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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Bibliographic Details
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:
Pacific
aleutian low
Siberia
Online Access:http://dx.doi.org/10.1002/met.2182
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/met.2182
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Summary: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.

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