Summers with low Arctic sea ice linked to persistence of spring atmospheric circulation patterns

The declining trend of Arctic September sea ice constitutes a significant change in the Arctic climate system. Large year-to-year variations are superimposed on this sea–ice trend, with the largest variability observed in the eastern Arctic Ocean. Knowledge of the processes important for this variab...

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Published in:Climate Dynamics
Main Authors: Kapsch, M., Skific, N., Graversen, R., Tjernström, M., Francis, J.
Format: Article in Journal/Newspaper
Language:English
Published: 2019
Subjects:
Online Access:http://hdl.handle.net/21.11116/0000-0002-004F-6
http://hdl.handle.net/21.11116/0000-0003-43DF-7
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spelling ftpubman:oai:pure.mpg.de:item_2637936 2023-08-20T04:03:27+02:00 Summers with low Arctic sea ice linked to persistence of spring atmospheric circulation patterns Kapsch, M. Skific, N. Graversen, R. Tjernström, M. Francis, J. 2019-02 application/pdf http://hdl.handle.net/21.11116/0000-0002-004F-6 http://hdl.handle.net/21.11116/0000-0003-43DF-7 eng eng info:eu-repo/semantics/altIdentifier/doi/10.1007/s00382-018-4279-z http://hdl.handle.net/21.11116/0000-0002-004F-6 http://hdl.handle.net/21.11116/0000-0003-43DF-7 info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/4.0/ Climate Dynamics info:eu-repo/semantics/article 2019 ftpubman https://doi.org/10.1007/s00382-018-4279-z 2023-08-01T23:17:50Z The declining trend of Arctic September sea ice constitutes a significant change in the Arctic climate system. Large year-to-year variations are superimposed on this sea–ice trend, with the largest variability observed in the eastern Arctic Ocean. Knowledge of the processes important for this variability may lead to an improved understanding of seasonal and long-term changes. Previous studies suggest that transport of heat and moisture into the Arctic during spring enhances downward surface longwave radiation, thereby controlling the annual melt onset, setting the stage for the September ice minimum. In agreement with these studies, we find that years with a low September sea–ice concentration (SIC) are characterized by more persistent periods in spring with enhanced energy flux to the surface in forms of net longwave radiation plus turbulent fluxes, compared to years with a high SIC. Two main atmospheric circulation patterns related to these episodes are identified: one resembles the so-called Arctic dipole anomaly that promotes transport of heat and moisture from the North Pacific, whereas the other is characterized by negative geopotential height anomalies over the Arctic, favoring cyclonic flow from Siberia and the Kara Sea into the eastern Arctic Ocean. However, differences between years with low and high September SIC appear not to be due to different spring circulation patterns; instead it is the persistence and intensity of processes associated with these patterns that distinguish the two groups of anomalous years: Years with low September SIC feature episodes that are consistently stronger and more persistent than years with high SIC. © 2018 The Author(s) Article in Journal/Newspaper Arctic Arctic Ocean Kara Sea Sea ice Siberia Max Planck Society: MPG.PuRe Arctic Arctic Ocean Kara Sea Pacific Climate Dynamics 52 3-4 2497 2512
institution Open Polar
collection Max Planck Society: MPG.PuRe
op_collection_id ftpubman
language English
description The declining trend of Arctic September sea ice constitutes a significant change in the Arctic climate system. Large year-to-year variations are superimposed on this sea–ice trend, with the largest variability observed in the eastern Arctic Ocean. Knowledge of the processes important for this variability may lead to an improved understanding of seasonal and long-term changes. Previous studies suggest that transport of heat and moisture into the Arctic during spring enhances downward surface longwave radiation, thereby controlling the annual melt onset, setting the stage for the September ice minimum. In agreement with these studies, we find that years with a low September sea–ice concentration (SIC) are characterized by more persistent periods in spring with enhanced energy flux to the surface in forms of net longwave radiation plus turbulent fluxes, compared to years with a high SIC. Two main atmospheric circulation patterns related to these episodes are identified: one resembles the so-called Arctic dipole anomaly that promotes transport of heat and moisture from the North Pacific, whereas the other is characterized by negative geopotential height anomalies over the Arctic, favoring cyclonic flow from Siberia and the Kara Sea into the eastern Arctic Ocean. However, differences between years with low and high September SIC appear not to be due to different spring circulation patterns; instead it is the persistence and intensity of processes associated with these patterns that distinguish the two groups of anomalous years: Years with low September SIC feature episodes that are consistently stronger and more persistent than years with high SIC. © 2018 The Author(s)
format Article in Journal/Newspaper
author Kapsch, M.
Skific, N.
Graversen, R.
Tjernström, M.
Francis, J.
spellingShingle Kapsch, M.
Skific, N.
Graversen, R.
Tjernström, M.
Francis, J.
Summers with low Arctic sea ice linked to persistence of spring atmospheric circulation patterns
author_facet Kapsch, M.
Skific, N.
Graversen, R.
Tjernström, M.
Francis, J.
author_sort Kapsch, M.
title Summers with low Arctic sea ice linked to persistence of spring atmospheric circulation patterns
title_short Summers with low Arctic sea ice linked to persistence of spring atmospheric circulation patterns
title_full Summers with low Arctic sea ice linked to persistence of spring atmospheric circulation patterns
title_fullStr Summers with low Arctic sea ice linked to persistence of spring atmospheric circulation patterns
title_full_unstemmed Summers with low Arctic sea ice linked to persistence of spring atmospheric circulation patterns
title_sort summers with low arctic sea ice linked to persistence of spring atmospheric circulation patterns
publishDate 2019
url http://hdl.handle.net/21.11116/0000-0002-004F-6
http://hdl.handle.net/21.11116/0000-0003-43DF-7
geographic Arctic
Arctic Ocean
Kara Sea
Pacific
geographic_facet Arctic
Arctic Ocean
Kara Sea
Pacific
genre Arctic
Arctic Ocean
Kara Sea
Sea ice
Siberia
genre_facet Arctic
Arctic Ocean
Kara Sea
Sea ice
Siberia
op_source Climate Dynamics
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1007/s00382-018-4279-z
http://hdl.handle.net/21.11116/0000-0002-004F-6
http://hdl.handle.net/21.11116/0000-0003-43DF-7
op_rights info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1007/s00382-018-4279-z
container_title Climate Dynamics
container_volume 52
container_issue 3-4
container_start_page 2497
op_container_end_page 2512
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