Patterns of wintertime Arctic sea-ice leads and their relation to winds and ocean currents

We use a novel sea-ice lead climatology for the winters of 2002/03 to 2020/21 based on satellite observations with 1 km 2 spatial resolution to identify predominant patterns in Arctic wintertime sea-ice leads. The causes for the observed spatial and temporal variabilities are investigated using ocea...

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Published in:The Cryosphere
Main Authors: Willmes, Sascha, Heinemann, Günther, Schnaase, Frank
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/tc-17-3291-2023
https://tc.copernicus.org/articles/17/3291/2023/
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spelling ftcopernicus:oai:publications.copernicus.org:tc109533 2023-09-05T13:16:59+02:00 Patterns of wintertime Arctic sea-ice leads and their relation to winds and ocean currents Willmes, Sascha Heinemann, Günther Schnaase, Frank 2023-08-17 application/pdf https://doi.org/10.5194/tc-17-3291-2023 https://tc.copernicus.org/articles/17/3291/2023/ eng eng doi:10.5194/tc-17-3291-2023 https://tc.copernicus.org/articles/17/3291/2023/ eISSN: 1994-0424 Text 2023 ftcopernicus https://doi.org/10.5194/tc-17-3291-2023 2023-08-21T16:24:14Z We use a novel sea-ice lead climatology for the winters of 2002/03 to 2020/21 based on satellite observations with 1 km 2 spatial resolution to identify predominant patterns in Arctic wintertime sea-ice leads. The causes for the observed spatial and temporal variabilities are investigated using ocean surface current velocities and eddy kinetic energies from an ocean model (Finite Element Sea Ice–Ice-Shelf–Ocean Model, FESOM) and winds from a regional climate model (CCLM) and ERA5 reanalysis, respectively. The presented investigation provides evidence for an influence of ocean bathymetry and associated currents on the mechanic weakening of sea ice and the accompanying occurrence of sea-ice leads with their characteristic spatial patterns. While the driving mechanisms for this observation are not yet understood in detail, the presented results can contribute to opening new hypotheses on ocean–sea-ice interactions. The individual contribution of ocean and atmosphere to regional lead dynamics is complex, and a deeper insight requires detailed mechanistic investigations in combination with considerations of coastal geometries. While the ocean influence on lead dynamics seems to act on a rather long-term scale (seasonal to interannual), the influence of wind appears to trigger sea-ice lead dynamics on shorter timescales of weeks to months and is largely controlled by individual events causing increased divergence. No significant pan-Arctic trends in wintertime leads can be observed. Text Arctic Ice Shelf Sea ice Copernicus Publications: E-Journals Arctic The Cryosphere 17 8 3291 3308
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description We use a novel sea-ice lead climatology for the winters of 2002/03 to 2020/21 based on satellite observations with 1 km 2 spatial resolution to identify predominant patterns in Arctic wintertime sea-ice leads. The causes for the observed spatial and temporal variabilities are investigated using ocean surface current velocities and eddy kinetic energies from an ocean model (Finite Element Sea Ice–Ice-Shelf–Ocean Model, FESOM) and winds from a regional climate model (CCLM) and ERA5 reanalysis, respectively. The presented investigation provides evidence for an influence of ocean bathymetry and associated currents on the mechanic weakening of sea ice and the accompanying occurrence of sea-ice leads with their characteristic spatial patterns. While the driving mechanisms for this observation are not yet understood in detail, the presented results can contribute to opening new hypotheses on ocean–sea-ice interactions. The individual contribution of ocean and atmosphere to regional lead dynamics is complex, and a deeper insight requires detailed mechanistic investigations in combination with considerations of coastal geometries. While the ocean influence on lead dynamics seems to act on a rather long-term scale (seasonal to interannual), the influence of wind appears to trigger sea-ice lead dynamics on shorter timescales of weeks to months and is largely controlled by individual events causing increased divergence. No significant pan-Arctic trends in wintertime leads can be observed.
format Text
author Willmes, Sascha
Heinemann, Günther
Schnaase, Frank
spellingShingle Willmes, Sascha
Heinemann, Günther
Schnaase, Frank
Patterns of wintertime Arctic sea-ice leads and their relation to winds and ocean currents
author_facet Willmes, Sascha
Heinemann, Günther
Schnaase, Frank
author_sort Willmes, Sascha
title Patterns of wintertime Arctic sea-ice leads and their relation to winds and ocean currents
title_short Patterns of wintertime Arctic sea-ice leads and their relation to winds and ocean currents
title_full Patterns of wintertime Arctic sea-ice leads and their relation to winds and ocean currents
title_fullStr Patterns of wintertime Arctic sea-ice leads and their relation to winds and ocean currents
title_full_unstemmed Patterns of wintertime Arctic sea-ice leads and their relation to winds and ocean currents
title_sort patterns of wintertime arctic sea-ice leads and their relation to winds and ocean currents
publishDate 2023
url https://doi.org/10.5194/tc-17-3291-2023
https://tc.copernicus.org/articles/17/3291/2023/
geographic Arctic
geographic_facet Arctic
genre Arctic
Ice Shelf
Sea ice
genre_facet Arctic
Ice Shelf
Sea ice
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-17-3291-2023
https://tc.copernicus.org/articles/17/3291/2023/
op_doi https://doi.org/10.5194/tc-17-3291-2023
container_title The Cryosphere
container_volume 17
container_issue 8
container_start_page 3291
op_container_end_page 3308
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