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 (SO...

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Main Authors: Min-Hee Lee, Joo-Hong Kim
Format: Article
Language:English
Published: MDPI AG 2019-08-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/10/8/474
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spelling doaj-508e1d8bb6b546ce870b050e7e1501292020-11-25T02:53:05ZengMDPI AGAtmosphere2073-44332019-08-0110847410.3390/atmos10080474atmos10080474The Role of Synoptic Cyclones for the Formation of Arctic Summer Circulation Patterns as Clustered by Self-Organizing MapsMin-Hee Lee0Joo-Hong Kim1Korea Polar Research Institute, 26, Songdomirae-ro, Yeonsu-gu, Incheon 21990, KoreaKorea Polar Research Institute, 26, Songdomirae-ro, Yeonsu-gu, Incheon 21990, KoreaContribution 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.https://www.mdpi.com/2073-4433/10/8/474Arctic summer circulation patternsextra-tropical synoptic cyclonesself-organizing maps (SOMs)cyclone detection and tracking
collection DOAJ
language English
format Article
sources DOAJ
author Min-Hee Lee
Joo-Hong Kim
spellingShingle 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
Atmosphere
Arctic summer circulation patterns
extra-tropical synoptic cyclones
self-organizing maps (SOMs)
cyclone detection and tracking
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 MDPI AG
series Atmosphere
issn 2073-4433
publishDate 2019-08-01
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.
topic Arctic summer circulation patterns
extra-tropical synoptic cyclones
self-organizing maps (SOMs)
cyclone detection and tracking
url https://www.mdpi.com/2073-4433/10/8/474
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