Climatic interactions between cold surges in the South China Sea and North Pacific extratropical cyclones

Abstract Cold surge events in the South China Sea (over 110–117.5° E longitude at 15° N latitude) from 1979 to 2019 are divided into four types depending on their correlation with North Pacific extratropical cyclones (ECs). Climatologic relationships between the two phenomena reveal that 92% (39%) o...

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Published in:Meteorological Applications
Main Authors: Xia, Lan, Zhang, Jialin, Hu, Yao
Other Authors: National Natural Science Foundation of China, Applied Basic Research Foundation of Yunnan Province
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2024
Subjects:
Online Access:http://dx.doi.org/10.1002/met.2182
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/met.2182
id crwiley:10.1002/met.2182
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spelling crwiley:10.1002/met.2182 2024-06-02T07:54:44+00:00 Climatic interactions between cold surges in the South China Sea and North Pacific extratropical cyclones Xia, Lan Zhang, Jialin Hu, Yao National Natural Science Foundation of China Applied Basic Research Foundation of Yunnan Province 2024 http://dx.doi.org/10.1002/met.2182 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/met.2182 en eng Wiley http://creativecommons.org/licenses/by-nc-nd/4.0/ Meteorological Applications volume 31, issue 2 ISSN 1350-4827 1469-8080 journal-article 2024 crwiley https://doi.org/10.1002/met.2182 2024-05-03T12:02:16Z Abstract Cold surge events in the South China Sea (over 110–117.5° E longitude at 15° N latitude) from 1979 to 2019 are divided into four types depending on their correlation with North Pacific extratropical cyclones (ECs). Climatologic relationships between the two phenomena reveal that 92% (39%) of all cold surges are accompanied by ECs (explosive extratropical cyclones, abbreviated as EC‐E), while 31% of ECs are accompanied by cold surges. The occurrence and development of ECs favour eruptions of cold air from higher latitudes, which in turn produce conditions conducive to cold surges. In the North Pacific, ECs travel in a northeastward direction, ultimately contributing to the Aleutian low. Meanwhile, the westerly jet is observed to strengthen following cold surge events. Both actions drive further EC activity, which in turn facilitates subsequent cold surges. Therefore, when ECs occur before and after cold surges, the cold surge event itself tends to be relatively strong and long lived. The transmission of energy by ECs is a primary link between the high and middle latitudes and contributes to the impact of cold surges on low latitudes. This study also explores the respective influences of the Siberia High and Aleutian Low on cold surges. The majority of cold surges that do not involve ECs occur in the context of the weaker Siberia High and Aleutian Low. Cold surges accompanied with ECs can be even stronger and longer lasting when the Siberia High and Aleutian Low strengthen. Article in Journal/Newspaper aleutian low Siberia Wiley Online Library Pacific Meteorological Applications 31 2
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract Cold surge events in the South China Sea (over 110–117.5° E longitude at 15° N latitude) from 1979 to 2019 are divided into four types depending on their correlation with North Pacific extratropical cyclones (ECs). Climatologic relationships between the two phenomena reveal that 92% (39%) of all cold surges are accompanied by ECs (explosive extratropical cyclones, abbreviated as EC‐E), while 31% of ECs are accompanied by cold surges. The occurrence and development of ECs favour eruptions of cold air from higher latitudes, which in turn produce conditions conducive to cold surges. In the North Pacific, ECs travel in a northeastward direction, ultimately contributing to the Aleutian low. Meanwhile, the westerly jet is observed to strengthen following cold surge events. Both actions drive further EC activity, which in turn facilitates subsequent cold surges. Therefore, when ECs occur before and after cold surges, the cold surge event itself tends to be relatively strong and long lived. The transmission of energy by ECs is a primary link between the high and middle latitudes and contributes to the impact of cold surges on low latitudes. This study also explores the respective influences of the Siberia High and Aleutian Low on cold surges. The majority of cold surges that do not involve ECs occur in the context of the weaker Siberia High and Aleutian Low. Cold surges accompanied with ECs can be even stronger and longer lasting when the Siberia High and Aleutian Low strengthen.
author2 National Natural Science Foundation of China
Applied Basic Research Foundation of Yunnan Province
format Article in Journal/Newspaper
author Xia, Lan
Zhang, Jialin
Hu, Yao
spellingShingle Xia, Lan
Zhang, Jialin
Hu, Yao
Climatic interactions between cold surges in the South China Sea and North Pacific extratropical cyclones
author_facet Xia, Lan
Zhang, Jialin
Hu, Yao
author_sort Xia, Lan
title Climatic interactions between cold surges in the South China Sea and North Pacific extratropical cyclones
title_short Climatic interactions between cold surges in the South China Sea and North Pacific extratropical cyclones
title_full Climatic interactions between cold surges in the South China Sea and North Pacific extratropical cyclones
title_fullStr Climatic interactions between cold surges in the South China Sea and North Pacific extratropical cyclones
title_full_unstemmed Climatic interactions between cold surges in the South China Sea and North Pacific extratropical cyclones
title_sort climatic interactions between cold surges in the south china sea and north pacific extratropical cyclones
publisher Wiley
publishDate 2024
url http://dx.doi.org/10.1002/met.2182
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/met.2182
geographic Pacific
geographic_facet Pacific
genre aleutian low
Siberia
genre_facet aleutian low
Siberia
op_source Meteorological Applications
volume 31, issue 2
ISSN 1350-4827 1469-8080
op_rights http://creativecommons.org/licenses/by-nc-nd/4.0/
op_doi https://doi.org/10.1002/met.2182
container_title Meteorological Applications
container_volume 31
container_issue 2
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