Climate, 15, 2616–2631, https://doi.org/10.1175/1520-0442(2002)015<2616:TTTVCB>2.0.CO;2, 2002. 
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Short summary
Reliable climate prediction requires accurate ocean initial conditions. We developed an ocean data assimilation system that incorporates ocean temperature and salinity reanalysis into a climate model. This system improves simulations of climate variability from years to decades and of U.S. winter temperature and precipitation. Additional hindcasts show no appreciable initialization shock and reproduce physically coherent ENSO teleconnection patterns, supporting more reliable climate predictions.
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