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...
Published in: | Climate Dynamics |
---|---|
Main Authors: | , , , , |
Format: | Text |
Language: | English |
Published: |
Springer Berlin Heidelberg
2018
|
Subjects: | |
Online Access: | http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6413483/ https://doi.org/10.1007/s00382-018-4279-z |
id |
ftpubmed:oai:pubmedcentral.nih.gov:6413483 |
---|---|
record_format |
openpolar |
spelling |
ftpubmed:oai:pubmedcentral.nih.gov:6413483 2023-05-15T14:35:34+02:00 Summers with low Arctic sea ice linked to persistence of spring atmospheric circulation patterns Kapsch, Marie-Luise Skific, Natasa Graversen, Rune G. Tjernström, Michael Francis, Jennifer A. 2018-05-30 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6413483/ https://doi.org/10.1007/s00382-018-4279-z en eng Springer Berlin Heidelberg http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6413483/ http://dx.doi.org/10.1007/s00382-018-4279-z © The Author(s) 2018 Open AccessThis article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. CC-BY Article Text 2018 ftpubmed https://doi.org/10.1007/s00382-018-4279-z 2019-04-07T00:27:53Z 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. ELECTRONIC SUPPLEMENTARY MATERIAL: The online version of this article (10.1007/s00382-018-4279-z) contains supplementary material, which is available to authorized users. Text Arctic Arctic Ocean Kara Sea Sea ice Siberia PubMed Central (PMC) Arctic Arctic Ocean Kara Sea Pacific Climate Dynamics 52 3-4 2497 2512 |
institution |
Open Polar |
collection |
PubMed Central (PMC) |
op_collection_id |
ftpubmed |
language |
English |
topic |
Article |
spellingShingle |
Article Kapsch, Marie-Luise Skific, Natasa Graversen, Rune G. Tjernström, Michael Francis, Jennifer A. Summers with low Arctic sea ice linked to persistence of spring atmospheric circulation patterns |
topic_facet |
Article |
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. ELECTRONIC SUPPLEMENTARY MATERIAL: The online version of this article (10.1007/s00382-018-4279-z) contains supplementary material, which is available to authorized users. |
format |
Text |
author |
Kapsch, Marie-Luise Skific, Natasa Graversen, Rune G. Tjernström, Michael Francis, Jennifer A. |
author_facet |
Kapsch, Marie-Luise Skific, Natasa Graversen, Rune G. Tjernström, Michael Francis, Jennifer A. |
author_sort |
Kapsch, Marie-Luise |
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 |
publisher |
Springer Berlin Heidelberg |
publishDate |
2018 |
url |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6413483/ https://doi.org/10.1007/s00382-018-4279-z |
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_relation |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6413483/ http://dx.doi.org/10.1007/s00382-018-4279-z |
op_rights |
© The Author(s) 2018 Open AccessThis article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. |
op_rightsnorm |
CC-BY |
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 |
_version_ |
1766308364493520896 |