Preprints
https://doi.org/10.5194/egusphere-2025-3991
https://doi.org/10.5194/egusphere-2025-3991
19 Sep 2025
 | 19 Sep 2025
Status: this preprint is open for discussion and under review for The Cryosphere (TC).

Sea ice data assimilation in ORAS6

Philip Browne, Eric de Boisseson, Sarah Keeley, Charles Pelletier, and Hao Zuo

Abstract. Accurate weather and climate forecasting relies heavily on the precise modeling of sea ice, a critical component of the Earth's climate system. Sea ice influences global weather patterns, ocean circulation, and the exchange of heat and moisture between the atmosphere and oceans. Initialisation of the sea ice component of global coupled models relies on data assimilation techniques to incorporate information from observations to constrain the system.

This study focuses on the development of sea ice data assimilation for ECMWF’s latest Ocean Reanalysis System 6 (ORAS6) that includes a multicategory sea ice model. The research addresses the challenge of appropriately distributing sea ice concentration increments across various thickness categories in the model.

Here, we show that using a simple proportional increment splitting method improves the accuracy of sea ice concentration analyses compared to previous approaches. Our findings indicate that adding an additional sea ice-sea water temperature balance brings further performance benefits.

These results suggest that the choice of increment distribution strategy significantly impacts the accuracy of sea ice representation in reanalysis systems. The system presented here will form the basis of ECMWF's data assimilation system for numerical weather prediction, as well as the next generation coupled reanalyses.

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Philip Browne, Eric de Boisseson, Sarah Keeley, Charles Pelletier, and Hao Zuo

Status: open (until 31 Oct 2025)

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Philip Browne, Eric de Boisseson, Sarah Keeley, Charles Pelletier, and Hao Zuo
Philip Browne, Eric de Boisseson, Sarah Keeley, Charles Pelletier, and Hao Zuo
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Latest update: 19 Sep 2025
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Short summary
An initial estimate of sea ice conditions are required to start modern weather forecasting models. To get these we have to combine observations, typically from satellites, with previous estimates of the sea ice conditions. This paper talks about how we do this in the latest version of the model, where the sea ice state has to be specified for ice of different thicknesses. We describe the method that is used when we produce an estimate for every hour for the past 50 years.
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