Regional Features of the Arctic Sea Ice Area Changes in 2000–2019 versus 1979–1999 Periods

One of the most striking manifestations of ongoing climate change is a rapid shrinking of the Arctic sea ice area (SIA). An important feature of the observed SIA loss is a nonlinear rate of a decline with an accelerated decrease in the 2000–2019 period relative to a more gradual decline in 1979–1999...

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Published in:Atmosphere
Main Authors: Tatiana A. Matveeva, Vladimir A. Semenov
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2022
Subjects:
Online Access:https://doi.org/10.3390/atmos13091434
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spelling ftmdpi:oai:mdpi.com:/2073-4433/13/9/1434/ 2023-08-20T04:03:25+02:00 Regional Features of the Arctic Sea Ice Area Changes in 2000–2019 versus 1979–1999 Periods Tatiana A. Matveeva Vladimir A. Semenov agris 2022-09-05 application/pdf https://doi.org/10.3390/atmos13091434 EN eng Multidisciplinary Digital Publishing Institute Climatology https://dx.doi.org/10.3390/atmos13091434 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 13; Issue 9; Pages: 1434 Arctic sea ice Arctic climate climate change ERA5 Text 2022 ftmdpi https://doi.org/10.3390/atmos13091434 2023-08-01T06:21:44Z One of the most striking manifestations of ongoing climate change is a rapid shrinking of the Arctic sea ice area (SIA). An important feature of the observed SIA loss is a nonlinear rate of a decline with an accelerated decrease in the 2000–2019 period relative to a more gradual decline in 1979–1999. In this study, we perform a quantitative assessment and comparison of the spatial-temporal SIA changes during these two periods. It was found that winter Arctic SIA loss is primarily associated with changes in the Barents Sea, where the SIA decline in 2000–2019 has accelerated more than three-fold in comparison with 1979–1999. In summer and autumn, rates of SIA decline in 2000–2019 increased most strongly in the Kara, Beaufort Seas, the Northwestern Passage, and inner Arctic Ocean. The amplitude of the SIA seasonal cycle has also increased in 2000–2019 in comparison with the earlier period, with the largest changes in the inner Arctic Ocean, the Kara, Laptev, East Siberian and Beaufort Seas in summer and in the Barents Sea in winter. The results may reflect a transition to a new dynamic state in the recent two decades with the triggering of positive feedbacks in the Arctic climate system. Text Arctic Arctic Ocean Barents Sea Climate change Kara-Laptev laptev Northwestern passage Sea ice MDPI Open Access Publishing Arctic Arctic Ocean Barents Sea Atmosphere 13 9 1434
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic Arctic sea ice
Arctic climate
climate change
ERA5
spellingShingle Arctic sea ice
Arctic climate
climate change
ERA5
Tatiana A. Matveeva
Vladimir A. Semenov
Regional Features of the Arctic Sea Ice Area Changes in 2000–2019 versus 1979–1999 Periods
topic_facet Arctic sea ice
Arctic climate
climate change
ERA5
description One of the most striking manifestations of ongoing climate change is a rapid shrinking of the Arctic sea ice area (SIA). An important feature of the observed SIA loss is a nonlinear rate of a decline with an accelerated decrease in the 2000–2019 period relative to a more gradual decline in 1979–1999. In this study, we perform a quantitative assessment and comparison of the spatial-temporal SIA changes during these two periods. It was found that winter Arctic SIA loss is primarily associated with changes in the Barents Sea, where the SIA decline in 2000–2019 has accelerated more than three-fold in comparison with 1979–1999. In summer and autumn, rates of SIA decline in 2000–2019 increased most strongly in the Kara, Beaufort Seas, the Northwestern Passage, and inner Arctic Ocean. The amplitude of the SIA seasonal cycle has also increased in 2000–2019 in comparison with the earlier period, with the largest changes in the inner Arctic Ocean, the Kara, Laptev, East Siberian and Beaufort Seas in summer and in the Barents Sea in winter. The results may reflect a transition to a new dynamic state in the recent two decades with the triggering of positive feedbacks in the Arctic climate system.
format Text
author Tatiana A. Matveeva
Vladimir A. Semenov
author_facet Tatiana A. Matveeva
Vladimir A. Semenov
author_sort Tatiana A. Matveeva
title Regional Features of the Arctic Sea Ice Area Changes in 2000–2019 versus 1979–1999 Periods
title_short Regional Features of the Arctic Sea Ice Area Changes in 2000–2019 versus 1979–1999 Periods
title_full Regional Features of the Arctic Sea Ice Area Changes in 2000–2019 versus 1979–1999 Periods
title_fullStr Regional Features of the Arctic Sea Ice Area Changes in 2000–2019 versus 1979–1999 Periods
title_full_unstemmed Regional Features of the Arctic Sea Ice Area Changes in 2000–2019 versus 1979–1999 Periods
title_sort regional features of the arctic sea ice area changes in 2000–2019 versus 1979–1999 periods
publisher Multidisciplinary Digital Publishing Institute
publishDate 2022
url https://doi.org/10.3390/atmos13091434
op_coverage agris
geographic Arctic
Arctic Ocean
Barents Sea
geographic_facet Arctic
Arctic Ocean
Barents Sea
genre Arctic
Arctic Ocean
Barents Sea
Climate change
Kara-Laptev
laptev
Northwestern passage
Sea ice
genre_facet Arctic
Arctic Ocean
Barents Sea
Climate change
Kara-Laptev
laptev
Northwestern passage
Sea ice
op_source Atmosphere; Volume 13; Issue 9; Pages: 1434
op_relation Climatology
https://dx.doi.org/10.3390/atmos13091434
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos13091434
container_title Atmosphere
container_volume 13
container_issue 9
container_start_page 1434
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