the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Novel Arctic sea ice data assimilation combining ensemble Kalman filter with a Lagrangian sea ice model
Abstract. Advanced data assimilation (DA) methods, widely used in geophysical and climate studies to merge observations with numerical models, can improve the state estimates and consequent forecasts. We interface the deterministic Ensemble Kalman filter (DEnKF) to the Lagrangian sea ice model, neXtSIM. The ensemble is generated by perturbing the atmospheric and oceanic forcing throughout the simulations and randomly initialized ice cohesion. Our ensemble-DA system assimilates sea ice concentration (SIC) from the Ocean and Sea Ice Satellite Application Facility (OSI-SAF) and sea ice thickness (SIT) from the merged CryoSat-2 and SMOS datasets (CS2SMOS). Because neXtSIM is computationally solved on a time-dependent evolving mesh, it is a challenging application for ensemble DA. As a solution, we perform the DEnKF analysis on a fixed reference mesh, where model variables are interpolated before the DA and then back to each member's mesh after the DA. We evaluate the impact of assimilating different types of sea-ice observations on the model's forecast skills of the Arctic sea ice by comparing against satellite observations and a free-run ensemble in an Arctic winter period, 2019–2020. Significant improvements in modeled SIT indicate the importance of assimilating weekly CS2SMOS SIT, while the improvement of SIC and ice extent are moderate but benefit from daily ingestion of the OSI-SAF SIC. In contrast, the bivariate improvements between SIC and SIT are unobvious. Our ensemble-DA system based on the stand-alone sea ice model is computationally efficient and demonstrates comparable skills to operational forecasting models that use DA.
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Notice on discussion status
The requested preprint has a corresponding peer-reviewed final revised paper. You are encouraged to refer to the final revised version.
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Preprint
(20643 KB)
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The requested preprint has a corresponding peer-reviewed final revised paper. You are encouraged to refer to the final revised version.
- Preprint
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- Final revised paper
Journal article(s) based on this preprint
Interactive discussion
Status: closed
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RC1: 'Comment on egusphere-2022-627', Anonymous Referee #1, 16 Oct 2022
The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2022/egusphere-2022-627/egusphere-2022-627-RC1-supplement.pdf
- AC1: 'Reply on RC1', Sukun Cheng, 27 Jan 2023
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RC2: 'Comment on egusphere-2022-627', Francois Massonnet, 21 Oct 2022
The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2022/egusphere-2022-627/egusphere-2022-627-RC2-supplement.pdf
- AC2: 'Reply on RC2', Sukun Cheng, 27 Jan 2023
Interactive discussion
Status: closed
-
RC1: 'Comment on egusphere-2022-627', Anonymous Referee #1, 16 Oct 2022
The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2022/egusphere-2022-627/egusphere-2022-627-RC1-supplement.pdf
- AC1: 'Reply on RC1', Sukun Cheng, 27 Jan 2023
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RC2: 'Comment on egusphere-2022-627', Francois Massonnet, 21 Oct 2022
The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2022/egusphere-2022-627/egusphere-2022-627-RC2-supplement.pdf
- AC2: 'Reply on RC2', Sukun Cheng, 27 Jan 2023
Peer review completion
Journal article(s) based on this preprint
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Yumeng Chen
Ali Aydoğdu
Laurent Bertino
Alberto Carrassi
Pierre Rampal
Christopher K. R. T. Jones
The requested preprint has a corresponding peer-reviewed final revised paper. You are encouraged to refer to the final revised version.
- Preprint
(20643 KB) - Metadata XML