Characteristics and causes of Taiwan's extreme rainfall in 2022 January and February

Over the past 40 years (1982–2021), the January and February (JF) rainfall in Taiwan has shown a clear decreasing trend. However, in 2022, the JF rainfall suddenly climbed to the third-highest value ever recorded in Taiwan. This study aims to explore the characteristics and causes of this unique eve...

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Main Authors: Shao-Chin Huang, Wan-Ru Huang, Yi-chao Wu, Yi-Chiang Yu, Jung-Lien Chu, Ben Jong-Dao Jou
Format: Article
Language:English
Published: Elsevier 2022-12-01
Series:Weather and Climate Extremes
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S2212094722001116
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author Shao-Chin Huang
Wan-Ru Huang
Yi-chao Wu
Yi-Chiang Yu
Jung-Lien Chu
Ben Jong-Dao Jou
author_facet Shao-Chin Huang
Wan-Ru Huang
Yi-chao Wu
Yi-Chiang Yu
Jung-Lien Chu
Ben Jong-Dao Jou
author_sort Shao-Chin Huang
collection DOAJ
description Over the past 40 years (1982–2021), the January and February (JF) rainfall in Taiwan has shown a clear decreasing trend. However, in 2022, the JF rainfall suddenly climbed to the third-highest value ever recorded in Taiwan. This study aims to explore the characteristics and causes of this unique event. Our results show that the significant increase in JF 2022 rainfall is contributed by both an increase in rainfall occurrence frequency and an increase in rainfall intensity. Further analysis shows that most of the JF 2022 rainfall is contributed by the rainy systems propagating from South China or the north of South China Sea to Taiwan but without the frontal structure, which is different from the general concept that JF rainfall is dominated by winter monsoon circulation-induced orographic rainfall and frontal rainfall. As a result, southern Taiwan experienced more than a 130% increase in JF 2022 rainfall compared to the JF climate mean. Possible physical explanations for the increase in JF 2022 rainfall can be attributed to the enhanced winter background circulation, which featured an enhanced regional northeasterly wind at 925 hPa coupled with an enhanced southwesterly wind transporting moisture at 700 hPa covering the domain of (10°-30°N, 100°-120°E). Consequently, an active convection zone extending from the southeastern Bay of Bengal to Taiwan was revealed in JF 2022 to result in the extreme rainfall in Taiwan. Further analysis also indicates that the relationship between the Taiwan JF rainfall and the tropical sea surface temperature has changed since 2002.
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spelling doaj.art-61e2d4607d184a4387692157ea723dfe2022-12-22T02:48:37ZengElsevierWeather and Climate Extremes2212-09472022-12-0138100532Characteristics and causes of Taiwan's extreme rainfall in 2022 January and FebruaryShao-Chin Huang0Wan-Ru Huang1Yi-chao Wu2Yi-Chiang Yu3Jung-Lien Chu4Ben Jong-Dao Jou5National Science and Technology Center for Disaster Reduction, New Taipei City, TaiwanDepartment of Earth Sciences, National Taiwan Normal University, Taipei, Taiwan; Corresponding author. Department of Earth Sciences, National Taiwan Normal University, No. 88, Sec. 4, Tingchou Rd., Wenshan District, Taipei, 11677, Taiwan.National Science and Technology Center for Disaster Reduction, New Taipei City, TaiwanNational Science and Technology Center for Disaster Reduction, New Taipei City, TaiwanNational Science and Technology Center for Disaster Reduction, New Taipei City, TaiwanDepartment of Atmospheric Sciences, National Taiwan University, Taipei, TaiwanOver the past 40 years (1982–2021), the January and February (JF) rainfall in Taiwan has shown a clear decreasing trend. However, in 2022, the JF rainfall suddenly climbed to the third-highest value ever recorded in Taiwan. This study aims to explore the characteristics and causes of this unique event. Our results show that the significant increase in JF 2022 rainfall is contributed by both an increase in rainfall occurrence frequency and an increase in rainfall intensity. Further analysis shows that most of the JF 2022 rainfall is contributed by the rainy systems propagating from South China or the north of South China Sea to Taiwan but without the frontal structure, which is different from the general concept that JF rainfall is dominated by winter monsoon circulation-induced orographic rainfall and frontal rainfall. As a result, southern Taiwan experienced more than a 130% increase in JF 2022 rainfall compared to the JF climate mean. Possible physical explanations for the increase in JF 2022 rainfall can be attributed to the enhanced winter background circulation, which featured an enhanced regional northeasterly wind at 925 hPa coupled with an enhanced southwesterly wind transporting moisture at 700 hPa covering the domain of (10°-30°N, 100°-120°E). Consequently, an active convection zone extending from the southeastern Bay of Bengal to Taiwan was revealed in JF 2022 to result in the extreme rainfall in Taiwan. Further analysis also indicates that the relationship between the Taiwan JF rainfall and the tropical sea surface temperature has changed since 2002.http://www.sciencedirect.com/science/article/pii/S2212094722001116Extreme winter rainfall eventEast Asian monsoon regionMultiple timescale variations
spellingShingle Shao-Chin Huang
Wan-Ru Huang
Yi-chao Wu
Yi-Chiang Yu
Jung-Lien Chu
Ben Jong-Dao Jou
Characteristics and causes of Taiwan's extreme rainfall in 2022 January and February
Weather and Climate Extremes
Extreme winter rainfall event
East Asian monsoon region
Multiple timescale variations
title Characteristics and causes of Taiwan's extreme rainfall in 2022 January and February
title_full Characteristics and causes of Taiwan's extreme rainfall in 2022 January and February
title_fullStr Characteristics and causes of Taiwan's extreme rainfall in 2022 January and February
title_full_unstemmed Characteristics and causes of Taiwan's extreme rainfall in 2022 January and February
title_short Characteristics and causes of Taiwan's extreme rainfall in 2022 January and February
title_sort characteristics and causes of taiwan s extreme rainfall in 2022 january and february
topic Extreme winter rainfall event
East Asian monsoon region
Multiple timescale variations
url http://www.sciencedirect.com/science/article/pii/S2212094722001116
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