Rapid sea ice changes in the future Barents Sea

Observed and future winter Arctic sea ice loss is strongest in the Barents Sea. However, the anthropogenic signal of the sea ice decline is superimposed by pronounced internal variability that represents a large source of uncertainty in future climate projections. A notable manifestation of internal...

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Published in:The Cryosphere
Main Authors: Rieke, Ole, Årthun, Marius, Dörr, Jakob Simon
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/tc-17-1445-2023
https://tc.copernicus.org/articles/17/1445/2023/
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spelling ftcopernicus:oai:publications.copernicus.org:tc103092 2023-05-15T15:06:48+02:00 Rapid sea ice changes in the future Barents Sea Rieke, Ole Årthun, Marius Dörr, Jakob Simon 2023-04-04 application/pdf https://doi.org/10.5194/tc-17-1445-2023 https://tc.copernicus.org/articles/17/1445/2023/ eng eng doi:10.5194/tc-17-1445-2023 https://tc.copernicus.org/articles/17/1445/2023/ eISSN: 1994-0424 Text 2023 ftcopernicus https://doi.org/10.5194/tc-17-1445-2023 2023-04-10T16:23:11Z Observed and future winter Arctic sea ice loss is strongest in the Barents Sea. However, the anthropogenic signal of the sea ice decline is superimposed by pronounced internal variability that represents a large source of uncertainty in future climate projections. A notable manifestation of internal variability is rapid ice change events (RICEs) that greatly exceed the anthropogenic trend. These RICEs are associated with large displacements of the sea ice edge which could potentially have both local and remote impacts on the climate system. In this study we present the first investigation of the frequency and drivers of RICEs in the future Barents Sea, using multi-member ensemble simulations from CMIP5 and CMIP6. A majority of RICEs are triggered by trends in ocean heat transport or surface heat fluxes. Ice loss events are associated with increasing trends in ocean heat transport and decreasing trends in surface heat loss. RICEs are a common feature of the future Barents Sea until the region becomes close to ice-free. As their evolution over time is closely tied to the average sea ice conditions, rapid ice changes in the Barents Sea may serve as a precursor for future changes in adjacent seas. Text Arctic Barents Sea Sea ice Copernicus Publications: E-Journals Arctic Barents Sea The Cryosphere 17 4 1445 1456
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Observed and future winter Arctic sea ice loss is strongest in the Barents Sea. However, the anthropogenic signal of the sea ice decline is superimposed by pronounced internal variability that represents a large source of uncertainty in future climate projections. A notable manifestation of internal variability is rapid ice change events (RICEs) that greatly exceed the anthropogenic trend. These RICEs are associated with large displacements of the sea ice edge which could potentially have both local and remote impacts on the climate system. In this study we present the first investigation of the frequency and drivers of RICEs in the future Barents Sea, using multi-member ensemble simulations from CMIP5 and CMIP6. A majority of RICEs are triggered by trends in ocean heat transport or surface heat fluxes. Ice loss events are associated with increasing trends in ocean heat transport and decreasing trends in surface heat loss. RICEs are a common feature of the future Barents Sea until the region becomes close to ice-free. As their evolution over time is closely tied to the average sea ice conditions, rapid ice changes in the Barents Sea may serve as a precursor for future changes in adjacent seas.
format Text
author Rieke, Ole
Årthun, Marius
Dörr, Jakob Simon
spellingShingle Rieke, Ole
Årthun, Marius
Dörr, Jakob Simon
Rapid sea ice changes in the future Barents Sea
author_facet Rieke, Ole
Årthun, Marius
Dörr, Jakob Simon
author_sort Rieke, Ole
title Rapid sea ice changes in the future Barents Sea
title_short Rapid sea ice changes in the future Barents Sea
title_full Rapid sea ice changes in the future Barents Sea
title_fullStr Rapid sea ice changes in the future Barents Sea
title_full_unstemmed Rapid sea ice changes in the future Barents Sea
title_sort rapid sea ice changes in the future barents sea
publishDate 2023
url https://doi.org/10.5194/tc-17-1445-2023
https://tc.copernicus.org/articles/17/1445/2023/
geographic Arctic
Barents Sea
geographic_facet Arctic
Barents Sea
genre Arctic
Barents Sea
Sea ice
genre_facet Arctic
Barents Sea
Sea ice
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-17-1445-2023
https://tc.copernicus.org/articles/17/1445/2023/
op_doi https://doi.org/10.5194/tc-17-1445-2023
container_title The Cryosphere
container_volume 17
container_issue 4
container_start_page 1445
op_container_end_page 1456
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