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https://doi.org/10.5194/egusphere-2025-104
https://doi.org/10.5194/egusphere-2025-104
11 Feb 2025
 | 11 Feb 2025

Enhancing sea ice knowledge through assimilation of sea ice thickness from ENVISAT and CS2SMOS

Nicholas Williams, Yiguo Wang, and François Counillon

Abstract. Arctic sea ice extent has declined significantly over the past two decades, opening up the Arctic to shipping and resource extraction while also impacting wildlife and local communities. This has led to an increasing need for skillful sea ice predictions. We focus on furthering the understanding of the role that sea ice thickness plays in the skilfulness of seasonal Arctic sea ice predictions. We look at how observations of sea ice thickness can improve both sea ice reanalyses and predictions. We use the Norwegian Climate Prediction Model (NorCPM), which has previously assimilated ocean and sea ice concentration observations. We additionally assimilate two sea ice thickness products: CS2SMOS, and, for the first time in any study, ENVISAT. This allows us to produce a 2-decade reanalysis with sea ice thickness assimilation focusing on the Arctic Ocean. This reanalysis is then used to initialise and generate a series of year-long seasonal hindcasts for each season of the reanalysis. The reanalysis and hindcasts are compared to observations and other reanalyses to assess the impact of sea ice thickness observations. Assimilation of sea ice thickness data strongly improves the representation of sea ice thickness and volume, primarily in the central Arctic as well as the ice edge location. Although ENVISAT observations have greater uncertainties, the dataset still provides a useful impact on the model. For prediction, sea ice thickness initialisation reduces the model biases of thickness throughout the year as well as errors in the detrended anomalies. Ice thickness bias correction results in improvements in the representation of the ice edge location, i.e., the timing and extent of the summer melting. Thickness initialisation has little improvements for detrended sea ice extent anomalies, but yields some skill in the Beaufort Sea and Central Arctic during summer. Overall, we show the impact of sea ice thickness assimilation has a positive effect on prediction skill in NorCPM.

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Nicholas Williams, Yiguo Wang, and François Counillon

Status: final response (author comments only)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2025-104', Alison Delhasse & Francois Massonnet (co-review team), 19 Mar 2025
    • AC1: 'Reply on RC1', Nicholas Williams, 02 Jul 2025
    • AC2: 'Reply on RC1', Nicholas Williams, 04 Jul 2025
  • RC2: 'Comment on egusphere-2025-104', Imke Sievers, 07 Jul 2025
    • AC3: 'Reply on RC2', Nicholas Williams, 28 Jul 2025
    • AC4: 'Reply on RC2', Nicholas Williams, 04 Aug 2025
Nicholas Williams, Yiguo Wang, and François Counillon
Nicholas Williams, Yiguo Wang, and François Counillon

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Short summary
We assimilate satellite observations of Arctic sea ice thickness to create a skillful initial sea ice state, assimilating ENVISAT-derived sea ice thickness for the first time. We produce a reanalysis and seasonal hindcasts showing that sea ice thickness and volume estimates are significantly improved in both reanalysis and prediction. Predictions of summer sea ice extent in our model are also substantially improved by reducing the high sea ice thickness bias.
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