Towards improving short-term sea ice predictability using deformation observations

Short-term sea ice predictability is challenging due to the lack of constraints on ice deformation features (open leads and ridges) at kilometre scale. Deformation observations capture these small-scale features and have the potential to improve the predictability. A new method for assimilation of s...

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Main Authors: Korosov, Anton, Rampal, Pierre, Ying, Yue, Ólason, Einar, Williams, Timothy
Format: Text
Language:English
Published: 2022
Subjects:
Online Access:https://doi.org/10.5194/tc-2022-46
https://tc.copernicus.org/preprints/tc-2022-46/
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spelling ftcopernicus:oai:publications.copernicus.org:tcd101548 2023-05-15T18:16:19+02:00 Towards improving short-term sea ice predictability using deformation observations Korosov, Anton Rampal, Pierre Ying, Yue Ólason, Einar Williams, Timothy 2022-02-22 application/pdf https://doi.org/10.5194/tc-2022-46 https://tc.copernicus.org/preprints/tc-2022-46/ eng eng doi:10.5194/tc-2022-46 https://tc.copernicus.org/preprints/tc-2022-46/ eISSN: 1994-0424 Text 2022 ftcopernicus https://doi.org/10.5194/tc-2022-46 2022-02-28T17:22:16Z Short-term sea ice predictability is challenging due to the lack of constraints on ice deformation features (open leads and ridges) at kilometre scale. Deformation observations capture these small-scale features and have the potential to improve the predictability. A new method for assimilation of satellite-derived sea ice deformation into the neXt generation Sea Ice Model (neXtSIM) is presented. Ice deformation provided by the Copernicus Marine Environmental Monitoring Service is computed from sea ice drift derived from Synthetic Aperture Radar at a spatio-temporal resolution of 10 km and 24 hours. We show that high values of ice deformation can be interpreted as reduced ice concentration and increased ice damage – scalar variables of neXtSIM. The proof-of-concept assimilation scheme uses a data nudging approach and deterministic forecasting with one member. Assimilation and forecasting experiments are run on example observations from January 2021 and show improvement of neXtSIM skills to predict sea ice deformation in 3–5 days horizon. It is demonstrated that neXtSIM is also capable of extrapolating the assimilated information in space — gaps in spatially discontinuous satellite observations of deformation are filled with a realistic pattern of ice cracks, confirmed by later satellite observations. The experiments also indicate that reduction in sea ice concentration plays a bigger role in improving ice deformation forecast on synoptic scales. Limitations and usefulness of the proposed assimilation approach are discussed in a context of ensemble forecasts. Pathways to estimate intrinsic predictability of sea ice deformation are proposed. Text Sea ice Copernicus Publications: E-Journals
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Short-term sea ice predictability is challenging due to the lack of constraints on ice deformation features (open leads and ridges) at kilometre scale. Deformation observations capture these small-scale features and have the potential to improve the predictability. A new method for assimilation of satellite-derived sea ice deformation into the neXt generation Sea Ice Model (neXtSIM) is presented. Ice deformation provided by the Copernicus Marine Environmental Monitoring Service is computed from sea ice drift derived from Synthetic Aperture Radar at a spatio-temporal resolution of 10 km and 24 hours. We show that high values of ice deformation can be interpreted as reduced ice concentration and increased ice damage – scalar variables of neXtSIM. The proof-of-concept assimilation scheme uses a data nudging approach and deterministic forecasting with one member. Assimilation and forecasting experiments are run on example observations from January 2021 and show improvement of neXtSIM skills to predict sea ice deformation in 3–5 days horizon. It is demonstrated that neXtSIM is also capable of extrapolating the assimilated information in space — gaps in spatially discontinuous satellite observations of deformation are filled with a realistic pattern of ice cracks, confirmed by later satellite observations. The experiments also indicate that reduction in sea ice concentration plays a bigger role in improving ice deformation forecast on synoptic scales. Limitations and usefulness of the proposed assimilation approach are discussed in a context of ensemble forecasts. Pathways to estimate intrinsic predictability of sea ice deformation are proposed.
format Text
author Korosov, Anton
Rampal, Pierre
Ying, Yue
Ólason, Einar
Williams, Timothy
spellingShingle Korosov, Anton
Rampal, Pierre
Ying, Yue
Ólason, Einar
Williams, Timothy
Towards improving short-term sea ice predictability using deformation observations
author_facet Korosov, Anton
Rampal, Pierre
Ying, Yue
Ólason, Einar
Williams, Timothy
author_sort Korosov, Anton
title Towards improving short-term sea ice predictability using deformation observations
title_short Towards improving short-term sea ice predictability using deformation observations
title_full Towards improving short-term sea ice predictability using deformation observations
title_fullStr Towards improving short-term sea ice predictability using deformation observations
title_full_unstemmed Towards improving short-term sea ice predictability using deformation observations
title_sort towards improving short-term sea ice predictability using deformation observations
publishDate 2022
url https://doi.org/10.5194/tc-2022-46
https://tc.copernicus.org/preprints/tc-2022-46/
genre Sea ice
genre_facet Sea ice
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-2022-46
https://tc.copernicus.org/preprints/tc-2022-46/
op_doi https://doi.org/10.5194/tc-2022-46
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