Organized Warm-Sector Rainfall in the Coastal Region of South China in an Anticyclone Synoptic Situation: Observational Analysis

Organized warm-sector rainfall (OWSR) near the coast of South China tends to occur in certain synoptic situations characterized with either a low-level jet or an anticyclone, with the latter being less investigated. This paper fills the gap by analyzing 15 OWSR events that occurred in an anticyclone...

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Veröffentlicht in:Journal of Meteorological Research 2021-06, Vol.35 (3), p.460-477
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description Organized warm-sector rainfall (OWSR) near the coast of South China tends to occur in certain synoptic situations characterized with either a low-level jet or an anticyclone, with the latter being less investigated. This paper fills the gap by analyzing 15 OWSR events that occurred in an anticyclone synoptic situation during the pre-summer rainy season of 2011–2016, based on high-resolution observational and reanalysis data. The results show that the anticyclone synoptic situation produces marked northerly boundary-layer winds inland and obvious northeasterly, easterly/southwesterly, and southeasterly boundary-layer winds near the coasts of eastern Guangdong, western Guangdong, and Guangxi, respectively. The coastal boundary-layer winds promote favorable environmental conditions and strong convergence for convection initiation; consequently, OWSR is prone to occur near the coasts of western Guangdong and Guangxi, but exhibits different formation and propagation features in the following two sub-areas. (1) The southeasterly boundary-layer winds tend to converge near the border area between Guangxi and Guangdong (BGG), promoting the formation of a stable convective line along the mountains. The convective line persists with support of upper-level southwesterly winds that facilitate convective cells to propagate along the convective line, producing heavy OWSR along the mountains near BGG. (2) In contrast, a west-east convective line tends to form and maintain near the coast of Yangjiang (YJ) area, about 200 km east of BGG, owing to stable convergence between the easterly (or southwesterly) and the northerly boundary-layer winds reinforced by the mountains near YJ. Moreover, the coupling of upper-level westerly winds with the easterly (southwesterly) boundary-layer winds facilitates expansion (eastward propagation) of the convective line, causing west-east-oriented heavy OWSR near the coast of YJ. In a word, this study reveals refined properties of OWSR initiation and development in the anticyclone synoptic situation, which may help improve the forecast skill of OWSR during the pre-summer rainy season in South China.
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This paper fills the gap by analyzing 15 OWSR events that occurred in an anticyclone synoptic situation during the pre-summer rainy season of 2011–2016, based on high-resolution observational and reanalysis data. The results show that the anticyclone synoptic situation produces marked northerly boundary-layer winds inland and obvious northeasterly, easterly/southwesterly, and southeasterly boundary-layer winds near the coasts of eastern Guangdong, western Guangdong, and Guangxi, respectively. The coastal boundary-layer winds promote favorable environmental conditions and strong convergence for convection initiation; consequently, OWSR is prone to occur near the coasts of western Guangdong and Guangxi, but exhibits different formation and propagation features in the following two sub-areas. (1) The southeasterly boundary-layer winds tend to converge near the border area between Guangxi and Guangdong (BGG), promoting the formation of a stable convective line along the mountains. The convective line persists with support of upper-level southwesterly winds that facilitate convective cells to propagate along the convective line, producing heavy OWSR along the mountains near BGG. (2) In contrast, a west-east convective line tends to form and maintain near the coast of Yangjiang (YJ) area, about 200 km east of BGG, owing to stable convergence between the easterly (or southwesterly) and the northerly boundary-layer winds reinforced by the mountains near YJ. Moreover, the coupling of upper-level westerly winds with the easterly (southwesterly) boundary-layer winds facilitates expansion (eastward propagation) of the convective line, causing west-east-oriented heavy OWSR near the coast of YJ. 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The convective line persists with support of upper-level southwesterly winds that facilitate convective cells to propagate along the convective line, producing heavy OWSR along the mountains near BGG. (2) In contrast, a west-east convective line tends to form and maintain near the coast of Yangjiang (YJ) area, about 200 km east of BGG, owing to stable convergence between the easterly (or southwesterly) and the northerly boundary-layer winds reinforced by the mountains near YJ. Moreover, the coupling of upper-level westerly winds with the easterly (southwesterly) boundary-layer winds facilitates expansion (eastward propagation) of the convective line, causing west-east-oriented heavy OWSR near the coast of YJ. In a word, this study reveals refined properties of OWSR initiation and development in the anticyclone synoptic situation, which may help improve the forecast skill of OWSR during the pre-summer rainy season in South China.