The Role of Synoptic Cyclones for the Formation of Arctic Summer Circulation Patterns as Clustered by Self-Organizing Maps

Contribution of extra-tropical synoptic cyclones to the formation of mean summer atmospheric circulation patterns in the Arctic domain (≥60° N) was investigated by clustering dominant Arctic circulation patterns based on daily mean sea-level pressure using self-organizing maps (SOMs). Three SOM patt...

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Published in:Atmosphere
Main Authors: Min-Hee Lee, Joo-Hong Kim
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2019
Subjects:
Online Access:https://doi.org/10.3390/atmos10080474
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spelling ftmdpi:oai:mdpi.com:/2073-4433/10/8/474/ 2023-08-20T04:03:23+02:00 The Role of Synoptic Cyclones for the Formation of Arctic Summer Circulation Patterns as Clustered by Self-Organizing Maps Min-Hee Lee Joo-Hong Kim agris 2019-08-19 application/pdf https://doi.org/10.3390/atmos10080474 EN eng Multidisciplinary Digital Publishing Institute Climatology https://dx.doi.org/10.3390/atmos10080474 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 10; Issue 8; Pages: 474 Arctic summer circulation patterns extra-tropical synoptic cyclones self-organizing maps (SOMs) cyclone detection and tracking Text 2019 ftmdpi https://doi.org/10.3390/atmos10080474 2023-07-31T22:31:57Z Contribution of extra-tropical synoptic cyclones to the formation of mean summer atmospheric circulation patterns in the Arctic domain (≥60° N) was investigated by clustering dominant Arctic circulation patterns based on daily mean sea-level pressure using self-organizing maps (SOMs). Three SOM patterns were identified; one pattern had prevalent low-pressure anomalies in the Arctic Circle (SOM1), while two exhibited opposite dipoles with primary high-pressure anomalies covering the Arctic Ocean (SOM2 and SOM3). The time series of their occurrence frequencies demonstrated the largest inter-annual variation in SOM1, a slight decreasing trend in SOM2, and the abrupt upswing after 2007 in SOM3. Analyses of synoptic cyclone activity using the cyclone track data confirmed the vital contribution of synoptic cyclones to the formation of large-scale patterns. Arctic cyclone activity was enhanced in the SOM1, which was consistent with the meridional temperature gradient increases over the land–Arctic ocean boundaries co-located with major cyclone pathways. The composite daily synoptic evolution of each SOM revealed that all three SOMs persisted for less than five days on average. These evolutionary short-term weather patterns have substantial variability at inter-annual and longer timescales. Therefore, the synoptic-scale activity is central to forming the seasonal-mean climate of the Arctic. Text Arctic Arctic Ocean MDPI Open Access Publishing Arctic Arctic Ocean Atmosphere 10 8 474
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic Arctic summer circulation patterns
extra-tropical synoptic cyclones
self-organizing maps (SOMs)
cyclone detection and tracking
spellingShingle Arctic summer circulation patterns
extra-tropical synoptic cyclones
self-organizing maps (SOMs)
cyclone detection and tracking
Min-Hee Lee
Joo-Hong Kim
The Role of Synoptic Cyclones for the Formation of Arctic Summer Circulation Patterns as Clustered by Self-Organizing Maps
topic_facet Arctic summer circulation patterns
extra-tropical synoptic cyclones
self-organizing maps (SOMs)
cyclone detection and tracking
description Contribution of extra-tropical synoptic cyclones to the formation of mean summer atmospheric circulation patterns in the Arctic domain (≥60° N) was investigated by clustering dominant Arctic circulation patterns based on daily mean sea-level pressure using self-organizing maps (SOMs). Three SOM patterns were identified; one pattern had prevalent low-pressure anomalies in the Arctic Circle (SOM1), while two exhibited opposite dipoles with primary high-pressure anomalies covering the Arctic Ocean (SOM2 and SOM3). The time series of their occurrence frequencies demonstrated the largest inter-annual variation in SOM1, a slight decreasing trend in SOM2, and the abrupt upswing after 2007 in SOM3. Analyses of synoptic cyclone activity using the cyclone track data confirmed the vital contribution of synoptic cyclones to the formation of large-scale patterns. Arctic cyclone activity was enhanced in the SOM1, which was consistent with the meridional temperature gradient increases over the land–Arctic ocean boundaries co-located with major cyclone pathways. The composite daily synoptic evolution of each SOM revealed that all three SOMs persisted for less than five days on average. These evolutionary short-term weather patterns have substantial variability at inter-annual and longer timescales. Therefore, the synoptic-scale activity is central to forming the seasonal-mean climate of the Arctic.
format Text
author Min-Hee Lee
Joo-Hong Kim
author_facet Min-Hee Lee
Joo-Hong Kim
author_sort Min-Hee Lee
title The Role of Synoptic Cyclones for the Formation of Arctic Summer Circulation Patterns as Clustered by Self-Organizing Maps
title_short The Role of Synoptic Cyclones for the Formation of Arctic Summer Circulation Patterns as Clustered by Self-Organizing Maps
title_full The Role of Synoptic Cyclones for the Formation of Arctic Summer Circulation Patterns as Clustered by Self-Organizing Maps
title_fullStr The Role of Synoptic Cyclones for the Formation of Arctic Summer Circulation Patterns as Clustered by Self-Organizing Maps
title_full_unstemmed The Role of Synoptic Cyclones for the Formation of Arctic Summer Circulation Patterns as Clustered by Self-Organizing Maps
title_sort role of synoptic cyclones for the formation of arctic summer circulation patterns as clustered by self-organizing maps
publisher Multidisciplinary Digital Publishing Institute
publishDate 2019
url https://doi.org/10.3390/atmos10080474
op_coverage agris
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
genre_facet Arctic
Arctic Ocean
op_source Atmosphere; Volume 10; Issue 8; Pages: 474
op_relation Climatology
https://dx.doi.org/10.3390/atmos10080474
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos10080474
container_title Atmosphere
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container_issue 8
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