The recent increasing frequency of strong cooling event in Southwest China in February

Abstract A strong cooling event refers to a sharp change in the average temperature over a short period. The rapid change of temperature has important effect on human health and is highly concerned recent years. Based on the observed temperature data set from stations in Southwest China (SWC) from 1...

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Published in:International Journal of Climatology
Main Authors: Chang, Sun, Zi‐Niu, Xiao
Other Authors: National Natural Science Foundation of China
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2024
Subjects:
Online Access:http://dx.doi.org/10.1002/joc.8550
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.8550
id crwiley:10.1002/joc.8550
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spelling crwiley:10.1002/joc.8550 2024-10-06T13:47:35+00:00 The recent increasing frequency of strong cooling event in Southwest China in February Chang, Sun Zi‐Niu, Xiao National Natural Science Foundation of China 2024 http://dx.doi.org/10.1002/joc.8550 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.8550 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor International Journal of Climatology volume 44, issue 11, page 3778-3791 ISSN 0899-8418 1097-0088 journal-article 2024 crwiley https://doi.org/10.1002/joc.8550 2024-09-11T04:12:26Z Abstract A strong cooling event refers to a sharp change in the average temperature over a short period. The rapid change of temperature has important effect on human health and is highly concerned recent years. Based on the observed temperature data set from stations in Southwest China (SWC) from 1979 to 2017, this paper analyses the characteristics of the strong cooling event (SCE). The result shows that SCE occurs with the highest frequency during the time from February to May. Among them, the frequency of SCE in February exhibits an abrupt change before and after 2005 with a significant increase. Further study reveals that the change of SCE frequency in February is associated with the large‐scale background circulation patterns. After 2005, there is a cyclonic circulation anomaly in Northeast Asia and an anticyclonic circulation anomaly in the Tibet Plateau (TP). This pattern provides a favourable condition for the southward movement of cold air mass, thereby increasing the frequency of SCE in SWC. Furthermore, it is revealed that there is a strong correlation between the variation of SCE frequency in February and sea surface temperatures (SST) in the Northwest Pacific in January before 2005. The cold SST anomaly could favour the occurrence of extreme TD events in SWC through vertical circulation. After 2005, the correlation between SCE and Northwest Pacific SST is not significant. The sea ice in the northern Barents Sea and Kara Sea becomes the dominant impact factor. The abnormally low sea ice concentration is conducive to strengthen the meridional circulation over East Asia, leading to an increasing frequency of SCE in SWC. Article in Journal/Newspaper Barents Sea Kara Sea Sea ice Wiley Online Library Barents Sea Kara Sea Pacific International Journal of Climatology 44 11 3778 3791
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract A strong cooling event refers to a sharp change in the average temperature over a short period. The rapid change of temperature has important effect on human health and is highly concerned recent years. Based on the observed temperature data set from stations in Southwest China (SWC) from 1979 to 2017, this paper analyses the characteristics of the strong cooling event (SCE). The result shows that SCE occurs with the highest frequency during the time from February to May. Among them, the frequency of SCE in February exhibits an abrupt change before and after 2005 with a significant increase. Further study reveals that the change of SCE frequency in February is associated with the large‐scale background circulation patterns. After 2005, there is a cyclonic circulation anomaly in Northeast Asia and an anticyclonic circulation anomaly in the Tibet Plateau (TP). This pattern provides a favourable condition for the southward movement of cold air mass, thereby increasing the frequency of SCE in SWC. Furthermore, it is revealed that there is a strong correlation between the variation of SCE frequency in February and sea surface temperatures (SST) in the Northwest Pacific in January before 2005. The cold SST anomaly could favour the occurrence of extreme TD events in SWC through vertical circulation. After 2005, the correlation between SCE and Northwest Pacific SST is not significant. The sea ice in the northern Barents Sea and Kara Sea becomes the dominant impact factor. The abnormally low sea ice concentration is conducive to strengthen the meridional circulation over East Asia, leading to an increasing frequency of SCE in SWC.
author2 National Natural Science Foundation of China
format Article in Journal/Newspaper
author Chang, Sun
Zi‐Niu, Xiao
spellingShingle Chang, Sun
Zi‐Niu, Xiao
The recent increasing frequency of strong cooling event in Southwest China in February
author_facet Chang, Sun
Zi‐Niu, Xiao
author_sort Chang, Sun
title The recent increasing frequency of strong cooling event in Southwest China in February
title_short The recent increasing frequency of strong cooling event in Southwest China in February
title_full The recent increasing frequency of strong cooling event in Southwest China in February
title_fullStr The recent increasing frequency of strong cooling event in Southwest China in February
title_full_unstemmed The recent increasing frequency of strong cooling event in Southwest China in February
title_sort recent increasing frequency of strong cooling event in southwest china in february
publisher Wiley
publishDate 2024
url http://dx.doi.org/10.1002/joc.8550
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.8550
geographic Barents Sea
Kara Sea
Pacific
geographic_facet Barents Sea
Kara Sea
Pacific
genre Barents Sea
Kara Sea
Sea ice
genre_facet Barents Sea
Kara Sea
Sea ice
op_source International Journal of Climatology
volume 44, issue 11, page 3778-3791
ISSN 0899-8418 1097-0088
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/joc.8550
container_title International Journal of Climatology
container_volume 44
container_issue 11
container_start_page 3778
op_container_end_page 3791
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