</description><subject>Analysis</subject><subject>Atmospheric Protection/Air Quality Control/Air Pollution</subject><subject>Atmospheric Sciences</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geophysics and Environmental Physics</subject><subject>Meteorology</subject><subject>Original Paper</subject><subject>Rain and rainfall</subject><issn>2095-6037</issn><issn>2198-0934</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><recordid>eNp1UU1P3DAQjapWKgJ-ADffegod2_Em6W21ooCEtBJLxdGaeJ2sUdYG21vYnvjpzBKknpBlz4z13ny8KYozDuccoP6ZuJSKlyDoclWX1ZfiSPC2KaGV1VfyoVXlDGT9vThN6QEARCtULcRR8bqMA3r3z67ZPcZtubImh8hu0fkex5E5z_LGskXAlHFkt3ZwwbPQs1XY5Q1bbJzHAwg9m_vszN6MwVu22vvwSCFbubzDTJxfbNklG_--B5RpTs8-uXRSfKNCyZ5-2OPiz--Lu8VVebO8vF7Mb0pTgcglb7HhwioFTa86RFSN5LKtm56LvrGqma0leT3OxNp2xnCoVVdXUCnokIaVx8WPKe8z0mR-0A9hF6mHpJ9eXjptBakHEmBGyPMJOeBoNekQckRDZ223ztB0vaP_eU1KQyMrSQQ-EUwMKUXb68fothj3moM-LEhPC9JUQh8WpCviiImTCOsHG__38znpDSW3kyc</recordid><startdate>20210601</startdate><enddate>20210601</enddate><creator>Liang, Zhaoming</creator><creator>Gao, Shouting</creator><general>The Chinese Meteorological Society</general><general>Springer</general><general>State Key Laboratory of Severe Weather,Chinese Academy of Meteorological Sciences,China Meteorological Administration,Beijing 100081</general><general>Southern Marine Science and Engineering Guangdong Laboratory(Zhuhai),Zhuhai 519082%Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing 100029</general><general>University of Chinese Academy of Sciences,Beijing 100049</general><scope>AAYXX</scope><scope>CITATION</scope><scope>IAO</scope><scope>2B.</scope><scope>4A8</scope><scope>92I</scope><scope>93N</scope><scope>PSX</scope><scope>TCJ</scope></search><sort><creationdate>20210601</creationdate><title>Organized Warm-Sector Rainfall in the Coastal Region of South China in an Anticyclone Synoptic Situation: Observational Analysis</title><author>Liang, Zhaoming ; Gao, Shouting</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c402t-19a812e5508f5baaa58313978f12f8e586d312ffa62debcc1075b740450ba9253</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Analysis</topic><topic>Atmospheric Protection/Air Quality Control/Air Pollution</topic><topic>Atmospheric Sciences</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Geophysics and Environmental Physics</topic><topic>Meteorology</topic><topic>Original Paper</topic><topic>Rain and rainfall</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Liang, Zhaoming</creatorcontrib><creatorcontrib>Gao, Shouting</creatorcontrib><collection>CrossRef</collection><collection>Gale Academic OneFile</collection><collection>Wanfang Data Journals - Hong Kong</collection><collection>WANFANG Data Centre</collection><collection>Wanfang Data Journals</collection><collection>万方数据期刊 - 香港版</collection><collection>China Online Journals (COJ)</collection><collection>China Online Journals (COJ)</collection><jtitle>Journal of Meteorological Research</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Liang, Zhaoming</au><au>Gao, Shouting</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Organized Warm-Sector Rainfall in the Coastal Region of South China in an Anticyclone Synoptic Situation: Observational Analysis</atitle><jtitle>Journal of Meteorological Research</jtitle><stitle>J Meteorol Res</stitle><date>2021-06-01</date><risdate>2021</risdate><volume>35</volume><issue>3</issue><spage>460</spage><epage>477</epage><pages>460-477</pages><issn>2095-6037</issn><eissn>2198-0934</eissn><abstract>Organized warm-sector rainfall (OWSR) near the coast of South China tends to occur in certain synoptic situations characterized with either a low-level jet or an anticyclone, with the latter being less investigated. 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The convective line persists with support of upper-level southwesterly winds that facilitate convective cells to propagate along the convective line, producing heavy OWSR along the mountains near BGG. (2) In contrast, a west-east convective line tends to form and maintain near the coast of Yangjiang (YJ) area, about 200 km east of BGG, owing to stable convergence between the easterly (or southwesterly) and the northerly boundary-layer winds reinforced by the mountains near YJ. Moreover, the coupling of upper-level westerly winds with the easterly (southwesterly) boundary-layer winds facilitates expansion (eastward propagation) of the convective line, causing west-east-oriented heavy OWSR near the coast of YJ. 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subjects Analysis
Atmospheric Protection/Air Quality Control/Air Pollution
Atmospheric Sciences
Earth and Environmental Science
Earth Sciences
Geophysics and Environmental Physics
Meteorology
Original Paper
Rain and rainfall
title Organized Warm-Sector Rainfall in the Coastal Region of South China in an Anticyclone Synoptic Situation: Observational Analysis
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